Most people who see or hear these letters spoken in the summer immediately think of air conditioning. However, meteorologists (who think differently from normal people) readily associate these letters with the international observation code for altocumulus clouds. These are common summertime clouds which form in the middle layers of the atmosphere. They are puffy, rounded masses, some with considerable vertical development. They typically form between 6500 ft and 25,000 ft. They indicate moderate instability and turbulence in the middle layers of the atmosphere, but they are not associated with severe weather.

Acicular Ice
After the Latin word "aciculus," meaning needle-like, "acicular ice" refers to a type of ice which forms in fresh water (lakes and slow moving rivers) between the bottom of the ice layer and the contact point with the underlying water surface. This form of ice, sometimes also called "fibrous ice" or "satin ice" consists of long crystals or needles and sometimes hollow tubes extended from the undersurface of the ice cover. It is more visible in the late winter or early spring as lake ice cover begins to thin out.

Aeolian Sounds
Aeolian sounds are produced by the action or effect of the wind. They tend to become more perceptible in the fall as wind speeds increase. Eddies or currents of air formed immediately beyond an obstructing object (such as the roof of a building, a chimney, a tree, or telephone wires) can produce their own sound, with a pitch that varies directly with the wind speed and inversely with the diameter of the object obstructing the wind. This is what leads to the humming of wires, the whispering of pine trees, and the howling around rooftops. Other aeolian sounds (such as the rattle of dried corn stalks in the field, the rustle of leaves down the sidewalk, the creaking and groaning of tree branches, and the flapping of flags) are due to combinations of wind and other factors.

Afterheat and Aftersummer
These are very old terms used to refer to the warm pleasant days in the late autumn (at or after Indian Summer). It was thought that the residual heat of summer stored in the ground was released under sunny skies and helped produce temperatures that were well above normal for the late autumn. Though the soil does indeed accumulate and store heat during the summer months, periods of late autumn warmth are more often attributed to advection - the regional-scale transport of heat carried in the surface winds from one area to another. Temperatures which reach 10 to 20 degrees above normal this time of year cannot be generated locally by the low sun beating down on the Earth or by heat released from the ground.

Contrary to popular opinion, agglomeration is not what they served the frontier soldiers at the Fort Snelling Commissary!

"Agglomeration" is a term used in cloud physics to describe a precipitation process whereby water droplets or ice crystals grow in size by collision and assimilation with other precipitation particles. When two colliding water droplets form a new larger droplet, this agglomeration process is called "coalescence." When an ice crystal collides with a supercooled water droplet which is assimilated and freezes, this agglomeration process is called "accretion." Accretion may eventually lead to the formation of hail. Snowflakes are agglomerations of various ice crystals as well.

This term is derived from the Latin word, albus which means whiteness. Meteorologists and climatologists use this term to refer to the characteristic reflectivity of a surface or composite landscape. Technically, albedo refers to the ratio of the amount of radiation (visible or total solar) reflected by a surface to the amount of radiation incident upon it. Albedo can make a big difference during the winter season, as bare ground or forest canopies may have an albedo of 10 to 20 percent, while fresh snow cover over prairies or flat agricultural fields may have an albedo of 80 to 90 percent. Thus, the absorption of the sun's radiation at the surface, which provides the energy to heat the air, may be greatly reduced by snow cover. As measured from space borne instruments, the planetary albedo including the radiation reflected by the composite land surface of Earth and its atmosphere is about 30 percent.

This is not a disease, but in many parts of Kentucky people are suffering from this. Hyetos is the Greek term for rain, so the meaning is deductive - lack of rainfall. The term is rarely used anymore, but was used at one time by academics who loathed the use of the term drought to describe short periods without rainfall.

Apparent temperatures
This has been used more commonly since about 1980 to refer to what various temperature and humidity combinations feel like based on human physiology and clothing science and the need for the body to maintain a thermal equilibrium. It particularly applies to the summer months, because relative humidity is much less important to human comfort when air temperatures are below 40 degrees F.

When relative humidities are very low, as in arid conditions, say below 30 percent, the air can actually feel cooler than indicated by a thermometer, because of evaporative cooling effects on the skin. On the other hand, when relative humidities are high, say above 60 percent, then we can feel warmer than the air temperature indicated by a thermometer because of the increased resistence to moisture and heat loss by our bodies (particularly if there is little air movement).

This is a National Weather Service acronym for Automated Surface Observing System. It is a system of weather sensors, data collection hardware, acquisition control modules, communications devices, and peripherals and displays for monitoring local environmental conditions, primarily at airports. Over 1700 such units are deployed around the country to replace manual observations. There is now one operating at the LEX airport, reporting air temperature, cloud ceiling, visibility, dew point, and wind among other things. Forecasters use the frequent ASOS reports to refine and update forecasts. In addition, for some locations computer generated voice reports are available for pilots to dial in and get airport conditions. ASOS systems are being evaluated, but have thus far been subjected to a number of criticisms, including the omission of important climate observations, such as snowfall, snow depth, snow water equivalence, cloud ceiling above 12,000 ft and obstructions to visibility (like smoke or dust). In some cases at busy airports, ASOS data transmissions are augmented by supplementary manual reports on other elements of the climate. It may be a number of years before data users are satisfied that ASOS data and reports are comprehensive enough to document local climatological conditions.

This is taken from the old Anglo Saxon word 'atter' meaning poison or inflammation. The Scottish Meteorological Office will still occasionally use this term to describe a spell of stormy weather, implying that it is like a poisonous, or inflamed condition of the atmosphere. Usually November brings "attery" weather to Kentucky, but there has been a conspicuous absence of it so far this month.

Bai-u, Plum Rains, and Mold Rains
"Bai-u" (in Chinese pronounced "mai-yoo") is the name of the rainy season in southern Japan and eastern China (generally April through July), when abundant rainfall suitable for the cultivation and transplanting of rice usually occurs. These rains are sometimes referred to as "plum rains" when they coincide with the ripening of the plum crop, or "mold rains" when they lead to the outbreak of this form of plant disease.

Some years, these rains have been more than simply abundant. They have been catastrophic in southeastern China and southern Japan, especially on the island of Kyushu. Severe flooding and mudslides have caused casualties, ruined crops, and washed out roads. While we have been complaining of our wet April and May in 2002 in Kentucky, southeastern China has been reporting rainfalls of 6 to 14 inches per week, while southern Japan has reported mold rains of up to 16 to 30 inches per week.

Beaufort weather notation
In addition to devising a scheme to visually estimate wind speed (the Beaufort wind scale) British Admiral Francis Beaufort (1774- 1857) also invented a system of abbreviations and symbols used as codes to represent types of weather observed and logged in diaries and observation books. His system was widely adopted in the 19th century and later modified by British and American meteorologists.

Belfries, Steeples, Spires, Cupolas, and Barns
These are obviously not meteorological terms! So what do they have in common? In the history of weather recording, these are the most common structures for mounting wind vanes (sometimes called weathervanes). The weathercock, which turns to face the wind and is perhaps the oldest style of wind vane, was first used in bronze form during the 9th century on churches in parts of northern Italy. Subsequently, metallic roosters, doves, eagles and lambs were used for wind vanes on many church and public buildings throughout Europe. In the United States, perhaps the best variety of wind vanes can still be seen across the agricultural landscape mounted on the tops of barns.

Billow Clouds
These are clouds which appear as if they are a series of breaking ocean waves. They are produced by the interaction of a saturated stable air layer, usually an inversion, and a pattern of vertical wind shear, which results in somewhat evenly spaced zones of updraft (where cloud tops crest in a wave-like pattern) and subsidence (where cloud droplets evaporate as they descind back to the stable layer. The height of the billows may vary from tens of feet to hundreds of feet and they may be spaced hundreds to thousands of feet apart horizontally.

This is a term used in climate classification to refer to a place on Earth that has two distinct rainy seasons within a year. Most often these are locations near the equator which measure more abundant rainfall at or shortly after the equinoxes (March and September), a period of high sun. Some equatorial African countries and equatorial South American Countries have such climates, including Zanzibar (east Africa) and Bogota (Cloumbia). Tropical rain forest vegitation thrives in this type of climate.

This is not unlike the word "blurt" which refers to a sudden, implusive, and often unexpected verbal response from person. This term is used primarily in Scotland to refer to sudden spells of wind gusts and rain which occur during unsettled highly overcast conditions. Blirty weather certainly fits for many of our early June days in Kentucky this year, some of which have been dominated by spells of rain and cool wind gusts from the north and east. We have seen plenty of clouds, fog, drizzle, rain and wind, along with some record low temperatures already this month.

This is a timely word, since western Kentucky and the eastern Dakotas experienced this type of storm earlier this week. The operational use of this term by the National Weather Service in winter weather warning statements specifies wind gusts of 35 mph or higher, low temperatures (generally less than 20 degrees F) and sufficient snow in the air (either from snow bearing clouds or from blowing snow) to reduce visibility to 0.25 miles or less. These conditions must be expected to last 3 hours or more.

The origin of the word "blizzard" is not entirely known. Early American settlers in Virginia used the term "blizz" to refer to a wind driven rain or snow which reduced visibility. Thus, blizzard may have derived from this term during the 18th century. On the other hand, real blizzard-like conditions are somewhat rare in Virginia and far more common in the Dakotas. Early German settlers in the Dakotas borrowed from the German word "blitzartig" (lightning like) to name sudden and severe winter storms "blizzards." This may be the more plausible explanation. In fact, at one time South Dakota was known as the "Blizzard State", but I suppose that did not prove to be a very marketable nickname, so it is not used much anymore.

Several regions have storms analogous to blizzards, but they refer to them by other names. The buran of Russia, the purga of northern Siberia, and the boulbie of southern France are of a similar nature to the American blizzard and can be life threatening.

Blustery and Tousie
Blustery is often used by the National Weather Service to refer to a day of strong and gusty winds, especially cool or cold northerly winds. Similarly the Scottish Weather Service will refer to such a day as tousie, which is a derivative of the term tousle meaning to tussle or rough about. While Kentucky often suffers a blustery day in winter due to strong, cold, dry winds from Canada, Scotland will get cold, damp winds from the North Sea.

This is a Greek term used to describe a sudden summer squall in the Mediterranean Sea. Strong winds up to 60 mph or greater may lead to high swells and destructive coastline waves and sea spray. Greek fishermen are especially mindful of watching for and reporting on bourini squalls as they move across the region. Some fishing boats are occaisionally lost in these types of storms. Bourinis are sometimes the result of a cold air mass moving rapidly into the Mediterranean off the Balkan Mountains of Bulgaria and colliding with a warm moist air mass over Greece.

No, this is not the guy who hands the bricks to the bricklayer.

Like Cock-eyed Bob and Willy-Willies , this is a colorful Australian term for winds. While we are transitioning to winter, downunder they are approaching summer. Sometimes in summer a hot, dry and dusty wind from the interior deserts blows south and affects the south coastal areas of Australia, making the people who live there uncomfortable and irritable. This wind is called the "brickfielder," presumably because it picks up the red, dusty, brick-like soil of the interior and deposits it over the coastal areas.

Buys-Ballot's Law
Buys-Ballot's Law, sometimes called the baric wind law, is an empirical law in meteorology that relates the horizontal wind field to the atmospheric pressure pattern. It was formulated in 1857 by Christoph H.D. Buys Ballot (pronounced Bowis-Ball-ott), then head of the Dutch Meteorological Services. Basically, the law states that, with your back to the wind, the pressure to your left is lower than the pressure to your right. This law is based on the known wind fields which circulate around low pressure and high pressure systems in the northern hemisphere. It is exactly reversed in the southern hemisphere. In the absence of any weather forecast, you can at least ascertain the direction of low pressure, where frontal activity such as precipitation may be occurring. If you place your back to the wind and are facing north, then low pressure and frontal activity is to the west and likely to be passing your way in the future. Conversely, if you find that you are facing south with your back to the wind, then low pressure is to the east and active weather systems are probably already heading away from you.

"C" Weather
"C" is the designator for contact weather, meaning that pilots of aircraft have sufficient visibility to fly without instruments and use only visual reference to the ground surface.

During the thunderstorm season in Kentucky, you may occasionally hear meteorologists use the term CAPE values. What does that mean? CAPE is an acronym, as is often the case with the National Weather Service. It stands for Convectively Available Potential Energy, an index derived from 12 hourly radiosonde data (balloons), to assess the potential for convective thunderstorms.

As warm air rises it may cool and reach the saturation point where condensation occurs. This process releases energy to the atmosphere (at the rate of 585 calories per gram of water). CAPE values are used to rate the potential energy from condensation between the 850 mb level and the 300 mb level in the atmosphere (roughly 5000 to 30,000 ft above the Earth). These integrated values are expressed in joules/kg. CAPE values in the range from 600 to 2000 are somewhat average. Values less than 600 indicate a very stable atmosphere, while values over 2000 indicate enough energy to produce convective thunderstorms. Values in excess of 2500 show enough energy to produce strong thunderstorms and may be used as a justification for the National Severe Storms Forecast Center (NSSFC) in Norman, OK to issue a severe thunderstorm watch.

CAT advisory
What would a meteorologist be doing issuing a CAT advisory? Do they have knowledge about weather which affects cats in an adverse way? Actually this term has nothing to do with pet cats. It is used by British meteorologists to designate a warning to pilots about Clear Air Turbulence, which is usually a cloud-free wind shear zone aloft that can make for a bumpy plane ride.

Chase Hotel, Dryline Chaser, Meatwagon, White Elephant, StormTracker, U.S.S. Phoenix
As we have suggested in earlier commentaries, storm chasers are in a league of their own when it comes to jargon. These terms have all been used to refer to storm chase vechicles, usually purchased cheaply, then drastically modified to accommodate a variety of instruments and cameras. The Chase Hotel was a 1996 Ford F-150 4X4 pickup. It was not only equipped with special instruments, but it had a sleeping area in back (I guess for the sometimes long waiting periods while severe weather develops). The Dryline Chaser was a 1991 Dodge Caravan, especially equipped with a computer, scanner, ham radio, color TV, camcorder, automated mobile weather station, cellular Internet hookup, and globabl positioning system. The Meatwagon was a 1986 Pontiac Parisienne station wagon which survived an assault by Hurricane Andrew in Florida. The White Elephant was a 1967 Pontiac Tempest, while the StormTracker was a 1990 Checy Astro Van with so many antennas hanging out it looked like a porcupine. One of the most economical storm chasing vehicles is the U.S.S. Phoenix, a Honda Civic SI hatchback used to chase storms in South Dakota and Kentucky.
Taken from old Middle English and Anglo Saxon terms ("chill," meaning cold or shiver, and "blains," meaning sore or swelling), this term refers to a distress of the skin as a result of exposure to cold temperatures. It occurs primarily on exposed hands, wrists, feet, or ankles, but sometimes ears, nose, or cheeks will show symptoms as well. Aside from some pain, the symptoms are swelling, itching, burning, or a redness or bluish mottled appearance. Sometimes the skin will crack. Not as severe as frostbite, this distress is primarily the result of the contraction in the blood vessels near the surface of the skin. The medical term used for this condition is "acrocyanosis." Perhaps in reaction to the arctic air mass this week, some Kentuckyns who failed to bundle up properly are suffering from chilblains.

