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Original Articles

On the cooling of the sea surface by evaporation and heat exchange

Pages 363-366 | Received 29 Apr 1963, Published online: 15 Dec 2016
 

Abstract

Differences between surface and subsurface water-temperature are caused by evaporation, long-wave radiation and exchange of sensible heat. The relative importance of these three components is discussed, especially with aid of observations under neutral conditions. Evaporation as well as back radiation contributes to a cooling of the surface of 0.1 to 0.2 centigrade under neutral conditions, while under diabatic conditions greater surface temperature deviations are caused by heat exchange.DOI: 10.1111/j.2153-3490.1963.tb01399.x