Answer:
Explanation:
Below are the given quantities:
Environmental lapse rate (\Gamma ) = 6 K/km
Dry adiabatic lapse rate (\Gammad) = 4 K/km for 12-km atmosphere, 2 K/km for 6-km atmosphere
Surface temperature (T) = 300 K
When we integrating the vertical momentum equation and assume that density is compensated by temperature, we have;
w.(dw/dz) = - \rho ' / \rho g = -[T ' - \Gammadz - (T ' - \Gamma d dz)] g
w2 / 2 = ( \Gamma - \Gamma d / T ) gdz
For 6-km layer atmosphere,
w= (2 [(6 - 2) / 300] (10 / 6000) )1/2 = 0.0066 m/s
For 12-km atmosphere,
w= (2 [(6 - 4) / 300] (10 / 12000) )1/2 = 0.0033 m/s
Thus, we can say that the 6-km deep environment is having a greater w than 12-km deep environment.
b. The Convective Available Potential Energy (CAPE) will be computed as
((T - Te ) / Te ) gdz
We have this has the potential energy which is also equivalent to kinetic energy of the parcel, meaning. 1 / 2 w2, maximum vertical velocity can be computed like;
1 / 2 w2 = CAPE
Thus, w = (2 CAPE) 1/2