Chionophile and Chionophobe
Taken from the Greek word for snow, "chiono" (ki-o-no), these are combination words used by ecologists and biologists to describe the character of certain plant or animal species. A chionophile is a snow-loving species and thrives well in winter snow cover; while a chionophole is a snow-hating species which does not do well in snow. I think that most Kentuckyns are chionophiles.

Chocolatero (the chocolate gale)
"Chocolatero" is the term used to describe a moderate to strong northern wind in the Gulf region of Mexico. Such a wind ushers in cold high pressure from the continental United States and temperatures drop markedly. These winds are most common between November and April. The origin of this term is unclear, but I suspect that it has something to do with drinking hot chocolate!

Chronoanemoisothermal diagram
That's a mouthful, pronounced chrono-anemo-iso-thermal diagram. This refers to a graphic which depicts the average temperature for a given place at all hours of the day for each cardinal wind direction (east, south, west, and north). It is especially helpful in regions where the wind direction has great influence on local temperature such as in a lake district or sea coast.

Clear, Scattered, Broken, and Overcast
These are the common terms used in aviation meteorology to refer to sky conditions. They are based on the percentage of sky obscured by clouds. The list below shows the criteria used:

CLEAR less than 10 percent of the sky covered by clouds
SCATTERED 10 to 50 percent of the sky covered by clouds
BROKEN 60 to 90 percent of the sky covered by clouds
OVERCAST greater than 90 percent of the sky covered by clouds

Clinometer, Alidade and Ceiling Projector
Sometimes frustrated middle school or high school mathematics students will ask, "What good is this trigonometry, anyway?" The angular and distance relationships which are learned in trigonometry are very applicable in engineering, navigation, surveying, and (of course) meteorology.

For example, the ceiling projector (also called a ceiling light or cloud searchlight) is used in conjunction with a clinometer or alidade to determine the height of the cloud ceiling at night. The ceiling projector shines a narrow beam of light up to the cloud base. The angular elevation of this spot of light is measured by a clinometer (portable instrument) or alidade (fixed instrument) some distance away from the projector light but on the same horizontal plane. The cloud height Z, is determined by the relationship

Z = L tan E

where L is the horizontal distance between the projector light and the detecting instrument and E is the elevation angle of the spot of light.

One problem with the nighttime measurement of cloud ceiling occurs when it happens to be snowing, when specular reflectance of the falling snow flakes can cause a false light spot to form well below the cloud base and therefore give a ceiling height that is much too low.

"Alidade" is derived from French and Latin words which describe the revolving radius of a circle, while "clinometer" is derived from the Greek words "clino" (meaning bed or horizontal plane) and "meter" (meaning to measure).

Cold Air Funnels
Cold air funnels are not uncommon in Kentucky, especially in the spring. They are always quite small in scale, short-lived, and hardly ever touch the ground. Unlike tornadoes, whose parent clouds are cumulonimbus (thunderheads) and of great vertical depth, cold air funnels may drop from ordinary cumulus clouds as a result of small scale local instability aloft. They represent cold air eddies and typically appear as small conical shaped protuberances, lasting from seconds to minutes. They are not terribly dangerous, but do contain winds of the same order as dust devils, so they might blow around items like lawn chairs if they do touch down.

Cold Soak
This is what some Kentuckyns do after they emerge from several minutes in a hot sauna. It is also a term used by climatologists and engineers to describe equipment exposure in cold climates, especially in polar regions. Machinery or engines which are stored or left idle in cold climates experience a cold soak. Metal becomes more brittle, lubricants thicken and operational tolerances are diminished. Preheating of the machinery before use is often prescribed for equipment that has been cold soaked for extended periods.

This is an acronym for the Cooperative Program for Operational Meteorology, Education and Training administered by the University Corporation for Atmospheric Research. Sponsors include the National Weather Service, the Air Force Weather Agency, and the Naval Meteorology and Oceanography Command. The COMET mission statement is.. "to serve as a premier resource to support, enhance, convey, and stimulate scientific knowledge about the weather for the benefit of providers, educators, and users of weather information." COMET was established in 1989 and has sponsored the development of special forecasting methods and tools. Some previous COMET projects have produced better methods of forecasting windstorms, marine weather for the Great Lakes, lake effect snow storms, and flash floods.
Comma Cloud
This term refers to the typical cloud pattern of a midlatitude cyclone (especially winter storms) when viewed in satellite images. The curvature of the cloud system is like that of a comma because of the counterclockwise rotation of winds that occurs with a strong low pressure system. Visually, a sharply curved cloud system, usually indicates a deep low pressure center and a strong storm. Real-time images of cloud systems over the entire Earth are available on the Internet through the Space Science and Engineering Center at the University of Wisconsin, Madison.

Cyclogenesis and Cyclolosis
"Cyclogenesis" and "cyclolosis" are terms used by meteorologists to refer to stages of an extratropical cyclone or low pressure system. "Cyclogenesis" may refer to the birth of a cyclone or the intensification of cyclonic flow (counterclockwise circulation) around a low pressure system. Typically the pressure gradient increases (central pressure drops), winds strengthen, and clouds become more pronounced during this phase. "Cyclolsis" refers to the death or weakening stage of a cyclone or low pressure system, when the pressure gradient relaxes, winds become lighter, and clouds become thinner and less organized.

Cyclones, Typhoons and Hurricanes
The recent floods in Mozambique and Madagascar are the result of a very active tropical storm season in the Indian Ocean this year. In the western South Pacific and the Indian Ocean severe tropical cyclones (wind speeds of 74 mph or greater) are simply called cyclones. Australian, Indian, and east African weather services will use this term to describe such storms. In the western North Pacific these storms are called typhoons, while in the eastern Pacific Ocean, the Atlantic Ocean, and the Caribbean they are called hurricanes. The current conditions in the western south Pacific, Indian Ocean, and Mozambique channel off east Africa show very high ocean surface temperatures, ranging from 80 to 90 degrees F in many places. This serves as fuel for cyclones to develop. In addition, the jet stream winds are rather weak favoring strong vertical development and sustainability of thunderstorms. Australia and Madagascar have already been affected by a number of cyclones this season, but fortunately in areas that are not heavily populated. On the other hand, Mozambique in east Africa has seen severe flooding brought on by two cyclones which moved very slowly over land and dropped heavy rainfall. Nearly a million people have been displaced from their homes there. This week, yet another cyclone (Gloria) passed over Madagascar and the Mozambique channel dumping excessive rainfall, with strong winds and high seas (15 to 20 ft waves).

Depression Storage
This term is used primarily by hydrologists to refer to the water stored in puddles, ditches, and other small depressions in the local landscape. During the winter in agricultural landscapes where moldboard plowing or ridge tillage has been done on the soil, this small scale depression storage can add up to quite a bit of water which must either be absorbed by the soil or drained before soils can be worked in the spring. In winters like this one, depression storage may be substantial and contribute to high volumes of runoff before soils thaw out enough to allow infiltration.

Derecho (day-ray cho)
"Derecho" is a Spanish word for "right ahead" or "straight ahead." It has become a severe weather term used to describe a windstorm which accompanies a large mesoscale convective complex (MCC) such as the one which crossed the state on July 1. These winds can be long-lived and very destructive as they move along with squall lines and thunderstorm systems. They are part of the family of downburst winds, often quite cool in terms of temperature. Their destructive pattern tends to be different than tornadic winds in that they scatter debris in a narrow vector rather than in all directions. The most severe recent episode of derecho winds was in July of 1995, when over 6 million trees were damaged or destroyed along a wide path in northern Kentucky.

Distinguishing an ice storm warning from a freezing rain/freezing drizzle advisory
The National Weather Service Forecast Offices provide many notices of significant weather events to warn the public about conditions which may present threats to public safety and health. Two of these notices which are sometimes issued during the winter season in Kentucky are an ice storm warning and a freezing rain/freezing drizzle advisory. The significant difference between these two notices is that an ice storm warning means that ice accumulations are expected to equal or exceed 1/4 inch, while a freezing rain/ freezing drizzle advisory pertains to ice accumulation of less than 1/4 inch. Both types of notices infer difficult driving conditions, while the ice storms also threaten power disruptions and damage to landscape plants and trees.

Doctor and Harmattan
These are old colloquisms from West Africa used to describe winds. The harmattan is derived from a Spanish term and refers to the northeast winds that blow in the dry season (November to March). These winds come from the Sahara Desert to the north and bring dry and dusty air, but air that has much lower dew points for the tropical environments of West Africa. Therefore this wind is considered a relief from the steamy heat of the rainy season and restores health to the body and soul.

The doctor is also used in the African tropics to describe a sea breeze which generally brings cool relief from the heat generated in the interior of the continent. During the summer of year in Kentucky, when high dew points (greater than 65 degrees F) sometimes make the air feel oppressive. This may last for days, until we get a a stronger northerly wind which typically ushers in much lower dew points and feels like natural air conditioning. This wind could be called the doctor as well, for it restores our vigor, lifts our spirits and allows us to sleep more comforably.

Dog Days
The "dog days of summer" are usually associated with the greatest heat of the year, characterized by thunderstorm activity and high dew points. The origin of this term is both ancient and astrological:

When Sirius rising with the sun
Marks the dog days well begun

The ancient Greeks and Romans observed that one of the brightest of the stars, Sirius the Dog Star (located in the constellation Canis Major, which is Latin for "greater dog") rose in conjunction with the sun during the six weeks of mid-summer. Hot and sultry weather, which depleted the energy of humans and caused vegetation to wilt, was often experienced during this period and was attributed to the evil effects of Sirius. In the United States, the dog days occur between mid-July and early September, while in western Europe they run from July 3 to August 11.

This term has been misconstrued to refer to the time of summer when dogs are most apt to go mad. Like other mammals, dogs exposed to high temperatures and high dew points will exhibit stress symptoms such as increased panting, change in diet, increased thirst, and lethargic behavior, but I don't know that they go mad more frequently. Some researchers have associated higher crime rates in U.S. cities with the dog days, and one researcher has found that aggression among Major League Baseball players is increased during this period of summer.

Though we felt the dog days of summer in Kentucky during July, they have been relatively mild in August so far, with most locations reporting only one or two days with temperatures of 90 degrees F or greater.

Doppler Radar
The Doppler radar is a type of weather survelliance radar which takes advantage of the Doppler effect. It can determine the radial velocity of atmospheric targets moving directly toward or away from the radar unit based on the change in the frequency between the outgoing and returning (reflected) radar signal. Thus wind speeds associated with thunderstorms can be interpreted, and in particular rotating winds associated with funnel clouds and tornadoes can be seen on the Dopplar radar displays.

Now that the major league baseball season has begun, Doppler radar are routinely used at most ballparks. They are positioned either behind home plate or in centerfield to measure the velocity of pitched balls, which typically range from 70 to 90 mph. In this position the radar gun cannot measure the speed of a throw from shortstop to first base, since the thrown ball crosses the radar beam rather than moving toward it or away from it.

"Duff" is an old English term for plum pudding made from a stiff flour mixture. It is also a term used to describe my golf shots. So how does it relate to meteorology, you ask? It is an important term in the fire weather program of the US Forest Service, used to describe the partially decayed organic matter on the forest floor which can become highly combustible during drought periods and contribute to the longevity and spread of forest fires. In fact, the Keetch-Byram Drought Index is sometimes referred to as the soil/duff drought index because it is a measure of how dry the soil and duff layers are.

Dumbbell or Dumbbelling
These terms are occasionally used by forecasters as verbs when describing the behavior of a low pressure system. Sometimes a low pressure system splits into two circulating lobes that are close to each other. They behave in the large scale weather pattern as a single system, but they actually appear on satellite imagery as two distinct rotating cloud masses. Such a system occurred on Thursday of this week in southern Ontario. Dumbbelling then refers to the shape of the pressure pattern (like a weight room dumbbell) rather than the character of the forecaster.

This word may have several meanings, but for agricultural researchers it refers specifically to management techniques designed to mitigate wind erosion, especially of the type that produces dust and sandstorms. In many semiarid regions where overgrazing has occurred or where farmers have chosen to fallow agricutlural fields, wind erosion can lead to environmental degradation and produce a health and safety hazard. Loss of productive topsoil and decreased visibility on local roads and highways are two of the more obvious negative effects. In addition, recent research has revealed that in some areas small particulate air pollution may come predominately from airborne soil. The EPA is concerned about this, since particulates with diameters of 10 microns or less are small enough to penetrate the lungs.

Dustbusting techniques that have been tried and proven in such areas as the desert regions of California, include construction of barriers such as fences, planting of living windbreaks such as shrubs and trees, or revegetation of the landscape using native or adaptive plant species seeded from aircraft. In California, plants such as buckwheat, saltbushes, Indian ricegrass, and even Califonia poppy have served to revegetate barren landscapes.

Dvorak Technique
In 1975, Vern Dvorak, a meteorologist with the National Environmental Satellite Services, derived a method to analyze and predict tropical storm intensity based on real-time satellite imagery. Though over 20 years old, this technique is still used to assess the strength and project the future intensity of hurricanes, tropical cyclones, and typhoons. The Dvorak technique is based on the pattern recognition of a storm's size and shape using satellite imagery, especially the infrared. Some of the more important storm features used in this technique include the curvature and size of the outerband cloud circulation, the vertical depth of the clouds which compose these bands, and the difference in temperature between the warm eye of the storm and the surrounding cloud tops. Though aircraft reconnaissance provides some of the most important data to assess storm intensity, the Dvorak technique is still used to examine storms between aircraft flights or in tropical areas where instrumented aircraft are not available for storm studies, such as parts of the Pacific Basin. For example, Super Typhoon Rosie in the western Pacific was analyzed continuously by the Dvorak technique this week as it headed toward the south coast of Japan.

Echelon Clouds
Originally derived from the french word for ladder, the term "echelon cloud" refers to a cloud form which produces stair-steps or a terrace illusion to the observer. Aligned clouds, all having the same base elevation much higher than the observer on the ground, are viewed at a lower elevation angle with distance towards the horizon. The observer sees an apparent stair- step effect as if the cloud base gets successively lower with distance to the horizon, even though all the clouds have the same base elevation. These formations can occur with fair weather cumulus or cirrus clouds over Kentucky.

Ekman Spiral
Named for Swedish physicist Walfrid Ekman (1874-1954), the Ekman spiral is an idealized mathematical representation of how the wind-driven surface currents of the ocean behave with depth. It's also a representation of how wind speed and direction vary with height above the ground.

In the oceans of the northern hemisphere, wind-driven surface currents spiral to the right with depth as a result of friction and the Coriolis force (rotation of the Earth). This motion traces an imaginary clockwise descending spiral.

In the atmosphere, the Ekman spiral refers to how winds spiral to the right with height above the ground, as a result of the balance between the Coriolis, pressure gradient, and friction forces. This motion traces an imaginary clockwise ascending spiral. Thus a wind from the south (180 degrees) at the ground level may become a stronger wind from the southwest (225 degrees) at a height of 1000 meters.

