pvE dz dA

(using hydrostatic balance to replace pdz by -dp/p) where ps is surface pressure. It turns out that the kinetic energy component of the net transport is negligible (typically less than 1% of the total), so we only need to consider the first three terms in Eq. 8-14.

Let us first consider energy transport in the tropics by the Hadley circulation which (in the annual mean) has equatorward flow in the lower troposphere and poleward flow in the upper troposphere. We may write

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