AOU as indicator of water-flow direction in the central North Pacific

SaÚlAlvarez-Borrego; P.Kilho Park

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AOU as indicator of water-flow direction in the central North Pacific

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Salinity, preformed phosphate and AOU distribution on the sigma-tsurfaces of 26.8 and 27.3 of the central North Pacific Ocean, as well as the topography of these density surfaces, were studied. The direction of water flow suggested by the AOU distribution on these density surfaces was compared to that indicated by the acceleration potential contours on theδt=125 cl/ton andδt=80cl/ton surfaces drawn by Joseph L.Reid, Jr. The disagreements were explained in terms of mixing and possible gradients of primary production at the sea surface. On the 26.8 sigma-tsurface a southward flow connecting the westward flow south of the Aleutian chain and the eastward flow farther south, between 175‡E and 180‡ is suggested by the AOU distribution but is not implied by the acceleration potential contours. If the circulation pattern at this density surface is similar to that at the sea surface, this southward flow is very likely to be

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《日本海洋学会誌》 |2005年第4期|142-151|共页
作者
SaÚlAlvarez-Borrego; P.Kilho Park;
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作者单位

Oregon State University;

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收录信息美国《科学引文索引》(SCI);
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正文语种英语
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AOU as indicator of water-flow direction in the central North Pacific

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