The clockwise drift of winds and ocean currents in the northern hemisphere becomes a counterclockwise drift in the southern hemisphere as a result of the Coriolis force.

Elfin Forests
This term is taken from the old Middle English word "elvene" meaning elf-like, small and sprightly. It is used to describe forests which grow in harsh environments, typically windblown, perhaps at high elevation, often dry and in very shallow or rocky soils. Many of the world's mountain ranges have elfin forests. Only dwarf trees can grow and they appear gnarled and misshapen, bearing little resemblance to members of the same species that grow in more favorable environments. The bristlecone pines that grow in Colorado is such a species. In parts of South America they call the elfin trees the Ceja de la Montana, meaning eyebrow of the forest.

This is a National Weather Service acronym for the Emergency Managers Weather Information Network. Developed in cooperation with FEMA (Federal Emergency Management Agency), EMWIN uses a variety of sources of data which are transmitted from the geostationary satellites (GOES 8 and GOES 10) to federal, state, and local emergency management offices which have satellite receiving dishes. A number of the information products are also available on the Internet, including severe weather warnings, hurricane warnings, flood warnings, air pollution statements, specialized forecasts, seismic activity, iceberg reports, and various advisories. Many can be found at the the following web site...

English Rule and American Rule of Groundwater Rights
Historically, under the common law doctrine, rights to utilize groundwater resources have been granted to landowners in the United States and many European countries. In humid climates with abundant precipitation and adequate recharge, the English Rule has applied which grants landowners absolute rights to pump as much water as they wish. This rule does not recognize the fact the pumping water from beneath one property will deplete acquifers that are shared with other property owners. In climates with deficit precipitation, inadequate recharge, and multiple users of groundwater resources, the American Rule applies, which allows landowners a so-called "reasonable use" taking into account the impacts on the water rights of others and depletion limits for specific acquifers. There are still many inconsistencies among states in groundwater rights, but the number of locations and situations where the English Rule applies is continuing to decline as a result of pressures to protect and conserve groundwater resources.

The Equation of Time
The Equation of Time is a simple way of expressing a complex periodic function. For any specific time zone, it represents the difference between mean solar time (local noon) and real solar time (solar noon) measured by the Sun's transit across the sky. The time between successive transits of the Sun across the same point in the sky varies throughout the year, by as much as 15 minutes. This is because of orbital features of the Earth, both its elliptical shape which causes the orbital speed to vary and because of the tilt of the Earth's axis with respect to the plane of the elliptical orbit. This is a primary reason why the earliest sunset in the winter is not coincident with the latest sunrise. More on this complex relationship can be found at the U.S. Naval Observatory web site.

Fair Weather
The word "fair" is derived from old Middle English usage and has many different meanings. It may be used as an adjective, adverb, verb, or noun. Examples of usage include "fair skin," "to play fair," "fair catch," "to hit a ball fair," and "to go to the fair," as is popular in Kentucky right now. In this context it is an exhibition of wares, farm products, and amusements, along with competitions and food, food, food.

Fair Weather
This term is commonly used to refer to visibly pleasant though not necessarily comfortable weather conditions. It is a purely subjective description and may be used with respect to what is normal or average for a particular location and time of year. When the National Weather Service includes this term in their forecasts it is supposed to satisfy some if not all of the following criteria: no precipitation expected; less than 0.4 sky cover of low clouds; very good visibility; and absence of any strong winds. The use of the term often has little regard for air temperature, so that a very warm or cold day may still be referred to as a fair weather day.

The word "fair" has been used to describe a particular weather condition for ages, as in "the weather faired as the night went on," or "fair skies are expected for star gazing," or "the parade will go on whether the weather be fair or foul." Generally speaking, to use the word "fair," a forecaster must ascertain that the skies will either be clear or contain only a few higher level clouds, winds will be light, and temperatures will not deviate significantly from seasonal normals. To be honest, although this term is still used around the world in English speaking countries, National Weather Service personnel probably use it less today than they used to. This is due to the public expectations for more accurate forecasts and the implementation of technology that allows the forecaster to be more precise about specific weather elements and events, particularly their timing.

In the early days of the U.S. Weather Bureau (under the USDA), when forecasts were provided to local communities either by mailing them on postcards or sending them by telegraph, a system of flag signals was used to post the forecasts in town for local residents. Each town had a designated forecast displayman (maybe the postmaster, local weather observer, sheriff, banker, or train station manager). This person would receive the Weather Bureau Forecast and then display the appropriate flag or flags to designate expected conditions. A plain white flag alone would indicate fair weather; a blue flag would indicate that precipitation was expected. Various combinations of square flags, triangular flags, and colored flags would indicate other types of weather conditions. Even as late as the 1960s and 1970s a bank building in downtown Minneapolis would display a colored ball (weather ball) indicating what the weather was going to be.

Four Basic Thunderstorm Types
Thunderstorms occur in a variety of forms, sometimes as an isolated cumulonimbus cloud (anvil shaped), sometimes as a cluster of clouds, sometimes as a squall line, and sometimes as a supercell (massive convective cloud system). The first type is known as a single cell storm usually composed of a convective cloud containing one updraft and one downdraft segment. These may produce some heavy rain, hail, or even a weak tornado, but they are usually short-lived (30 minutes or less). The second type is known as a multicell cluster composed of a group of convective clouds that move together as a single unit. There may be multiple updraft and downdraft segments, highly variable rates of rainfall, and some moderate hail. These systems may last for hours and produce flash flooding or weak tornadoes. The third type is the squall line composed of a line of convective clouds which share a common gust front along the leading edge (sometimes seen as a wall cloud). They can move at rapid speeds and produce heavy rainfall and moderate hail, sometimes resulting in flash flooding. Tornadoes may occur behind the squall line as well. The fourth type of thunderstorm is the most damaging, that is the supercell, which is composed of a system of clouds which rotate as one unit containing imbedded strong updrafts and downdrafts, large hail and frequent lightning. These can produce flooding and moderate to severe tornadoes. They may last for hours and travel across multiple states.

More information about types of thunderstorms can be found at the University of Illinois Atmospheric Sciences Dept.

Frazil Ice
This is an interesting term not frequently used. It refers to ice crystals or needle-like spicules which form in supercooled water of river or stream currents which move too fast for surface ice sheets to form. In salt water is is called lolly ice. The term frazil is from the French fraisil which means cinders. These ice crystals form under the surface in pools or along channel edges and often build up into masses which extend to the stream bottom. The mass of ice may become so large that it effectively dams the flow of the river or stream and causes local flooding. A similar situation can develop from anchor ice, which develops on the rocky bottom of some rivers and builds up toward the surface.

Freezing level
This is a term used in meteorology to refer to the lowest altitude in the atmosphere over a given location at which the air temperature is 32 degrees F (0 degrees C). In other words, the height of the 32 degree temperature surface. It is highly variable and changes markedly with the seasons in Kentucky. In summer it might be as high as 10,000 ft, while in winter it comes right down to the ground at times. Average height of the freezing level at LEX airport during the first week of November is about 3200 ft, but by the end of the month it is about 1200 ft. This change in average freezing level during the month of November is associated with a number of other significant changes in climate during the month including: over a 1 hour reduction in daylength (over 10 hrs to just over 9 hrs); an 18 degree decline in daily mean temperature (from 40 degrees to 22 degrees); an increase in cloudiness; and a increase in the occurrence of freezing precipitation (freezing rain, sleet, snow).

Freshet and Coulee
"Freshet" and "coulee," old and rarely used words, have a gentler connotation associated with the surplus flows of water across a landscape than the words "flood" or "crest."

"Freshet" is derived from Scottish and Middle English terms and has three meanings: (1) a running stream of fresh water which empties into salt water (as in Shakespeare's "He shall drink naught but brine; for I'll not show him where the quick freshets are"); (2) in cold climates, the annual spring rise in streambeds which occurs with snowmelt runoff; (3) a sudden great rise in a stream when it overflows its banks due to heavy rain or snowmelt runoff, causing a local scale flood (much of this has occurred in Kentucky this spring).

"Coulee" is taken from the French word for flow, and may refer to channeled flow or sheet flow off a landscape into a lowland area or basin. "Coulee" sometimes refers to a steep- sloped valley such as the Grand Coulee of the Columbia River basin in the western U.S. Coulees feed into Devils Lake, ND, which has no natural outlet and therefore has been growing in size due to abnormally wet years recently. With abundant snowmelt runoff this year, Devils Lake is expected to grow and perhaps surpass its maximum estimated historical size which occurred in 1830.


Frost Heaving
"Frost heaving" is the lifting of a surface by the internal action of frost. It generally occurs as a result of freeze-thaw cycles. It can also occur, to a lesser extent, by sublimation (ice forming from water vapor at high humidity).

During a thaw period, water droplets can fill the pore spaces in soils or road pavements. This is especially true for macropores or the larger cracks and channels. Subsequent freezing produces lenticular masses of ice or "ice lenses," which by expansion force the overlying material upward. Because moisture is not evenly distributed in the soil or pavement, this expansion is irregular and may produce considerable bumpiness in the surface. This is good for agricultural soils (helping with drainage and aeration), but in pavements and roadbeds this process is very destructive.

This word is used by both geologists and meteorologists. Derived from the Latin root word "fulgur", meaning lightning, this is a term used for the glassy, rootlike tube that is formed when lightning strikes a sandy soil. The intense heat causes soil moisture to vaporize, and the remaining molten material fuses into a tube-like sturcture which may be an inch or two in diameter and inches to several feet in length. The wall-like material holding them together is very thin and fragile, so they typically crumble and fall apart when dug up. Recently University of Florida lightning researchers reported finding a fulurite with three branches, one of which extended 16 feet into the soil. This was noted as a world record size for a fulurite. More on this topic can be found in the July/August issue of Weatherwise Magazine.

This is another acronym that's kind of fun to pronounce. It stands for Global Ocean Observing System, which is part of a global climate monitoring system initiated by the World Meteorological Organization, the International Oceanographic Commission, the United Nations Environment Programme and the International Council of Scientific Unions. Besides monitoring winds, temperature and moisture for climate assessment and prediction, this program will monitor and assess marine living resources, coastal zone environmental changes, carbon fluxes, sea ice and the general health of the oceans. Research in recent years has consistently pointed to the oceanic-atmospheric coupled processes that regulate the climate of Earth. Most historical climate data and research has been associated with land-based studies, but through this program much greater attention will be given to ocean processes in future years.

Garcia Method
No, this does not refer to a style of guitar play or to a method of fishing, even though the Garcia name is known in both these areas! It is a method for forecasting the amount of snowfall expected from a given winter storm system. Named for Chris Garcia, a lead forecaster with the National Weather Service in Milwaukee, WI, this method was published in 1994 and has become a favorite tool of National Weather Service. The method is emperical and considers a number of parameters (ingredients) which cause snowfall, including vertical velocity (upward lift which carries air aloft to a condensation level) and mixing ratio (the mass of water vapor per mass of dry air expressed as g/kg). The method also considers the wind speed aloft because it is important to the advection (transport) of water vapor into the storm system (increasing the mixing ratio) and also because it dictates how fast the winter storm moves over a given area. The level of the atmosphere where these processes are considered important for winter storms ranges from 7,000 to 10,000 feet. A number of studies in recent years have shown that the Garcia Method is superior to many others in forecasting the amount of snow to expect over a 12 hour forecast period. In fact, thanks to the new computing and display power provided by the Advanced Weather Interactive Processing System (AWIPS) installed at the National Weather Service Forecast Offices, the Garcia Method has become a favority tool of their meteorologists in forecasting snowfall amounts 6 to 18 hours ahead.

Originally the Greek word gnomon meant an interpreter, judge or knowledgeable person. The center post of of a sundial is called a gnomon, because it casts a shadow to show what time it is. Thus gnomonists are people in the know who tell time and direction by reading the size and shapes of shadows. The shadow is not always cast upon a sundial. Historically other objects that cast shadows, such as rock formations (Stonehenge), buildings or monuments have been used as well. The space probe named Mars Surveyor carries a sundial of sorts. A gnomon has been added to a color target that is used to calibrate the landers camera. So when the space probe lands on Mars in 2002, an image will be transmitted back to Earth which, in effect, will convey what time it is on Mars.

The term "gorge" is used by many Americans to describe a Thanksgiving Holiday habit, but that is not the definition I intend. The term is used by hydrologists to describe a blockage in a stream or river. This may be in the form of ice, debris such as old logs, or a composite of both. A gorge can be particularly destructive during the onset of winter conditions by blocking the stream or river and allowing surroundings lowlands to flood, or the shoreline to be scoured away by moving ice or depris.

Green Flash
"Green flash" refers to what meteorologists call a twilight or optical phenomenon. It is a brilliant green coloration, often in the form of a dish or disk, located over the upper rim of the sun's apparent disk just before or after it crosses the distant horizon. There is an excellent article about the green flash by Mark Coco in the January (1997) issue of Weatherwise magazine

The green flash results from two characteristics of our Earth's atmosphere. It is produced by atmospheric refraction, causing sunlight to be bent as it passes through a prism. Longer wavelengths which produce red light are refracted or bent less than shorter wavelengths which produce blue or green light. Secondly, when the atmosphere has distinctly different temperature or density structure in the vertical, it acts as a lens, producing a large mirage-type image, and therefore magnifies the size of the green flash. Because the sun sets and rises more rapidly with respect to the horizon in the low latitudes, the green flash is a fleeting image (lasting only seconds) and difficult to view or capture on film. In higher latitudes, because the suns movement with respect to the horizon is slower, the green flash may last for several minutes. It was observed to do so by Admiral Byrd at the South Pole. One needs to have a clear, unobstructed view of the horizon to observe the green flash.

While vacationing on the Gulf Coast of Florida this spring, I hope to view the green flash at sunset.

Gustiness factor
Not much used anymore, this term was used to describe the variability in the wind conditions, based on short temporal measurements of wind gusts. It was more precisely defined as the ratio of the range in wind gusts (maximum minus minimum) divided by the mean wind speed. For example, the wind gusts during the 3 pm hour on Wednesday of this week in the Twin Cities ranged from a 30 mph maximum speed down to 6 mph minimum speed and the mean wind speed for the hour was 24 mph. The ratio was 24/24 which equals a gustiness factor of 100 percent. This is not uncommon in the spring. This measurement used to be routinely reported from airports in order to alert pilots about significant wind variation that might affect their approach and take-off.

This is not a type of seabird, but a Scottish term used to describe a cold, damp wind blowing from the sea. This type of wind often brings either fog, rain or mist. The literal meaning of this word is a "gray coastal meadow." The term is also used in Norway. It could apply equally to the type of weather experienced in Duluth and along the northshore earlier this week (especially Monday), when a cool east wind brought fog, rain and mist inland over the hills and meadows of the Superior National Forest.

Like a downburst from a thunderstorm which brings destructive winds, a heat-burst sometimes occurs as a result of sinking motion within the downdrafts of thunderstorms. It is not destructive, but it does bring a rise in temperature as a result of compressional heating (rising air cools, falling air warms). This can produce some remarkable effects as it did last Friday at Sioux City, IA. At 10pm, well after sunset, a heat burst occurred which temporarily raised the surface temperature from 84 degrees F to 93 degrees F, a value which tied the all-time record high for that date (Sept 25th). As the thunderstorm cell passed by, the temperature dropped to 82 degrees F in less than one hour.

