Abstract
The characteristics of a boundary layer depend both on conditions at the surface and in the interior of the medium. In the undisturbed tropics, the latter are largely determined by subsidence and by infrared radiational cooling. One-dimensional models are used to establish relationships between the inversion height, subsidence, upper-air humidity and sea-surface temperature. In particular, it is shown that a universally colder tropical ocean would probably be covered by more extensive clouds.
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Contribution No. 1700 Rosenstiel School of Marine and Atmospheric Science, University of Miami.
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Kraus, E.B., Hanson, H.P. Climatological aspects of the tropical convective boundary layer. Boundary-Layer Meteorol 6, 219–233 (1974). https://doi.org/10.1007/BF00232486
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DOI: https://doi.org/10.1007/BF00232486