Stability of the Atmosphere

Total Totals Index (TT)

The Total Totals Index consists of two components, the Vertical Totals (VT) and the Cross Totals (CT). The VT represents static stability or the lapse rate between 850 and 500 mb. The CT includes the 850 mb dewpoint. As a result, TT accounts for both static stability and 850 mb moisture, but would be unrepresentative in situations where the low-level moisture resides below the 850 mb level. In addition, convection may be inhibited despite a high TT value if a significant capping inversion is present.

    TT = VT + CT
    VT = T(850 mb) - T(500 mb)
    CT = Td(850 mb) - T(500 mb)

in degrees C, where T represents temperature at the indicated level and Td represents dewpoint temperature.

VT = 40 is close to dry adiabatic for the 850-500 mb layer. However, VT generally will be much less, with values around 26 or more representing sufficient static instability (without regard to moisture) for thunderstorm occurrence. CT > 18 often is necessary for convection, but it is the combined Total Totals Index that is most important.

     TT = T(850 mb) + Td(850 mb) - 2[T(500 mb)]      in degrees C.

TT = 45 to 50: Thunderstorms possible.
TT = 50 to 55: Thunderstorms more likely, possibly severe.
TT = 55 to 60: Severe thunderstorms most likely.

Source: NWS

Other UKAWC Stability Indices:
Lifted Index (LI) K-Index CIN Showalter Index SWEAT Total Totals

Ag Weather Center, Department of Biosystems & Agricultural Engineering, University of Kentucky