Heat Index
The National Weather Service provides public advisories and warnings when the combination of temperature and humidity becomes high enough to pose a health risk. The Heat Index is used somewhat interchangeably with the term Comfort Index, or Temperature-Humidity Index, to evaluate the combined effects of temperature and humidity on the body's ability to cool itself. An air temperature of 85 degrees F with a relative humidity of 60 percent feels the same as a temperature of 90 degrees F with a humidity of 30 percent according to the Heat Index. For nighttime values of 80 F or above and daytime values 105 F or more, the National Weather Service usually issues a heat advisory. These conditions can cause fatigue, heat cramps, sunstroke or heat exhaustion in some people. Recently some deaths in the northeastern United States were blamed on a persistent heat wave that produced Heat Index Values of 105 to 115 F.

Heat Lightning
This term was derived from observations of lightning under clear skies during warm summer evenings. It was misconstrued that the lightning was produced by an excessively heated atmosphere.

Heat lightning is really the luminosity of the sky overhead produced by distant lightning flashes off the horizon and too far away to be seen. There was some heat lightning in the Twin Cities area on Tuesday evening of this week.

Technically all lightning produces heat, since a single stroke can heat the surrounding air to over 50,000 degrees F, causing sound waves due to the rapid expansion of air, which we later hear as thunder. Sound travels approximately a mile every 5 seconds, so you can gage the distance of the lightning flashes by counting how many seconds pass between the flash and the resulting thunder (approximately 1/5 of a mile for every second). Thus a 15 second interval between observed lightning and the sound of thunder indicates that the flash occurred about 3 miles away. Lightning strokes from over 10 miles away are rarely heard as thunder.

Heliotropic Plants
Some plants exhibit a character known as heliotropism, taken from the Latin root words "helio" for "sun" and "tropos" meaning "to turn." The daily orientation of these plants actually changes with the position of the sun in the sky. For this reason these plants are called "sun trackers." Agronomic crops like sunflowers and some species of cotton are heliotropic, facing east to greet the sun in the morning, and west to say goodbye to the setting sun in the evening. It has been estimated that the sunflower receives up to 40 percent more sunlight on its leaves than it would if it were in a fixed orientation all day. Some desert plants exhibit heliotropic behavior but only during the winter months when the daylength is shorter and the sun's elevation angle is lower.

Horn Card
A couple of weeks ago, we discussed veering winds (wind shifts in a clockwise direction) and backing winds (wind shifts in a counterclockwise direction). Many years ago, sailors aboard trade ships used horn cards to remind them of wind conditions associated with tropical cyclones (storms). Horn cards were transparent disks with diagrams etched on each side to show average wind directions associated with pressure falls in a tropical cyclone. One side showed average wind directions for northern latitudes and the other side for southern latitudes. Sailors could use these cards to determine where their ships were located with respect to the storm field and to anticipate wind shifts as they moved through it.

Hostile Ridge
This term, used earlier in the week by forecaster Byron Paulson of the National Weather Service Forecast Office in Chanhassen, MN can be safely called a meterological colloquialism. But among friends and colleagues of the Weather Service it might be referred to as a Paulsonism. Ridge used by itself refers to an area of high pressure, characterized by low dewpoints, sunny skies, and light winds. However, when combined with the word hostile it has a somewhat different meaning. A relatively strong high pressure ridge will deflect or weaken approaching low pressure systems, diminishing their potential to deliver any significant precipitation. This is the character of a hostile ridge noted by forecasters who might otherwise forecast significant snowfall from an approaching low pressure center in the high plains. It is thus appropriate that those who might be hoping for more snowfall should call this particular weather feature hostile. Similarly, a hostile ridge may be the undoing of an approaching thunderstorm complex in the summer severe weather season. In this context, this weather feature might be more appropriately referred to as a protective ridge or a ridge shield.

Hurricane and Typhoon Seasons
Severe tropical cyclones (wind speeds greater than 74 mph) are called hurricanes in the central and eastern Pacific, Gulf of Mexico and north Atlantic Oceans, typhoons in the western Pacific and Indian Oceans, and willy-willies off the west coast of Australia. The portion of the year having the highest relative frequency of these types of storms is called the hurricane or typhoon season. For the north Atlantic and Gulf of Mexico region this season is June 1 to November 30, while for the eastern Pacific it is May 15 to November 30. In the southwestern Pacific and Indian Oceans the typhoon season runs from November to April, while in the northwestern Pacific it runs from April to October. The typhoon season for Hong Kong is July through September.

Currently Typhoon Maggie is tracking through the Philippine Sea in the northwestern Pacific, but is not presently a threat to make landfall soon.

"Hydrogenesis" is an old word used to describe the process in which natural condensation occurs within the surface cracks and pore spaces of rocks and soils. When the air drops below the dew point within these spaces and cavities, condensation can occur. The liquid water can absorb soluble constituents on the rock or soil and sometimes even percolate to deeper layers.

Used by resource managers, hydrologists, politicians, and to a limited extent by climatologists, this highly contemporary term refers to political negotiation and confrontation over riparian rights which may be associated with both water use and water quality. Two areas of the world where much attention is being given to hydropolitics are the Colorado River Basin in the southwestern United States and northern Mexico, and the Nile, Jordan, and Tigris-Euphrates river systems of the Middle East. The rapid growth in water consumption as more and more land is settled and developed, along with the relative scarcity of alternative water resources in these regions have contributed to somewhat of a hydropolitical crisis. In order to insure an adequate and stable water supply in the face of even normal climatic fluctuations and extrapolated population growth curves, nations and states are negotiating water-sharing treaties and agreements with more vigor than ever. We will undoubtedly be hearing much more use of the term hydropolitics in our remaining lifetime.

Rarely used anymore, but in the old glossary of meteorology, "hythergraph" referred to a climate diagram which showed temperature along one axis and some form of moisture, such as humidity or precipitation, along the other axis. For example, certain climate zones could be characterized by the shape of a hythergraph using mean monthly values. Another form of hythergraph is the comfort chart which shows values of temperature versus values of humidity. For indoor environments in the winter, our comfort zone is most tolerable from 68 to 70 degrees if the indoor humidity remains between 35 and 60 percent. If humidities are lower than this range, we tend to feel too cool; if higher than this range, we tend to feel too warm.

Ice Shove
The word "shove," taken from the old Middle English word "shouven," is most often used as a verb, meaning to push or force away. In the term "ice shove," however, it is a noun, referring to the slabs of ice pushed upon a shoreline as a result of thermal expansion of lake, sea, or river ice cover, or as a result of strong winds. These sometimes large, flat slabs of ice, called pans, may pile up along the shore into odd shaped mounds and towers.

Ice shoves become more evident along the shorelines of larger lakes in Kentucky during late winter and early spring as the temperatures warm up and the winds tend to increase in strength. Some good pictures of ice shoves are online at the U.S. Army Corps of Engineers Web site, which can be found at the following URL:

Ice Spar
The term "ice spar" is used to refer to a stout beam, raft, or spear-like protrusion of ice extending out from a glacier or an iceberg. Spars may be entirely visible or partially submerged in water. Such a feature is suspected to have been the cause of rupture in the sides of the ocean liner Titanic; the vessel avoided a head-on collision with an iceberg, but skirted along one side of it.

This acronym stands for the Indian Ocean Experiment, a collaborate effort among scientists from Asia, Europe and the United States. One of the primary objectives during the 1999 field campaign was to utilize ships, balloon soundings, aircraft measurements and satellite imagery to assess how much pollution (dust, soot, fly ash, sulfates, nitrates, etc) was in the atmosphere over the Indian Ocean and how much was precipitating out in convective storms. During the northern hemisphere winter, a number of pollution plumes originating over India and the Asian continent can be tracked for hundreds of kilometers out over the Indian Ocean. Scientists think that these plumes may be having some impact on the temperature and water vapor patterns detected over that region. Given the severity of convective storm development in recent months (cyclones in the Indian Ocean which have struck Madagascar and Mozambique), this experiment may provide some valuable insight into why this region has seen an increased frequency and intensity of storms.

More information about this experiment is available on their web site:

Interception and interceptometer
These words are taken from the disciplines of agricultural and forest meteorology. Interception refers to the manner by which trees, brush, and crop canopies prevent all precipitation from reaching the soil. The amount of precipitation interception among these species varies from 40 to 100 percent depending on the rate that it is falling, the wind conditions, and the size and shape of the vegetative canopy. Interception helps prevent soil erosion by reducing both the amount of moisture and the kinetic energy which reaches the soil surface.

The interceptometer is the old name given to a rain gage or collection device that is placed underneath the vegetative canopy and allowed to catch the drip from the leaves and stems, or the throughfall which is not intercepted. This catch is compared to that of a rain gage left in an unshielded open setting in order to estimate the amount of rainfall being intercepted.

The Intertropical Convergence Zone (ITCZ)
Highly visible on satellite imagery of the Earth's equatorial regions, this is the somewhat narrow discontinuous belt along either side of the equator where convective clouds and thunderstorms often dominate. The easterly trade winds (NE in the northern hemisphere and SE in the southern hemisphere) converge here, forcing air to rise which triggers convective storms and squalls. The storminess is often more prevalent over the oceans than over the equatorial land surfaces.

Isophane or Isophene
"Isophane" (or "isophene") is a word derived from Greek terms, "iso" meaning "equal" and "phainein" meaning "to show." Either word is used to refer to a line drawn through geographical points on a map where a given seasonal phenological event occurs at the same time. For example, the dates of flowering for crab apple trees or the blooming of lilacs in the spring might be depicted as isophanes on a map. Certainly the maps which commonly appear this time of year in our local newspapers showing where the fall colors are beginning, peaking, or ending might be considered a depiction of isophanes as well.

This is not a type of rodent, nor is it a meteorological term. It is a term from soil science and means a line connecting points on a map which have an equal erosivity index. The average erosivity of soils (loss of soil in sediment runoff) is computed from the Universal Soil Loss Equation partially based on the long term historical rainfall and rainfall intensity. Many other soil characteristics are considered as well. The relative differences in the erosivity index across a landscape can be compared by mapping these values using isoerodents (lines of equal value).

Katabatic and Anabatic Winds
Katabatic winds (taken from the Greek word "katabatikos," meaning "to go down") are sometimes called "gravity winds," "drainage winds," "mountain winds," or "glacier winds." They result when air flows downward from higher positions in the landscape. The air may be channeled through canyons as it flows to lower elevations. This will tend to accelerate the air flow and produce strong winds. Some regional winds such as the foehn (German and Austrian Alps), Chinook (Rocky Mountains), and Santa Ana (Southern California) are dry, warm katabatic winds. On the other hand, glacier winds, which flow downslope as well, are very cold winds, some of which produce the world's worst windchill conditions. An example would be the Cape Denison-Commonwealth Bay region of Antarctica, where winds flowing downward from the interior of the continent to the coast may reach 100 to 200 mph, producing windchill conditions well below -100 degrees F.

Anabatic winds (taken from the Greek word "anabatikos," meaning "to mount") are ascending or upslope winds, often the result of heating along valley slopes. These winds are prevalent in many landscapes with pronounced topography, especially during the daylight hours. Balloonists and pilots of sailplanes often use these winds to maintain or gain altitude. There is even a type of sailplane called an Anabat.

Keras-meltem and Karpooz-meltem
The eastern Mediterranean is famous for many climate characteristics well documented by the ancient Greeks and Romans. One of these climate characteristics is the etesian (periodic) wind of the summer months. This is a moderate to strong northerly wind which blows from mid May to mid October, peaking during July and August. The winds stir up the Aegean and Ionian Seas so much that many still refer to this time as "the season of large boats" because travel becomes too dangerous in smaller craft.

When the winds first start during the increasing daylength up to the summer solstice, they are modest (10-20 mph) and intermittent, usually occurring in the early part of the day, then diminishing in the afternoon and evening. These are called the keras-meltem by the Turkish people because they occur when the cherries (keras) are ripening and being picked. After the summer solstice, the northerly winds become stronger and more persistent, sometimes blowing all day at 25 to 35 mph. These winds are called the karpooz-meltem by the Turkish people because they occur when watermelons (karpooz) are being harvested.

This is the Arabic name given to a class of winds which occur in Egypt and over the Red Sea. The word also means 50 and implies that the frequency of these winds is greatest during the 50 days following the Shem el Nassim holiday in April. But, most commonly these winds occur anywhere from February through June. These hot, dry winds are generally from the southeast, south, or southwest and may range from 30 to 40 mph, carrying a good deal of dust and sand. They result from low pressure systems moving along the Mediterranean near the coast of Egypt.

Historians and Egyptologists have associated these winds with the drifting sands that have buried many Egyptian structures and artifacts. They have also linked these winds to the highly eroded and weathered surfaces of Egyptian monuments, obelisks, and pyramids. Some have claimed that these winds may have assisted in the Exodus of the Israelites from Egypt across the Red Sea, by blowing strong enough to push back the waters.

Lamb Storm, Lamb-showers, or Lamb-blasts
Our April snow showers, not uncommon in northern Kentucky, do not have a colloquial name associated with them. But they certainly do in England and Scotland. "Lamb storm," "lamb-showers," and "lamb-blasts" are used to refer to nuisance storms which produce a light falling of snow in the spring when new lambs are born, most often during March or early April. More severe snow storms or squalls during lambing can be lethal to the newborn lambs, so the U.K. Meteorological Office provides special forecasts to sheep producers during the spring season to help them avoid, or at least anticipate, any weather-related difficulties.

The Laplace Formula
Pierre Simon Laplace was born in Normandy in 1749. Residing in Paris for much of his life, he was a mathematical genius and published many pioneering works in fluid mechanics, calculus and probability theory. His best known work is Mecanique celeste in which he describes a formula for the determination of height from barometric pressure. The fall of air pressure with elevation had been observed for many years, but few had attempted to develop an equation to describe it. This is one of the most important formulas in meteorology and has been used for generations to standardize barometric pressure readings taken from all kinds of landscape elevations to mean sea level values. Aircraft alitmeter settings are based on the Laplace formula.

This is a term used in meteorology to describe a shimmering or terrestrial scintillation observed over a hot surface on a calm, cloudless summer day. In Kentucky this shimmering may be seen on a hot cloudless summer afternoon over a paved road or a stubble field where small grains have been harvested. The shimmering is caused by the unequal refractions of light caused by numerous convective air columns (some only inches in diameter) which differ in temperature and density.

The term laurence comes from St Laurence, the partron saint of cooks, who lived in Roman times (mid 3rd century AD). Laurence was a deacon in the Church of Rome. Only days after the death of Pope St Sixtus, a Roman magistrate demanded that Laurence bring him the riches of the church. Laurence gathered the poor people of Rome and brought them before the magistrate, claiming that they were the riches of the church. The magistrate was so offended that he order Laurence to be roasted alive on a gridiron (basically barbecued). He was later canonized as a saint. In fact tomorrow (August 10) is the traditional St Laurence Day or Feast of St Laurence.

