Abstract
The net heat gain of the ocean is determined by summing the fluxes of shortwave (SR) and longwave radiation (LR) and the turbulent fluxes of sensible (H) and latent heat (LE) at the sea surface.
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© 2001 Springer-Verlag Berlin Heidelberg
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Lindau, R. (2001). Net Air-Sea Heat Flux and Meridional Heat Transport. In: Climate Atlas of the Atlantic Ocean. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-59526-4_4
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DOI: https://doi.org/10.1007/978-3-642-59526-4_4
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-64009-4
Online ISBN: 978-3-642-59526-4
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