Abstract
It is well recognized that successful modeling of seasonal and long term climate variability requires a good representation of atmosphere-ocean heat exchange, as well as oceanic heat storage and transport. This has motivated the analysis of the main elements of heat transfer in the ocean during the last decades. In this review we look at heat transfer and formation of Warm Water Mass (WWM) in the eastern North Atlantic Subtropical Gyre (NASG), approximately between Cape Vert (15°N) and the Strait of Gibraltar (36°N) and between the African coast and 30°W.
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© 1997 Springer-Verlag Berlin Heidelberg
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Pelegrí, J.L., Sangrà, P., Hernández-Guerra, A. (1997). Heat Gain in the Eastern North Atlantic Subtropical Gyre. In: Díaz, J.I. (eds) The Mathematics of Models for Climatology and Environment. NATO ASI Series, vol 48. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-60603-8_14
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