Leaching and Denitrification
"Leaching" and "denitrification" are terms used more often by soil scientists and farmers discussing fertilizer options than climatologists. Leaching refers to the movement or washing out of soluble constituents (chloride, bromide, sulfate or nitrate) within the soil by percolation of water. Moisture moves through successive layers of soil by gravity. In many agricultural soils the moisture is stored until it is removed by plant roots during the growing season. However with some soils, deeper percolation occurs, depositing these soluble materials into acquifers which may be sources of drinking water or water for irrigation. Potential leaching losses are governed by soil moisture, soil texture, and rainfall frequency and intensity.

Denitrification is the biological process in the soil where nitrate nitrogen is converted into a gas and lost through the soil surface to the atmosphere. This process occurs more rapidly under warm and moist conditions and in fine textured soils. Unlike leaching which represents an environmental concern with respect to ground water quality, denitrification losses are not an environmental threat instead can represent an economic loss with respect to a farmers fertilizer program.

Little Brother or Little Sister
These terms are sometimes used by meteorologists to refer to a subsidiary (smaller scale) storm which follows a major one. For example, a tropical cyclone, typhoon or hurricane may be accompanied by a weaker low pressure system which trails along its path. Even in our continental climate here in Kentucky, an occasional little sister or little brother will trail along behind a major winter or spring storm system and bring some addition precipitation or wind following a significant snowfall.

Long Range Forecasting (Outlooks)
"Long range forecasting" refers to the creation of weather statements which forecast for the next 10 days or longer. These are sometimes referred to as "outlooks," since they provide information about expected departures from normal temperatures and precipitation. Long range forecasts are released once per month, on or about the 15th.

Mandatory Levels
Twice daily, at 12 hour intervals, the weather services around the world probe the atmosphere with balloon launched instrumentation, called radiosondes. These measurements of temperature, pressure, humidity and wind throughout the vertical profile of the atmosphere provide the input to a number of numerical forecast models. The design of the forecast models mandates numerical input from certain constant pressure levels in the atmosphere (e.g. 1000 mb, 850 mb, 700 mb, 500 mb, and others). These are called mandatory levels because they are required to make the forecast models work. Radiosondes are generally designed to sample the atmosphere up to an elevation of 19 miles, at which point the balloon may burst and the instrument package released will parachute back to the Earth's surface. The 19 mile elevation includes nearly 99 percent of the Earth's atmospheric mass. The radiosonde balloons are designed to ascend at a nearly constant rate of 300 meters/minute. Numerous precautions are taken to insure that high quality data are collected to run the forecast models. For example if the balloon does not ascend to at least the 400 mb level (approximately 4.5 miles), then a second attempt is made with another balloon. Even if the balloon ascends properly to the 19 mile elevation or beyond, if for any reason it fails to transmit data for an interval of 10 minutes or longer, a second balloon is launched to try again. This reflects on the importance of maintaining a consistent and comprehensive data flow to run the operational forecast models.

Medium Range Forecasting
"Medium range forecasting" refers to the creation of weather statements which forecast for the next 3 to 10 days. Models used to make this forecast are run once per day and depict the weather conditions for either 12 hour or 24 hour time steps. The medium range forecast in Kentucky is often updated each evening using the European Center for Medium Range Weather Forecast model (ECMWF) run out to 6 days, while in the morning the medium range forecast is updated using the Medium Range Forecast (MRF) Model of the National Weather Service run out to 7 days.

Mercury on the chute
This is an expression rarely used anymore, but in the first 50 years of the National Weather Service it was used to describe the onset of a cold wave, when temperatures fall rapidly and reach levels that are a threat to agriculture and commerce. Often times when the mercury in the thermometer was dropping rapidly, meteorologists would report that the "mercury was on the chute." We have already had two episodes of mercury on the chute this month, the 8th to the 9th and the 18th to the 19th when the temperatures fell by more than 30 degrees F.

Mesoscale Convective System (MCS)
This expression, often used by the National Weather Service, refers to a cluster of thunderstorms which is larger in scale than any individual cumulonimbus cloud, but smaller in scale than a frontal system. These systems appear on satellite imagery as circular or linear cloud forms with very bright tops (indicating cold air). Often times severe weather including, hail, damaging winds, heavy rainfall and tornadoes are associated with an MCS. We have already recorded a number of these over the state this June. Many have produced hail, ranging in size from 0.5 to 3.0 inches in diameter.

This is an acronym for the meteorological aviation reports which specifically refer to the international coded reports issued hourly from airport stations. Tailored to the needs of aviation, these reports describe current conditions such as air temperature, dew point, humidity, wind direction, wind speed, altimeter setting, visibility, and cloud ceiling. In coded form they are difficult for the general public to read and interpret. However, in recent years many sites on the Internet have made them available in decoded form, and in real-time. Some of these web sites are:

National Weather Service Home Page
Kentucky Interactive Weather Information Network
National Weather Service Forecast Office in Chanhassen, MN

Meteograms are charts which depict various weather elements (meteorological parameters) for a given location over time based on National Weather Service forecast models. They are available in a variety of forms, but only for major cities in the United States. Typically they show the expected pattern for air temperature, dew point, pressure, wind, sky condition, and precipitation. The graphic for each of these parameters may be plotted hour by hour, or in 3, 6, 12 or 24 hour time steps.

Both the National Weather Service Forecast Office in Chanhassen, MN and the Weather Processor at Purdue University have websites which display meteograms.

"Michael-riggs" is an old term relating to Michaelmas, an English name for the fall season. Celebrated for St Michael, the patron saint of healing, Michaelmas Day falls on September 29 and is commonly marked by a harvest festival in many towns. Symbols of the festival include a glove, representing openhanded generosity, a cooked goose as the centerpiece of the harvest dinner, and gingerbread or gingerbeer because ginger is recognized as a healing spice.

"Michael-riggs" is the term given to the occasional strong gales which blow over England during this season. "Rig" by itself is an old English term for a gale, derived from the observation of how quickly a strong wind can fill the sailing rigs of ships.

Moby Dick Balloon
Most instrumented balloons are released and tracked by weather services around the world every 12 hours for the purpose of taking profile measurements of the atmospheric conditions aloft (pressure, temperature, humidity and wind). However, on occasion weather services have used an instrumented constant-level balloon for long duration flights (over 24 hours) to characterize atmospheric conditions over ocean or land transects. These balloons often reach elevations of 40,000 ft. or higher and maintain a constant altitude as they move with upper level winds. With such low air pressure at these altitudes, these plastic balloons, initially inflated to 6 to 8 ft. diameters at ground launching sites, expand to considerable dimensions (perhaps 20 or 30 ft. diameters) and look perhaps like floating whales in the sky. Thus the nickname, "Moby Dick balloon."

This is an acronym for Model Output Statistics, a tool used by meteorologists to make local forecasts. It refers specifically to a statistical method of relating the output parameters of a numerical weather prediction model (usually scaled for the entire United States or northern hemisphere) to local weather elements such as temperature and humidity. Using the historical relationship between climate records of a given location and past forecasts, the numerical model values are adjusted for local scale effects or biases. The National Weather Service provides forecasters with updated MOS data every three hours which they can use to revise forecasts throughout the day and night if warranted.

This term is derived from the Greek words nepho, meaning "cloud," and scope, meaning "to view." A Nephoscope is an instrument for viewing clouds and determining their motion. There are two types of Nephoscopes: one with a direct view and one with a mirror view of the sky. Each instrument allows the observer to determine the compass direction in which clouds are moving. Cloud motions may vary with elevation; that is, low clouds may be moving in one direction and high clouds moving in another.

We have already seen this type of cloud several times this month. This term is derived from the original Latin based cloud classification system proposed by Englishman Luke Howard in 1803. The cloud form is gray, with a low, ill-defined ceiling. Generally, it completely obscures the sun. Nimbostratus clouds bring rain, snow or sleet. On satellite imagery, they show up as darker clouds when compared to the higher, colder cloud tops.

Here's a word for the master Scrabble player to use. A medical term derived from two Greek words: "nipha" meaning snow; and "blepsia" (after "blepharon" for eyelid) meaning affliction of the eye. Those who don't speak Classical Greek or medical jargon use the more common term "snow blindness" to describe this condition, which is caused by the high reflection of sunlight from snow cover. This intense reflection is so bright that it can cause impaired vision or even temporary blindness. It is most common on bright, sunny winter days in areas where snow has drifted into a relatively uniform surface with little roughness to it. I am sure numerous citizens in Kentucky have been exposed to this condition this winter.

Adopted by participants at the Western Snow Conference in 1942, "niphometrology" was used to refer to the science of snow measurement. It is a composite formed from the Greek root words "nipho," meaning "snow," and "metron," meaning "to measure." This term never caught on in the scientific community, perhaps because it sounded a bit too academic for a process as simple as sticking a yardstick in the snow.

Noctilucent clouds
These are rarely seen wavy, thin bluish or silvery clouds. They appear in shapes and patterns similar to cirrus clouds, but they are much higher, 45 to 55 miles above the Earth's surface in the mesosphere, where temperatures range below -100 degrees F. Most often seen at high latitudes just before sunrise or just after sunset, noctilucent clouds are thought to be composed of ice that is deposited on ejected volanic depris or the dust particles from meteorites.

A meteorological acronym pertaining to weather prediction, this term stands for Navy Operational Global Atmospheric Prediction System. This global scale weather prediction model operates on a gridded resolution of about 12 miles and calculates conditions at 18 different vertical layers in the atmosphere. It is one of the few models which produce a wind field analysis on a global scale, showing streamlines aloft and at the surface, over oceans and over land masses. In addition to the normal radiosonde data, the NOGAPS assimilates ship observations, buoy observations and satellite observations from the Defense Meteorological Satellite Program system of polar orbiters. The web site to access NOGAPS model output is:

Nordenskjold Line
The "Nordenskjold line" is named for the early 20th century Norwegian geologist and polar explorer, Otto Nordenskjold. He documented expeditions to Antarctica, Greenland, the Yukon, Tierra del Fuego and southern Chile. The Nordenskjold line is used to estimate the arctic tree line, which denotes the boundary between the Boreal forest and tundra. This is done by drawing a line through geographic points where the mean temperature for the warmest month (usually July) is equal to 51.4 - 0.1k, where k is equal to the mean temperature of the coldest month (usually January). This equation shows a climate warm enough to produce tree growth in the warmest month, but not cold enough in winter to kill all tree species. The Nordenskjold line is rarely used anymore, since the Boreal forest and tundra boundaries are now more precisely discriminated by satellite imagery.

"Nowcasting" refers to the creation of weather statements which highlight current conditions and forecast for the next few minutes to hours. For example, radar and satellite data are used to project when skies will clear or severe weather will end.

Omega High
An omega high is a ridge of high pressure which disrupts the normal westerly flow pattern across North America. On a surface or upper air map of the pressure pattern it shows up as a feature which looks like the Greek letter omega. Persistent dry, fair weather under the high pressure ridge is often the case, lingering for days or sometimes weeks on end. This feature is also called a "blocking high" because it prevents the normal progression of weather systems and fronts from west to east. Omega highs are more prevalent in the spring, summer, and fall than they are during the winter months.

Operational Weather Limits
Most commonly this refers to the limiting values of cloud ceiling, visibility and winds which allow for safe operation of aircraft, particularly in takeoff and landing. They are typically different for daytime and nighttime operations and are also tailored to the specific airport environments, which account for navigational aids and types of aircraft used. There are also operational weather limits for other endeavors such as snowplowing, well drilling, shipping, painting, and just about any other outdoor activity you can think of.

The Ozone Season
During the warm season in North America, stronger sunlight and heat combine to convert industrial and transportation emissions into smog (ground-level ozone). This is particularly true for major metropolitan areas. The Environmental Protection Agency (EPA) and others have monitoring sites in over 1300 locations, covering more than 70 metropolitan areas and 30 states. National Weather Service forecast models along with data from these monitoring sites are used to produce daily ozone forecasts during the "ozone season", defined for North America as May 10 to September 30 for most places, except in California where it extends to October 31. The season is defined based on the historical frequency of ozone levels (sometimes called the Air Quality Index) that may be unhealthy.

Daily ozone forecast maps and health risks for major cities in the United States can be found on the Internet at the EPA's Office of Air and Radiation web site:

Additional information about ozone and health risks can be found on the Internet at the National Oceanic and Atmospheric Administraton Public Affairs Office web site:

Yes, another scientific acronym, courtesy of the Australian Meteorological Services. The acronym stands for Australian Surface Pressure Bogus Data for the Southern Hemisphere). These are estimated surface pressure observations for the southern hemisphere derived from satellite observations, interpolated from conventional data (ship, buoy, or land surface barometer readings), or extrapolated over time from radiosonde (balloon) measurements. These data are important to an international data assimilation project, called Long Range Reanalysis, which is an attempt to reconstruct all of the surface and upper air meteorological data taken over the last 40 years. The data, originally taken from a variety of measurements and analyzed by a variety of methods, will be quality controlled, and reconstructed in a similar format for researchers to examine large scale trends and patterns in the behavior of the Earth's atmosphere. The PAOBS are important because the southern hemisphere of the Earth is dominated by oceans and has far fewer meteorological data points than the northern hemisphere. The Australian Meteorological Services attempts to routinely characterize the pressure pattern in the southern hemisphere by making PAOB estimates. Though far from perfect, PAOBs are nevertheless a consistent source of data over the decades and valued by the Reanalysis* research community. Both climatologists and meteorologists should gain a better understanding of the behavior in large scale pressure patterns of the Earth from this effort.

*Reanalysis uses available observations and the equations for conservation of energy and momentum that govern the atmosphere to interpolate in time and space meteorological conditions for areas where no observations exist. This is superior to a simple graphical interpolation because the resulting pressure fields are consistent with the physical equations that describe atmospheric fluid dynamics.

Percent Possible Sunshine
Percent possible sunshine is a standard climate measurement made at National Weather Service Offices, but it is often misunderstood as a indicator of solar energy. It is the ratio of the actual duration of bright sunshine (unobstructed sunlight measured by a sunshine recorder) in hours and minutes compared to the astronomically possible duration of sunshine in hours and minutes, from sunrise to sunset, for the local station. Thus, in the winter, when only 8 hours of sunshine are possible for the Twin Cities, 7 hours of actual sunshine would equal 87.5 percent possible sunshine; while in summer when 15 hours of sunshine are possible, 7 hours of actual sunshine would only equal about 47 percent possible sunshine.

Incidentally, long term climate averages show that it is this time of year that we see the maximum percent possible sunshine in Kentucky (typically the last few days of September and first few days of October). Indeed, this climatology seems to be holding true this year!

Derived from the Greek word "phreatos" meaning well or underground water, this term refers to types of plants with extensive root systems that utilize water from the underlying water table. These plants generally have adapted to more arid climates in establishing powerful root systems which can lift water from great depths. The root systems of some phreatophytes have been traced to the depths of 45 feet. Greasewood, mesquite, willow, and alfalfa, among others, are considered phreatophytes.

