Abstract
Following on from the global energy balance described in the previous chapter, latitudinal energy balance is considered here. The energy balance of a zonally and vertically averaged atmosphere is described using the latitude-dependent energy balance model. The pole-to-equator temperature difference is evaluated with the energy balance model in which meridional heat transport is modeled using a diffusion coefficient. The latitudinal profiles of radiative fluxes and their balance are also described using the energy balance model. Furthermore, the possibility of multiple equilibrium states is investigated using the relation between solar flux and albedo. In the final section, a constraint on the latitudinal distribution of water vapor is argued using the balance of the latitudinal transport of water vapor.
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Satoh, M. (2014). Latitudinal energy balance. In: Atmospheric Circulation Dynamics and General Circulation Models. Springer Praxis Books(). Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-13574-3_13
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DOI: https://doi.org/10.1007/978-3-642-13574-3_13
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