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contributor authorAssaf, Gad
date accessioned2017-06-09T14:44:03Z
date available2017-06-09T14:44:03Z
date copyright1975/01/01
date issued1975
identifier issn0022-3670
identifier otherams-25496.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162285
description abstractThe 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.
publisherAmerican Meteorological Society
titleThe Lowest Mode of Oceanic Convection
typeJournal Paper
journal volume5
journal issue1
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1975)005<0183:TLMOOC>2.0.CO;2
journal fristpage183
journal lastpage185
treeJournal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 001
contenttypeFulltext


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