Pirry, Parry, or Perry
These are not all news anchors! "Pirry," "parry," or "perry" are Scottish and English terms used to describe a sudden squall, or heavy rainfall. Technically, they sometimes refer to squalls that approximate a "half gale" on the Beaufort wind scale (20-22 mph). Some of the brief storms that have occurred this July (1997) might be described as a "perry."

Pleion and Antipleion
In the old days, before meteorologists and climatologists referred to significant climate departures as "anomalies", they used the terms "pleion" and "antipleion" to describe areas with abnormal and persistent positive and negative departures in the elements of climate. These terms were introduced by the famous Polish meteorologist, oceanographer, and geologist Henryk Arctowski (1871-1958), who was the first to keep an entire year of meteorological observations in the Antarctic.

Like the word "anomaly," these words imply a trend in the long term climate, such as a prolonged warm spell lasting many months. The word "pleion," taken from the Greek, means greater than average, while "antipleion" means less than. Thus, pleion signifies an area of positive departure in the pattern of temperature, pressure, or precipitation, while antipleion signifies an area of negative departure.

Using pleionic terminology for the current winter, Kentucky would be described as a pleion with respect to snowfall and snow cover, and an antipleion with respect to temperature.

Plimsoll's Mark or Plimsoll's Line
This is the name given to the conspicous marks painted on the sides of merchant ships that indicate the limit of submergence allowed by law. It is named for Samuel Plimsoll, who championed the law before the British Parliament to prevent captains from overloading their merchant ships. The British merchant ships used this system for years (since at least 1899) before the United States adopted a similar system in 1930.

Load limits or lines were designated as FW (fresh water), S (summer), W (winter) and WNA (winter in the North Atlantic). For merchants carrying goods to and from India, there was an additional Plimsoll Mark, IS (Indian Summer), but this actually a misnomer. It was meant for the October to April period in the Indian Ocean when the summer monsoon season had ended and seas were relatively calm. Loads could be greater during this time.

In fact, expected or prevailing weather is an important factor in designating load limits on merchant ships both on inland waters and in open seas. Since its inception, the Plimsoll Mark has been partially based upon the seas traveled, the time of year, and the prevailing weather. Where the weather historically produced rougher seas with larger swells, Plimsoll Marks designated lighter load limits for ships. If these lines or marks were not rigidly observed, shipping companies could be fined and their insurance policies could be cancelled.

Pluviometric Coefficient
Taken from the Latin root words "pluvio," meaning "rain," and "metre," meaning "to measure," the pluviometric coefficient is a manner of expressing rainfall as a ratio of the average monthly value to one-twelfth of the normal annual amount. Sometimes called an "isomer," it is a way for climatologists to express each month's "share" of the annual precipitation for a particular location. Values less than one represent less than an equal share of the annual precipitation (a relatively dry month), while values greater than one represent a greater than equal share of the annual precipitation. Taking LEX average monthly precipitation values as an example shows that February's 0.88 inch average represents less than a 0.4 share (pluviometric coefficient), while June's 4.05 inch value represents a 1.7 share (pluviometric coefficient). This variability in the pluviometric coefficient is typical of mid-latitude continental climates, while equatorial and marine type climates often have values that are uniformly close to one.

Portmanteau words
This term, meaning "to carry a cloak or mantle," is derived from two french words, porter and manteau. Portmanteau words are formed from partial combinations of two or more words, with parts of each word suppressed.

These are common in meteorological jargon. For example, in upper air measurements and observations "rabals" (radiosonde balloons), "pibals" (pilot balloons), and "pireps" (pilot reports) are used to determine the strength and direction of winds aloft. In air quality terminology, smog is a portmanteau word formed from smoke and fog.

Prognostic Chart and Agnostic Chart
A prognostic chart, often referred to by meteorologists as a "prog," depicts the expected pressure pattern or height pattern of a given synoptic chart (typically scaled to a country, a continent, or an entire hemisphere) for some specified future time, perhaps 24 hours or even 196 hours ahead. Positions of weather fronts and cloud formations are often shown on these charts, which assist forecasters in determining the areal coverage of different weather types. Several times each day, the National Weather Service produces various progs using a variety of models.

An "agnostic chart" is the tongue-in-cheek term used by forecasters to refer to a prog which no one believes. This may be due to observed differences in the local weather conditions, errors in the forecast model, or bad initial measurements to set up the model run. I suppose economists must have a similar term for their bad forecasts.

Psychrometric Tables
These are tables used by meteorologists to determine measures of atmospheric water content (dewpoint, vapor pressure, or relative humidity) from the observed dry-bulb and wet-bulb temperature values taken with a psychrometer. Today's modern electronic instrumentation is often programmed to give these values. The term is composed of the Greek word "psychros" meaning cooling, and meter meaning to measure. The cooling power of the air is related to the water vapor content, the drier the air the more rapidly evaporation, or cooling will occur.

These acronyms refer to models that are used by various meteorological services around the world to forecast the movement of volcanic ash plumes in the atmosphere. PUFF (short for ash puff), a real-time tracer model named by its developer H. Tanaka, uses atmospheric profile data including winds aloft, along with hypothetical particle size distributions of ash to forecast the plume trajectory, dispersion and settling rate of particles. The model forecast is updated and corrected using satellite observations of the ash plume, when it is large enough to detect.

VAFTAD stands for Volcanic Ash Forecast Transport and Dispersion Model and is used in conjunction with the numerical forecast models of the National Weather Service to predict the track and dispersion of ash plumes. The chief purpose of this model is to provide alerts for aircraft route forecasting since ash plumes can present a severe hazard to high flying commercial aircraft. A number of historical cases document aircraft problems with turbulence and stalled engines when flying near or through ash plumes.

Qanik and Aput
According to a new book, Snow in America (available from the Smithsonian Institution Press), "qanik" and "aput" are Eskimo words used to describe snow. "Qanik" refers to snow in the air while "aput" refers to snow on the ground. According to the book, studies by anthropologists have suggested that Eskimos may use over 200 different terms to describe snow. That sounds like overkill to me.

The Reseau Mondial
Derived from French terms, "reseau mondial" translates literally to mean a "network of observations" for an Earth day. Seeing a need for worldwide weather observations to be both organized and standardized, the International Meteorological Committee proposed the establishment of a worldwide observational network in 1907. Seventeen countries promoted this idea. To achieve their goal, they wanted to use a reseau, or gridded network, that covered the entire Earth. Each 10 degree latitude by 10 degree longitude grid was to have at least two meteorological stations, for a total of about 2600 stations worldwide. These stations would all record the same data on a daily basis, including air pressure, temperature, humidity, wind, sky condition, and precipitation, among others. Though it has been nearly a century since this idea was proposed, and there are many thousands of manual and automated meteorological stations currently operating under the standards of the World Meteorological Organization, we have still not achieved the idealized spatial coverage of observations described in the reseau mondial. Perhaps, with the increased deployment of satellite-based meteorological observations, there is no longer the need for it.

Recurrence Interval and Exceedance Interval
In climatology and hydrology "recurrence interval" and "exceedance interval" have been used for many years to describe frequencies of weather parameters and events. The recurrence interval is often called the "return period" and refers to the average time interval between the occurrence of a given quantity and that of an equal or greater quantity. The exceedance interval is similar but refers to the average number of years between the occurrence of a given quantity or event and that of a greater magnitude. Both of these distribution parameters require the analysis of long term measurements.

In Kentucky, for example, the recurrence interval for a rainfall rate of 2 inches per hour is about 25 years. The recurrence interval for a six inch rainstorm in a 24-hour period is about 100 years in southern Kentucky.

The magnitude of floods on major watersheds can be characterized in the same way. However, the measurement record on floods is just over 100 years. The characterization of the flooding this spring in Kentucky as a "500 year flood" is speculation and not based on the statistics of a record period of that duration. In this sense, it is a highly uncertain statement.

Renegade showers
This is how meteorologists often refer to isolated thunderstorms and showers that have broken away from a major complex of thunderstorms or a large frontal system. Often times these clouds escape from the main air flow aloft and may linger over areas of the landscape already saturated by the earlier passage of strong thunderstorms. They typically only effect small areas ranging up to less than 100 square miles. The use of the Spanish term renegade connotates a hostile deserter from the main band of active weather.

With the conversion to electronic maximum/minimum thermometers by most governmental weather services, this term is hardly used anymore. It has been used historically to refer to a defective mercury thermometer used for recording the maximum temperature. The mercury sometimes flows too freely through the constriction in the glass tube designed to prevent it from returning by gravity to the glass bulb at the base. However, because of a defect, the column of mercury expanded by increasing temperature during the daytime, retreats with the fall of temperature and does not properly register the maximum value. When this occurs the maximum temperature for the day is consistently registered too low and climatologists have to correct for such data by using temperature values from a nearby observation point.

Rills and Rivulets
"Rills" and "rivulets" are used to describe the overland flow of water, especially with respect to erosion. "Rills," derived from a similar German word ("rille," meaning stream) are furrow-like and are defined by the Natural Resources Conservation Service as narrow channeled flow less than 4 inches deep with uniform dimensions of size and spacing, which appear and disappear somewhat randomly on slopes from year to year. They are relatively short in length and terminate at a footslope where deposition occurs. Rills may conduct water only during spring snowmelt or precipitation runoff events.

"Rivulets," derived from the Latin word "rivulus," is not as well defined as rills, but refers to a small stream or brook. Rivulets may be larger or smaller flow channels which persist from year to year and terminate in larger streams or rivers. This term also implies that water is always present in the flow channel.

Both of these features will be common in Kentucky this spring, due to the large quantities of snowmelt runoff that are expected to drain and leave signs of erosion on the landscape.

Robin Hood's Wind
"Robin Hood's wind" is a term used to describe a raw and penetrating wind which usually occurs in saturated air with temperatures at or below freezing. This wind robs the heat from even the best dressed (rich) people, much like the legendary Robin Hood robbed from the rich to give to the poor (thus the term).

Robinson anemometer
This instrument is more commonly known today as the cup anemometer, used for measuring wind speed. It was invented by Irish physicist John Thomas Romney Robinson in 1846. He used a vertical shaft, with horizontally mounted spindles at the top, each end capped with a hemispheric cup to catch the wind. The spindles and cups rotated on the vertical shaft and caused a gear with 16 contact points to turn. The number of complete turns was proportional to the mean wind speed. His invention quickly became popular in the scientific community and was adopted as the standard for wind speed measurements in America and several European countries. The mechanical nature of the instrument required frequent calibration and maintenance intervals. Versions of this instrument are still popular today.

Rogue Clouds
The term "rogue clouds" appeared in some of the forecast discussions this week (Greg Tipton with the National Weather Service used it). These are rebel clouds which are left behind when a large cloud mass, usually associated with a surface low or upper air trough, exits the state. They may not last terribly long, as the drier air which usually follows a frontal passage mixes with them until they thin out and disappear. But at this time of year, these clouds can cause some local scale differences in overnight minimum temperatures. They provide a blanket effect to the loss of long wave radiation during the night and tend to keep the underlying surface warmer than the surrounding landscape. When rogue clouds are present overnight, minimum temperature differences within a county or region of the state can vary by 10 or more degrees, as they did on the morning of February 12th.

Route and Terminal Forecasts
These are both terms used in aviation meteorology. A route forecast is specially derived for the planned flight altitude and path to a destination. One element of this forecast is the route component which is the expected wind aloft parallel to the flight path. It may be positive (tailwind) which assists the aircraft speed and fuel efficiency, or it may be negative (headwind) which diminishes the aircraft speed and fuel efficiency.

A terminal forecast is provided to pilots so that they know what type of weather to expect at their destination air terminal. These forecasts may range from 1 hour ahead to 12 hours ahead, depending on the length of the flight.

RUSLE (Revised Universal Soil Loss Equation)
RUSLE is an equation used far more by soil scientists than meteorologists. Originally developed in 1978 (Wischmeier and Smith) and published in the USDA Agricultural Handbook 282, then revised in 1994 (Renard et al) and published in the Journal of Soil and Water Conservation, this equation provides a means to estimate soil erosion and to design conservation practices for limiting the loss of soil. Several factors and subfactors are considered by this equation. An R value (rainfall factor including intensity) is one of the primary factors, but others include soil type, slope, tillage, canopy cover, residue cover, soil moisture, freezing and thawing, and surface roughness.

A paper published this year by Larson, Lindstrom and Schumacher (in Journal of Soil and Water Conservation) pointed out that the RUSLE, based on long term climate records, provides estimates of mean annual soil erosion, but conservation practices should be based on the results obtained for some of the most intense rainstorms because these are the ones which contribute to most of the excessive erosion losses. Conservation structures such as terraces and sedimentation ponds can help limit erosion losses from these rare, high intensity rainstorms. RUSLE can be used for this purpose in areas where rainfall intensity frequencies can be derived from historical records.

Saddle Point and Saddle-Back
"Saddle point" and "saddle-back" must have been coined by cowboy meteorologists! The saddle point (sometimes called a "col") refers to a point in the air pressure pattern depicted on a weather map. A saddle point is both the lowest point of pressure in a trough or depression between two ridges (high pressure systems) and the highest point in a ridge between two lows. Way back in 1916, A. J. Henry wrote of the low pressure saddle, "In summer the pressure saddle is more frequently the seat of local thunderstorms, which are repeated as long as this distribution of pressure lasts; it is the best breeding place for summer afternoon thunderstorms."

A similar concept is that of the "saddle-back." It is a term used by both meteorologists and pilots to describe a certain type of cloud pattern that looks like a saddle. A saddle-back is the cloudless, quiet air overlying a lower cloud deck but between two towering cumulus congestus or cumulonimbus clouds. Jet aircraft can often fly above these menacing cloud forms, but low flying aircraft will sometimes fly through the saddle-backs to avoid longer detours around the thunderheads.

Last week we talked about sounds made by the wind (flags flapping, wires humming, pine trees whispering). Wind also causes various visible types of motion. Two of the most conspicuous in the rural landscape are soil erosion (in extreme cases, dust storms and sandstorms) and the drifting of snow. The movement of soil particles or snow across the landscape is often described as rolling, tumbling, drifting, or even creeping (especially when it is continually in motion by a constant wind). Occasionally, this motion is observed to be a series of leaps or jumps which only occur with strong gusts of wind. This type of motion is called "saltation," taken from the Latin "saltare," meaning "to dance." So, in essence, this term describes dancing soil or dancing snow.

Sand Auger
This term is used to refer to a dust devil or dust whirl which occurs in Death Valley, CA. It usually happens on calm, hot afternoons with clear skies when surface heating is at a maximum. A strong surface level rotating wind up to 300 ft in height may develop and be strong enough to actually auger a hole in the dry layer of surface sand.

Scotch Mist
To some people, Scotch mist is what you sip while sitting in front of a roaring fireplace in the winter. But my frame of reference is strictly meteorological!

This term has been used for generations to describe a combination of thick mist (or fog) and heavy drizzle in Scotland and parts of England. Droplets vary in size from less than .01 inches in diameter to .02 inches in diameter. Some remain suspended in the atmosphere while others fall to the ground. Visibility is is greatly reduced. In southwestern England, particularly Devon and Cornwall, the same type of weather is referred to as "mizzle" (a combination of mist and drizzle).

