Tropical Atmosphere-Ocean Interactions
he oceans that most directly affects the atmosphere is the sea surface temperature, which affects the upward longwave radiation, the sensible heat flux, and the latent heat flux. The roughness of the sea surface can also affect the efficiency of near-surface turbulent exchange. The albedo of the oce...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.36.8355 2023-05-15T18:17:34+02:00 Tropical Atmosphere-Ocean Interactions Copyright David David A. Randall The Pennsylvania State University CiteSeerX Archives 2000 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.36.8355 http://kiwi.atmos.colostate.edu/group/dave/at605pdf/AT605_Ch_9.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.36.8355 http://kiwi.atmos.colostate.edu/group/dave/at605pdf/AT605_Ch_9.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://kiwi.atmos.colostate.edu/group/dave/at605pdf/AT605_Ch_9.pdf text 2000 ftciteseerx 2016-01-08T00:47:12Z he oceans that most directly affects the atmosphere is the sea surface temperature, which affects the upward longwave radiation, the sensible heat flux, and the latent heat flux. The roughness of the sea surface can also affect the efficiency of near-surface turbulent exchange. The albedo of the ocean is determined in part by the turbidity of the near-surface water, and of course by sea ice, where present. Sea ice also affects the sensible and latent heat fluxes, by presenting to the air a surface which can be much colder than the sea water below; and it can affect the atmospheric turbulence through its roughness and the presence of leads and other breaks in the ice. Many properties of the atmospheric column can affect the ocean. These include the near-surface temperature, which influences sensible heat exchange and downward long wave radiation; the near-surface humidity which influences latent heat exchange and downward longwave radiation;, and cloudiness, which can affect the surface Text Sea ice Unknown |
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ftciteseerx |
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English |
description |
he oceans that most directly affects the atmosphere is the sea surface temperature, which affects the upward longwave radiation, the sensible heat flux, and the latent heat flux. The roughness of the sea surface can also affect the efficiency of near-surface turbulent exchange. The albedo of the ocean is determined in part by the turbidity of the near-surface water, and of course by sea ice, where present. Sea ice also affects the sensible and latent heat fluxes, by presenting to the air a surface which can be much colder than the sea water below; and it can affect the atmospheric turbulence through its roughness and the presence of leads and other breaks in the ice. Many properties of the atmospheric column can affect the ocean. These include the near-surface temperature, which influences sensible heat exchange and downward long wave radiation; the near-surface humidity which influences latent heat exchange and downward longwave radiation;, and cloudiness, which can affect the surface |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Copyright David David A. Randall |
spellingShingle |
Copyright David David A. Randall Tropical Atmosphere-Ocean Interactions |
author_facet |
Copyright David David A. Randall |
author_sort |
Copyright David |
title |
Tropical Atmosphere-Ocean Interactions |
title_short |
Tropical Atmosphere-Ocean Interactions |
title_full |
Tropical Atmosphere-Ocean Interactions |
title_fullStr |
Tropical Atmosphere-Ocean Interactions |
title_full_unstemmed |
Tropical Atmosphere-Ocean Interactions |
title_sort |
tropical atmosphere-ocean interactions |
publishDate |
2000 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.36.8355 http://kiwi.atmos.colostate.edu/group/dave/at605pdf/AT605_Ch_9.pdf |
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Sea ice |
genre_facet |
Sea ice |
op_source |
http://kiwi.atmos.colostate.edu/group/dave/at605pdf/AT605_Ch_9.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.36.8355 http://kiwi.atmos.colostate.edu/group/dave/at605pdf/AT605_Ch_9.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766191921948000256 |