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John Marshall, David Ferreira, J-M. Campin, and Daniel Enderton

zonal-average residual momentum balance in the two fluids that can be written as Integrate from the surface, where τ = τ s and τ e = 0, across the planetary boundary layers of the two fluids to where τ = 0, neglecting Reynolds stress processes in both fluids, we obtain the following: Adding the two together we find where Ψ A res = ρ A ψ A res and Ψ O res = ρ O ψ O res are the mass transports in the two fluids. We now consider two limit cases. In the mid–high-latitude atmosphere, the

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