Secondary air pollutant
This category of atmospheric pollutant refers to a substance or contaminant in the air which results from a chemical reaction between other constituents that are present. An example is photchemical smog which results from a mixture of sunlight, automobile exhaust (nitrous oxides) and various volatile organic compounds. This type of smog often forms in valleys or areas with poor ventilation climatology.

This is an old Swiss term which refers to the oscillating behavior in the surface of a lake or landlocked sea. The oscillations are measurable by minor changes in depth and have a period of several minutes to several hours. This behavior is governed by a number of factors, including changes in atmospheric pressure and variations in wind.

Partially derived from the Greek term "sema," meaning "sign," the literal translation of "semaquir" is "signature stone." In Finland, this stone has the reputation as a weather forecasting tool. It is composed of rock salt and sodium nitrate, both of which are hygroscopic (water absorbing material). When they absorb the vapor from very moist air, the surface of the stone becomes dark, and rain is expected. In dry weather, the surface has a mottled dark and white appearance as a result of salt depositions left after evaporation.

Short Range Forecasting
"Short range forecasting" refers to the creation of weather statements which forecast for the next 12 to 72 hours. Several different forecast models are used for this purpose, all of which are updated every 12 hours. These models project weather conditions in 3 hour, 6 hour, or 12 hour time steps.

This is an acronym for significant meteorological observations used in aviation forecasting. When significant events are observed or forecast a SIGMET is ussued to help pilots plan routes and anticipate conditions. A SIGMET might refer to thunderstorms, icing levels, severe clear air turbulence, volcanic smoke plumes, or other features which affect visibility or aircraft performance.

"Singularity" is a term used by climatologists to describe a highly unusual meteorological condition which tends to occur on or near a specific calendar date much more frequently than pure chance would indicate. This concept has been applied to the January thaw which residents in the northeast United States often see in the last week of the month. In Kentucky, this term has been used to describe the very high frequency of clear days that occurs in late September and early October.

Not used much anymore, this used to be a more common term used in describing a weather condition that was a combination of smoke and haze, or a very light smoke condition that resembled haze. It was more typically used in the 1930s, 1940s, and 1950s in the industrial cities of the United States to describe conditions that were quite frequent during the winter months when inversions can keep haze and smoke around for many consecutive days. However, I don't think it counts in a game of Scrabble!

Snawwreath and Snawbroo
These are terms Scottish meteorologists would have used in describing our weather earlier this week. Snaw is Scottish for snow. A snawwreath is the term for snowdrift, something which was visible in the Kentucky landscape on Tuesday of this week. Broo is a Scottish term used to refer to water for cooking. Thus, snawbroo is melting snow, a feature that was quite visible on Wednesday and Thursday this week.

This term is used by the English and Scottish to refer to a type of biting snow, usually composed of small, wind-driven snow crystals or sleet which stings when they strike exposed skin such as the face or hands. Often winter squalls from the North Sea can produce this type of precipitation.

Snow Penitents
The term "snow penitents" is used to describe a peculiar formation of old snow that is melting mostly as a result of sunlight rather than ambient air temperature. As snow cover ripens and decays in cold temperatures, the suns rays begin to melt the snow where its density is lowest. Hollows form and deepen in the snow crust. These hollows are able to concentrate the sun's rays by reflection and the absorption of radiation is increased. As the hollows deepen, dewpoint and air temperature within these pockets rise, further accelerating the melting process. Finally, the surface looks like a series of minature snow peaks or snow spikes somewhat oriented toward the midday sun. This phenomena is observed routinely in a number of places around the world, including the Himalayas, the Andes, the Alps, mountains of East Africa, Greenland, and Antarctica. Sometimes even in Kentucky, within river valleys, heavily forested areas or sloping terrain, the ripening and melting of the snow cover in late winter under stronger sunlight and cold air temperatures will yield this appearance of snow penitents. I think that the name is derived from an old church practice where sinners doing penitence were required to remain standing during the entire worship service.

Snoweaters and Fogeaters
Snoweaters are atmospheric phenomena which accelerate the melting of snow cover. Meteorologists sometimes refer to both wind and fog as snoweaters. Warm descending air on the leeward side of mountains (Chinook winds) or strong southerly winds coming from warmer latitudes can rapidly melt snow cover in the western or central plains states. These winds are sometimes referred to as snoweaters. Additionally, a fog which forms as a result of warm air advection can be called a snoweater, as the heat released by condensation helps accelerate the melting of snow covering the ground.

Fogeaters are basically any light source which is strong enough to penetrate a layer of fog. A strong airport beacon, a search light, or even a full moon might be referred to as a fogeater. The light passes through the fog (seemingly eating the fog along the path it travels) and gives the observer some perspective of how thick the fog layer is.

Socked In
This is a term derived from the early days of aviation and refers to very low values of cloud ceiling or visibility, most often due to fog. Visibility is so poor that airports used to be closed under such conditions. Improved technologies for instrument flying, airport illumination and fog dissipation have greatly reduced the frequencies of major airports being socked in.

The term was derived from reference to the wind sock, a cloth tube mounted on a mast to indicate wind direction along the runway. When the cloud ceiling was low or visibility so bad that the sock was obscured from view, the airport was said to be "socked in," that is, the sock was in the clouds.

"Sounding" derives from both Latin and Anglo-Saxon terms meaning to submerge something in order to detect depth. In meteorology, the term "sounding" refers to an upper air observation or a complete radiosonde report. Balloons equipped with instrumentation are launched twice each day (12 hours apart) from upper air stations. They transmit back data about temperature, pressure and humidity as they pass through various vertical layers of the atmosphere. These are referred to as "radiosondes." Another type is a "rawinsonde," which is a radiosonde that is tracked by either radar or or a radio direction finder such that wind direction and speed aloft can be plotted for various vertical layers.

These balloons rise to heights of 80,000 to 100,000 feet before they burst. Sometimes farmers and others find the instrument package in their fields. There are instructions on the container to mail the package back to the government so the instruments can be reconditioned and reused.

Derived partially from the Greek word for cave, spelaion, this term means the study of the atmosphere of caves. Research into the atmospheric properties of caves began to flourish in the 1950s and 1960s partially motivated by the medical community which sought to treat patients with bronchial or asthmatic diseases by using cave therapy. The air inside caves was thought to have qualities that would help alleviate respiratory problems. Measurements were made to confirm that the cave atmosphere was (1) more humid, (2) free of allergens such as pollens and dusts, (3) had a lower pH which would restrict the virulence of pathogenic germs, and (4) contained a higher concentration of carbon dioxide which would induce patients to breathe deeper.

With better controlled environments for patients now available in modern medical facilities, I don't think the medical profession is as interested in spelaeo-meteorology as they once were.

This does not refer to the CDs in the music library! In meteorology this term refers to a condition of continuity in the vertical of a low pressure or high pressure system. That is, the geographic center of low pressure at the surface, tends to be the same for low pressure aloft as well. So there is little tilt or horizontal distortion in the pressure field. This may happen with large scale, slow moving low pressure systems and show up in satellite water vapor imagery as a large rotating white blob.

Stagnation area
In air pollution meteorology this refers to a region of the lower atmosphere (planetary boundary layer) near the surface where the following conditions persist for at least 4 days: wind speeds less than 17 mph (poor ventilation), no frontal passages (change in air mass), and no precipitation (washout). Under these conditions, fossil fuel emissions, particulates and other aersols can build up in the atmosphere reducing the air quality.

Earlier this week, these conditions persisted over parts of Florida reducing the air quality significantly.

Stagnation area
This is a term used in pollution meteorology and air quality studies. It refers to a region where the surface layer of the atmosphere is influenced for a period of time (usually 4 or more consecutive days) by high pressure, an inversion layer, calm or little wind, no frontal passages and no measurable precipition. In these conditions, aersols and particulates increase in concentration, reducing local visibility and sometimes producing a health hazard to those with respiratory ailments.

Pollution domes are often visible from aircraft over major metropolitan areas when these conditions persist, but stagnation areas can occur over agricultural and forested landscapes as well. They are just not as visible.

Station Model
In the meteorological community this refers to a specific set of symbols and a pattern for using them to show the state of the weather at each observing station plotted on the map. The symbols and numbers used typically represent air temperature, dewpoint, pressure, sky cover, wind speed and direction, and character of the weather (snowing, raining, fog, dust, etc). More on the station model and interpreting data presented in this form can be found at the Unisys Weather web site:

Staubosphere or Konisphere
"Staubosphere" was a term coined by S. Cyril Blacktin during the dustbowl years of the 1930s. It refers to the dust content of the atmosphere. A more common term is "konisphere," which refers to the dust content in the lower atmosphere as measured by a koniscope or konimeter. A koniscope measures the optical properties of the atmosphere, then estimates the dust content. A konimeter actually samples the air and collects microscopic dust particles on a sticky film surface.

In the central plains states, dust content is clearly higher during prolonged drought periods and even briefly higher during spring tillage and planting, when soils are disturbed by tractors and associated implements like plows, chisels, disks, and cultivators.

storm surge, swash, and backwash
These terms all refer to actions of ocean waters as they erode shorelines and beaches. A storm surge is produced by the wind action of large storms such as hurricanes. They literally push water up on shore and inland beyond the limits of normal tidal actions. Swash is the action produced by waves as they intermittently break across shorelines and beaches, while backwash is the return flow of water back to the sea. The combined erosive effect of these actions can be quite destructive, depending on their intensity and duration. Because of its relatively slow movement, Hurricane Bonnie may produce long lasting erosive effects along North Carolina's seacoast.

This word refers to the pattern of air flow or wind moving horizontallly at a given level in the atmosphere. The lines on a weather map will run parallel to the wind direction, but they may form different patterns depending on which vertical level is being examined. For example the surface stream lines may look quite different from those depicted at the 500 mb level (say 18,000 ft aloft). The streamlines aloft earlier this week over Kentucky ran northwest to southeast.

Stuve Diagram
These diagrams are plots of radiosonde data, which are taken at 12 hour intervals by government weather services. They typically show the pattern of temperature, dewpoint, pressure, wind speed, and wind direction with height. Pilots find them useful in assessing how stable the atmosphere is, and what kinds of headwinds or tailwinds they might encounter. There are several Web sites on the Internet, where Stuve diagrams can be found for major cities in the United States, Canada, and Mexico including the following:
(University of Illinois Weather Visualizer)
(Northern Illinois University)
(University of Wyoming)
Sugar, Mashed Potato, Powder, White Asphalt
"Sugar," "mashed potato," "powder," and "white asphalt" are used by skiers to refer to different types of snow. Each term infers the skiability of slope conditions. Sugar snow is composed of crumbly ice crystals, while mashed potato snow is dense heavy snow so thick a shovel will stand up in it. I think sugar snow is relatively better for skiers. Powder snow is the dry, cold, powdery mix of ice crystals which Alpine skiers love. Though an ideal mix, it does not typically last very long, crusting or compressing as it ages. White asphalt is the subsurface, compacted layer which rests several inches to several feet underneath the powder or sugar snow on the surface.

This is a Russian word (pronounced sue-koo-vay) for the hot, dry winds that sometimes blow during their growing season. In the absence of sufficient soil moisture, these winds can rapidly lead to drought conditions and drastically reduce crop yields, up to 30 to 40 percent. Like the Corn Belt in America, the most critical time for poor weather to occur in Russia is in the month of July when most crops are blooming or heading out. The sukoveis brings temperatures of 80 and 90 degrees F, humidities less than 20 percent and winds from 10 to 20 mph, all of which last for several days. This causes rapid dessication of most plants. The agriculturally productive area of the Caspian plains is sometimes buffered from the effects of the sukoveis by the water available from the Volga River flood plain..

This term derives from swelter or sultry which refers to hot and humid weather conditions, making the air feel "close" or "oppressive." Forecasters may use the term when they are predicting high dew points, combinations of high temperature and high humidity. It is more commonly a term used in forecasting in the tropics, but certainly applied this week in Kentucky when our dew point temperatures rose into the 70s.

This is a term used to describe the reaction of some people (usually the elderly who suffer from forms of dementia) to the loss of sunlight in the late afternoon or evening. In some cases the loss of light triggers an agitated or confused state, or sometimes anxious and restless behaviors. There are a variety of explanations being offered for this but I am not aware of any consensus opinion. Like those who suffer from Seasonal Affective Disorder, some who suffer from sundowning are helped by photo therapy and being in rooms with bright lights.

Sun-glade or sun glint
Both of these terms refer to a type of bright reflection of the sun from the surface of a water body. This may be observed from an aircraft flying over a large lake, or even in visible weather satellite imagery. In fact sun glint seen in visible satellite imagery often appears as a large bright region over the tropical ocean areas. Small brighter spots of sun glint over otherwise dark ocean surfaces indicate relatively calm seas (glassy and smooth) with very light surface winds.

The SWEAT Index and Total-Totals Index
The SWEAT Index was derived by the Air Force, not for putting cadets through basic training but for indicating the potential for severe weather to pilots. The Severe Weather Threat (SWEAT) Index uses atmospheric stability, wind shear, and wind speeds aloft (taken from radiosonde reports). In general, the differences in temperature, dew point, and winds measured at the 850 mb and 500 mb levels of the atmosphere are considered in this index. Values of 250 or greater indicate a potential for severe weather. The SWEAT Index is not used as much as it used to be, as more sophisticated indices have taken its place. The Total-Totals Index is also used to assess the threat of severe weather. It also considers two different vertical layers in the atmosphere, 850 mb and 500 mb. The variables used are temperature and dew point. In general terms, this index is calculated by taking the sum of the temperature and dew point at 850 mb minus twice the temperature at 500 mb. Values of 55 or greater are considered strong indicators of severe weather potential. A glossary of terms used by meteorologists in dealing with severe weather can be found at a web site maintained by the National Severe Storms Laboratory in Norman, OK.

This is another term occasionally used by Scottish meteorologists to describe a gust of wind. It is derived partially from the Norwegian term sweel, which means to whirl around. A visiting Norwegian meteorologist may have very well passed this term on to the Scottish sometime in the past hundred years or so.

Tablecloth, Sansan, Cap Cloud, Crest Cloud, or Banner Cloud
These are either local or generic names for the same cloud form. "Crest," " cap," or "banner" is used to describe the standing cloud that forms across the peak of a mountain ridge. Uplifted air on the windward side reaches saturation forming a cloud over the mountain crest, while subsiding or downslope winds on the leeward side warm and dry out the air, causing sufficient evaporation to abruptly terminate the cloud form. Strong winds over a mountain peak may lead to a banner form (a cloud that looks like a white flag). In the Canadian Rockies this type of cloud is called a "sansan;" in Cape Town, South Africa, this type of cloud form is frequently seen (and photographed) over Table Mountain and is called the "Tablecloth."

"Taiga" is a Russian word (pronounced "ti-ga") used to refer to the Boreal woodlands or open forest which lies just south of the tundra in high latitudes. It consists of coniferous trees growing in cold and swampy soils occupied by lichens. In these areas, trees can grow for a limited time each year. The landscape is often flooded in the spring by north flowing rivers. Some climatologists refer to these areas as subarctic climates.

