Dry, unstable air increases the probability that wild land fires will become large and/or erratic. The index here provides an atmospheric reference, Lower Atmosphere Severity Index (LASI), for these fires, based on the environmental lapse rate of a layer of air coupled with its moisture content.
LASI = a(Tp1 - Tp2) + b(Tp - Tdp)
First, select the proper index variant based on surface elevation. There are three categories according to the station altitude.
i) If the station is at a low elevation (<= 500 m), A is computed by
(A) 950mb T(C degree) - 850mb T(C degree) factor value:
less than 4: 1
4 to 8: 2
greater than/equal to 8: 3
and B is computed by:
(B) 850mb T(c degree) - 850mb Tdp(c degree) factor values:
less than 6: 1
6 to 10: 2
greater than/equal to 10: 3
ii) If the station is at a middle elevation (500m ~ 1500m), A is computed by
(A) 850mb T(C degree) - 700mb T(C degree) factor values:
less than 6: 1
6 to 11: 2
greater than/equal 11: 3
and B is computed by
(B) 850mb T(c degree) - 850mb Tdp(c degree) factor values:
less than 6: 1
6 to 13: 2
greater than/equal to 13: 3
iii) If the station is at a high elevation (>= 1500m), A is computed by
(A) 700mb T(C degree) - 500mb T(C degree) factor values:
less than 18: 1
18 to 22: 2
greater than/equal to 22: 3
B is computed by
(B) 700mb T(c degree) - 700mb Tdp(c degree) factor values:
less than 15: 1
15 to 21: 2
greater than/equal to 21: 3
Second, add the factor values (A + B)
(A + B) Class of day (potential for large fire)
2 or 3 very low
4 low
5 moderate
6 high