The Lowest Mode of Oceanic ConvectionSource: Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 001::page 183Author:Assaf, Gad
DOI: 10.1175/1520-0485(1975)005<0183:TLMOOC>2.0.CO;2Publisher: American Meteorological Society
Abstract: The assumption that the Antarctic polar front is a quasi-material frontal surface that separates the Antarctic from the warm ocean gives an estimate of 8 cm per year of upwelling and 0.4 cm2 s?1 of vertical diffusivity in the world thermocline.
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| contributor author | Assaf, Gad | |
| date accessioned | 2017-06-09T14:44:03Z | |
| date available | 2017-06-09T14:44:03Z | |
| date copyright | 1975/01/01 | |
| date issued | 1975 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25496.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162285 | |
| description abstract | The assumption that the Antarctic polar front is a quasi-material frontal surface that separates the Antarctic from the warm ocean gives an estimate of 8 cm per year of upwelling and 0.4 cm2 s?1 of vertical diffusivity in the world thermocline. | |
| publisher | American Meteorological Society | |
| title | The Lowest Mode of Oceanic Convection | |
| type | Journal Paper | |
| journal volume | 5 | |
| journal issue | 1 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1975)005<0183:TLMOOC>2.0.CO;2 | |
| journal fristpage | 183 | |
| journal lastpage | 185 | |
| tree | Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 001 | |
| contenttype | Fulltext |