Where f _ 0 is the Coriolis parameter, approximated by the constant 1e " 4 s " 1; R is the atmospheric ideal gas constant; \ beta is the latitudinal change in the Coriolis parameter \ beta = \ frac { \ partial f } { \ partial y }; \ sigma is a static stability parameter; c _ p is the specific heat at constant pressure; p is pressure; T is temperature; anything with a subscript g indicates geostrophic; anything with a subscript a indicates ageostrophic; J is a diabatic heating rate; and \ omega is the Lagrangian rate change of pressure with time . \ omega = \ frac { Dp } { Dt }.
32.
Where f _ 0 is the Coriolis parameter, approximated by the constant 1e " 4 s " 1; R is the atmospheric ideal gas constant; \ beta is the latitudinal change in the Coriolis parameter \ beta = \ frac { \ partial f } { \ partial y }; \ sigma is a static stability parameter; c _ p is the specific heat at constant pressure; p is pressure; T is temperature; anything with a subscript g indicates geostrophic; anything with a subscript a indicates ageostrophic; J is a diabatic heating rate; and \ omega is the Lagrangian rate change of pressure with time . \ omega = \ frac { Dp } { Dt }.
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