Static Stability of the Atmosphere
•
G
e =
environmental lapse rate
•
G
d =
dry adiabatic lapse rate
•
G
m = moist adiabatic lapse rate
•
•
Absolutely Stable
•
G
e <
G
m
•
Absolutely Unstable
•
G
e >
G
d
•
Conditionally Unstable
•
G
m <
G
e <
G
d
(from
Meteorology Today)