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If the base of atmospheric layer is saturated, but the top of the layer is very dry because the layer is stably stratified. Find an expression for the height the layer must be lifted (Az) for the layer to become conditionally unstable. Your solution must be of the form Δz = f (ΔΖι, Γs, Γα, Γο) where Azi is the depth of the air layer, To is the initial lapse rate of the layer, and Is and la are the moist and dry adiabatic lapse rates, respectively.

If the base of atmospheric layer is saturated, but the top of the layer is very dry because the layer is stably stratified. Find an expression for the height the layer must be lifted (Az) for the layer to become conditionally unstable. Your solution must be of the form Δz = f (ΔΖι, Γs, Γα, Γο) where Azi is the depth of the air layer, To is the initial lapse rate of the layer, and Is and la are the moist and dry adiabatic lapse rates, respectively.

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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If the base of atmospheric layer is saturated, but the top of the layer is very dry because the layer is stably stratified. Find an expression for the height the layer must be lifted (Az) for the layer to become conditionally unstable. Your solution must be of the form Az = f (Azi, s, [d, [o) where Az is the depth of the air layer, To is the initial lapse rate of the layer, and I, and I are the moist and dry adiabatic lapse rates, respectively.
Transcribed Image Text:If the base of atmospheric layer is saturated, but the top of the layer is very dry because the layer is stably stratified. Find an expression for the height the layer must be lifted (Az) for the layer to become conditionally unstable. Your solution must be of the form Az = f (Azi, s, [d, [o) where Az is the depth of the air layer, To is the initial lapse rate of the layer, and I, and I are the moist and dry adiabatic lapse rates, respectively.
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