An Estimation of Oceanic Thermal-Sublayer ThicknessSource: Journal of Physical Oceanography:;1971:;Volume( 001 ):;issue: 004::page 284Author:Wu, Jin
DOI: 10.1175/1520-0485(1971)001<0284:AEOOTS>2.0.CO;2Publisher: American Meteorological Society
Abstract: The thickness of the oceanic thermal layer is considered to be one-half of the viscous-sublayer thickness, which decreases as the wind velocity increases. The thermal-layer thickness is estimated to be between 4 and 0.25 mm for light winds and between 0.25 and 0.1 mm for strong winds.
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| contributor author | Wu, Jin | |
| date accessioned | 2017-06-09T14:43:31Z | |
| date available | 2017-06-09T14:43:31Z | |
| date copyright | 1971/10/01 | |
| date issued | 1971 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25281.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162047 | |
| description abstract | The thickness of the oceanic thermal layer is considered to be one-half of the viscous-sublayer thickness, which decreases as the wind velocity increases. The thermal-layer thickness is estimated to be between 4 and 0.25 mm for light winds and between 0.25 and 0.1 mm for strong winds. | |
| publisher | American Meteorological Society | |
| title | An Estimation of Oceanic Thermal-Sublayer Thickness | |
| type | Journal Paper | |
| journal volume | 1 | |
| journal issue | 4 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1971)001<0284:AEOOTS>2.0.CO;2 | |
| journal fristpage | 284 | |
| journal lastpage | 286 | |
| tree | Journal of Physical Oceanography:;1971:;Volume( 001 ):;issue: 004 | |
| contenttype | Fulltext |