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contributor authorLiu, Zhengyu
date accessioned2017-06-09T14:41:54Z
date available2017-06-09T14:41:54Z
date copyright1997/03/01
date issued1997
identifier issn0003-0007
identifier otherams-24718.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161421
description abstractA coupled theory is proposed to account for the magnitude of the Walker circulation in the tropical Pacific. It is suggested that the Pacific Walker circulation is at a saturation state, at which the zonal sea surface temperature difference is bounded by about a quarter of the latitudinal difference of the radiative?convective equilibrium sea surface temperature.
publisherAmerican Meteorological Society
titleOceanic Regulation of the Atmospheric Walker Circulation
typeJournal Paper
journal volume78
journal issue3
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/1520-0477(1997)078<0407:OROTAW>2.0.CO;2
journal fristpage407
journal lastpage412
treeBulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 003
contenttypeFulltext


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