Talik or Tabetisol
These are Russian words, both used to refer to a layer of permanently unfrozen ground within regions of permafrost. Usually refers to a layer that lies above the permafrost, but these terms may also relate to layers of soil within or beneath the permafrost. Talik or tabetisol layers may vary from a few inches to several feet in thickness and support a number of micro- organisms which are tolerant to cold temperatures. These soils are usually found at fairly high latitudes.

This is the name (taken from the Latin word for Earth) given to the new NASA spacecraft which was launched in December 1999 with a mission focus to study the interactions of land, ocean and atmosphere. The Terra spacecraft, about the size of a school bus, orbits the Earth from pole to pole using multispectral sensors to capture images of land and water surfaces, as well as cloud formations in great detail. It is on a six year mission to provide earth systems scientists with data to study ocean currents and cycles, as well as surface temperature patterns, radiation budgets, and other features the Earth (including polar ice caps) which may provide some insights on global climate change.

More information on Terra can be found on the NASA web site at:

Tessellated clouds
Taken from the Latin word tessellatus, meaning to form as a mosaic from smaller squares or oblong shapes. These types of clouds are typically stratocumulus or cirro-cumulus layers which look like a patchwork in the sky, sometimes even a checkerboard. There were some present in the Twin Cities area on Tuesday of this week. Sometimes these cloud forms appear as a warm front approaches.

Thermal Equator
This is different from the geographic equator which circuscribes the Earth at 0 degrees latitude. The thermal equator is a line which circumscribes the Earth connecting all points of highest annual mean temperature. Its course varies with the continents and ocean currents and rarely runs parallel to the geographic equator. For example in the western hemisphere it ranges from nearly 20 degrees north latitude across Mexico to 14 degrees south latitude across parts of Brazil.

Thirl and Tirl
Both of these words are Scottish in origin, initially meaning to whirl, rotate, or spin, such as in a dance. Among Scottish meteorologists, these terms -- "thirl" (pronounced thurl) and "tirl" (pronounced turl) -- refer to a fresh, strong breeze. I suppose this is based on observations of the wind causing leaves to spin about across the ground. It is certainly not based on the wind causing people to spin about uncontrollably, which is called a gale! We have certainly experienced a good deal of strong wind in March, one of the windiest in recent memory.

This is not the kind used to smooth out new cement. This term is used by some Canadian meteorologists to refer to a tongue or wedge of warm air isolated aloft. This sometimes happens when a cold front overtakes a warm front (forming an occluded front), lifting the warmer air away from the surface. It is usually relatively short-lived, but shows up as an unusual layer of warm air on an upper air soundiing. Trowels sometimes signal the possibility of freezing rain or an ice storm, as the warm moist air aloft reaches saturation and precipitaites through a colder layer of air below, causing the droplets to become supercooled and freeze on impact with the Earth's surface. My recollection is that a trowel of warm air aloft contributed to the terrible ice storm over Northern New England and the St Lawrence River Valley last January that caused widespread power outages.

Twilight (including civil, nautical, and astronomical)
An enquiry from my adult evening class at the University prompted this selection. In simple terms twilight is the term used to describe the period of incomplete darkness that occurs after sunset and before sunrise. It is derived from Saxon or Middle English terms, which imply that it occurs twice daily. The British use the term crepuscule as well, which means a dim or faint light. With the sun below the horizon, the multiple scattering of light produced by constituents in the upper atmosphere may commonly produce a purple, red or yellow glow.

Three somewhat arbitrary subdivisions of twilight have been used historically to define outdoor visibility.

Civil twilight refers to the interval of incomplete darkness that occurs when the sun's center is approximately 6 degrees below the horizon. The amount of light is still sufficient to carry on outdoor work without the aid of artificial light.

Nautical twilight refers to the interval of incomplete darkness that occurs when the sun's center is approximately 12 degrees below the horizon. The amount of light is still sufficient to navigate using visible features on the surface of water or land.

Astronomical twilight refers to the interval of incomplete darkness that occurs when the sun's center is approximately 18 degrees below the horizon. There is no discernible horizon glow left over the sun's azimuth. Stars (sixth magnitude) directly overhead.

The duration of twilight varies considerably with latitude and season. The daily path of the sun across an observer's celestial sphere will be significantly different near the equator versus the poles for example. The rotational speed of the Earth and changing angles of the sun make it so. At the equator civil twilight my last only 21 minutes and vary little from season to season. At our latitude civil twilight may vary from 30 to 40 minutes, while at high latitudes civil twilight in the summer can literally last all night.

Tyndall Flowers (not botanical)
John Tyndall was an English physicist who studied the scattering of light as it passed through smokey air, mist, fog and ice. He noted the effects of the differential radiative absorption and scattering by ice.

A legacy of his work is the name given to small water-filled, hexagonally shaped cavities which appear in the interior of ice masses bathed in sunlight. These are called Tyndall flowers. They are formed when ice melts by radiative absorption at points of defect in the ice lattice. Occasionally, they may be seen through clear lake ice on bright sunny winter days in Kentucky.

UTC, GMT and Z time
By international agreement, all governmental weather services provide observational data and summaries at specified times during the day. Meteorological reports all follow the Universal Time Coordinated System (UTC), formally referred to as Greenwich Mean Time (GMT) or referenced often by the military as Z time, all meaning the clock time at the Prime Meridian of longitude located at zero degrees running through England. Instrumented balloon launches are done each day at 0000Z and 1200Z. This time is five hours ahead of Kentucky, so the National Weather Service balloon launches from Paducah are done at 7 am and 7 pm when it is not Daylight Saving Time. Surface weather observations are provided by all countries at 0000Z, 0600Z, 1200Z, and 1800Z. Incidentally, if you are ever interested in setting your clock to the precise time observed by the Master Clock at the U.S. Naval Observatory, you can go to their web site and see it at

Veering and Backing Winds
In meteorology, "veering" and "backing winds" are terms used to describe the manner in which winds are shifting or changing. In the northern hemisphere, a veering wind is one which shifts in a clockwise direction, while a backing wind is one which shifts in a counterclockwise manner. Low pressure systems which pass south of Kentucky tend to produce backing winds, while those that pass north of the state produce veering winds.

Ventifact and Dreikanter
These terms are used both in geology and climatology. Ventifact is taken from the Latin root words, ventus for wind, and factum meaning "to make." Like artifact (human-made), ventifact is the term used to refer to a stone or rock which has been sculptured by wind blown sediments. Its surface may appear worn, polished or multifaceted as a result of a sort of long term sandblasting effect. These types of stones or rocks are found in dry arctic climates, near glaciers, or in desert regions.

The dreikanter, a German term, refers to a three edged or three faceted type of ventifact. Exposed to wind blown sediments coming from different directions, the carving and sculpturing of the surface may give distinctly different appearances to the sides and edges of the stones.

Ventometer and Ventose
"Ventometer" and "ventose" are both old words. Before the use of the term "anemometer" to describe an instrument for measuring wind speed, several countries called this instrument a "ventometer," from the Latin words "ventus" meaning wind and "meter" for measure. For example, military history shows that a ventometer was used by the Italian and French military to measure wind velocity on their artillery target ranges during practice sessions.

The term "Ventose" dates from the Revolutionary Calendar devised by the First French Republic (1793) following the French Revolution. This calendar divided the year into 12 months, each 30 days long, with five additional days each year for festivals (six in every 4th year). Further, each month was divided into 3 ten day periods, with weeks being abolished. The year began on the autumnal equinox (Sept 22 or so). Ventose was the 6th month of the year, covering the period from February 19 to March 20, typically a windy period in France. Hence, the name derived from the Latin word for windy or flatulent (ventosus). To this day, the term ventosity refers to windiness, and is derogatory when describing a person who is too conceited or boastful.

This is a term used by meteorologists to describe the rotation of a fluid. An example is the rotation of the atmosphere (a gaseous fluid) around relatively large scale low and high pressure cells. It is most often used to describe the rotational field about a vertical axis, such as a surface low pressure system.

"Vorticity" is defined as positive if it rotates counterclockwise about a low pressure cell (storm system) in the northern hemisphere. Vorticity about a high pressure cell with clockwise rotation in the northern hemisphere is defined as negative.

This can be illustrated using the righthand rule. Hold out your righthand with the thumb pointed upward and curl your fingers slowly (they will rotate counterclockwise). This is an example of positive vorticity (with your thumb pointing upward), with your fingers pointed in the direction of the flow. Now place your righthand with your thumb pointed downward and slowly curl your fingers (they will rotate clockwise). This is an example of negative vorticity (your thumb pointed downwards), again with your fingers pointed in the direction of the flow.

A weather forecaster who describes the upstream weather pattern as having positive vorticity is referring to the approach of a storm (low pressure center and associated front), while the approach of negative vorticity usually brings high pressure and a more stable weather pattern. The relative strength of vorticity is sometimes observable in animated satellite views.

Vorticity is a standard calculation made by many numerical forecast models which helps meteorologists determine what the future three dimensional states of the atmosphere might look like, in time steps ranging from 3 hours out to 72 hours.

This term is an acronym for the World Area Forecast System, a worldwide satellite communications system sponsored by the World Meteorological Organization and the International Civil Aviation Organization. Its purpose is to provide critical weather analyses and products to national meteorological services, aviation authorities and airline operators. Gridded wind, pressure, and temperature fields are available from observational data, as are various upper air observations and satellite images.

"The Water Tower of Europe"
"The water tower of Europe" is a phrase used to describe the country of Switzerland, specifically the Swiss Alps which serve as a source region for many of Europe's great rivers. Many major watersheds in Germany, France, Austria, and Italy are fed by the spring and summer runoff from the Swiss Alps. These waters are vital to the European community in terms of hydroelectric power generation, agricultural and municipal water supply, and recreation.

Wind Profiler
This is a three beam Doppler Radar system aimed vertically to measure atmospheric winds at different altitudes over a station. These data provide forecasters with an atmospheric profile of wind so they can detect where wind shear (sharp changes in direction or speed) is occurring and the altitude of maximum wind speeds. This information aids in forecasting for aviation. There is a wind profiler system located at Wood Lake, MN west of the Twin Cities area.

Wind Ripple or Snow Ripple
These terms refer to a type of wave-like formation visible in the snow covered rural landscapes of western Kentucky in the winter. A series of small waves, about an inch high are observable running at right angles to the prevailing wind direction. These often occur several times over the course of a snow season if the land is undisturbed. They result more commonly from falls of light fluffy snow than heavier dense snow. There orientation in Kentucky is frequently from SW to NE due to the dominance of northwesterly winds in the winter time.

The strongest winds of March blew earlier this week on the 25th to the 27th, with many gusts between 40 and 50 mph. Exposure to such a wind, especially when the air is very dry, can lead to windburn. This is a superficial inflammation of the skin which appears somewhat like sunburn, but it is caused by exposure to dry winds which induce a dilation of the surface blood vessels in the skin. Windburn usually appears for shorter duration than sunburn. Sometimes dessication injury to landscape plants which is caused by strong, warm, and dry winds is also called windburn.

This is another scientific acronym and stands for the World Ocean Circulation Experiment, a multi-national research effort carried out under the World Climate Research Programme. The experiment essentially ended this summer, but it will take many years to analyze all of the data. Instrumented ships, buoys, and floats provided measurements of many physical and chemical characteristics related to ocean circulation patterns. In addition to meteorological measurements of atmospheric conditions, measurements were made of ocean temperature with depth, velocity of ocean currents, depth of mixing layers, salinity, oxygen, carbon dioxide, and other chemical constituents. These data will be used in conjunction with satellite data to better understand the interactions of ocean circulation patterns with the Earth climate system.

Those wishing to find out more details about this experiment and the available data sets can browse the National Oceanographic Data Center.

Woolpack or Cauliflower Cloud
These terms are old ones used to refer to some types of cloud formations, namely cirrocumulus (high cumulus) and altocumulus (mid-level cumulus). When these clouds are seen in abundance, they may have a fleecy appearance and look like an airborne flock of sheep or lambs. Seen in isolation, one of these clouds may have the appearance of a head of cauliflower. These terms were first used by 19th century British meteorologists Abercromby and Scott, who contributed to the first International Cloud Atlas published in 1896. These cloud forms are more frequent during the spring months in Kentucky, when it is fun to observe the wide variety of cloud formations.

Those readers wishing to learn more about clouds can consult two educational web sites which catalog the different cloud types:
(University of Illinois Atmospheric Sciences Dept project 2010)
(Plymouth State College Cloud Boutique page)

Who's escaping? Just kidding. This term is used to describe landscape planning and planting practices which strive to conserve water by mulching, using soil amendments like compost or manure, and by selecting species with low water requirements such that they can thrive on natural precipitation for the most part. This is not a common practice in Kentucky, but it has been tried in the drier climates of North Dakota, some of the western states, and especially the desert southwest. In some areas of the country over half of the residential water use goes to watering landscape plants and lawns. Xeriscaping has been shown to reduce water usage by up to 70 percent in some cases. The USDA and National Weather Service conducted a joint meeting in Washington D.C. to discuss drought strategies for the coming growing season in the United States. This was done with an awareness that more of the U. S. landscape is in drought or at least a dry weather pattern this winter than any other winter since that of 1987-88. Xeriscaping was one of the major topics on the agenda for this week's meeting, so we may see this practice being promoted more in parts of the country this year.

This is an old Scottish term, perhaps a derivative of yowt which means to scream or howl. Anyway it is a term for snow that is driven by the wind, such as in a blizzard. I suspect it would have been appropriately used to describe the weather on Wednesday of this week in the Red River Valley, where up to 4 inches of snow fell, followed by strong northwesterly winds.

Zenith, Nadir, and the Celestial Sphere
"Zenith," "nadir," and the "celestial sphere" are terms used by meteorologists, climatologists, and other scientists with reference to astronomical positions. They are derived from ancient terms used to refer to heaven and hell. The celestial sphere is the apparent or imaginary sphere, of infinite radius, with the Earth at its center. Thus, any person standing on Earth can see one half of the celestial sphere when they look from one horizon across the sky overhead to the other horizon.

In this context, directly above the observer is the zenith, or the highest point in the heavens. The term "zenith" is often used in other ways; for example, to say that a musician or athlete is at the zenith of their career would mean that they are at peak performance or productivity. Conversely, the nadir is the point directly below the observer in the celestial sphere, exactly opposite of the zenith. The term "nadir" is also used to describe when an individual or organization is at an all-time low in terms of performance or productivity.

Zonal and Meridional
Meteorologists will often use the terms "zonal" and "meridonial" to describe the upper level wind patterns which indicate the trajectory of air masses and weather systems. "Zonal" refers to a wind flow pattern which runs along parallels of latitude (that is easterly or westerly). For our midwest region, zonal would refer to a west to east flow trajectory, which is associated with a somewhat moderate or quiet weather pattern and not much change in air mass. "Meridional" refers to a wind flow pattern which runs parallel to meridians of longitude (that is southerly or northerly). This pattern brings large changes in air mass and very active weather systems to our midwest region, with oscillating southerly and northerly winds every few days.