METEOROLOGIST JEFF HABY
1. What is TT?
The TT (Total Totals) is an index used to assess storm strength.
2. How is TT determined?
The TT is a combination of the Vertical Totals (VT) and Cross Totals (CT). The VT is the temperature difference
between 850 and 500 mb while the CT is 850 mb dewpoint minus the 500 mb temperature.
TT = (T850 - T500) + (Td850 - T500)
The equation above for the TT is stating (850 mb temperature minus 500 mb temperature) plus (850 mb dewpoint
minus 500 mb temperature)
The Skew-T below gives a TT value of 44 for that sounding. Here is how that number was determined:
850 mb Temperature = 20 C
500 mb Temperature = -7.5 C
850 mb Dewpoint = 9 C
TT = (20 - (-7.5)) + (9 - (-7.5)) = 27.5 + 16.5 = 44
3. Operational significance of TT:
|<44 ||Convection not likely||44-50 ||Likely thunderstorms
||51-52 ||Isolated severe storms
||53-56 ||Widely scattered severe
||>56 ||Scattered severe storms
a. TT does not assess wind shear and
CAPE directly. See CAPE
and shear environment to see how relevant
index is for severe storms.
b. May not pick up a capping inversion that prevents storms from developing.
c. Index will be too stable if a layer of moisture is just under the 850 mb level.
d. VT may be very high and contributes to causing a high TT even when moisture is lacking. Index will be
too unstable in these situations.
e. Works best for flat areas in low to moderate elevations. Does not work for high elevations.
f. Index value interpretation varies with season and location.