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.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 2001 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
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
Download citation
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
eBook Packages: Springer Book Archive