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Titlebook: Poleward Flows Along Eastern Ocean Boundaries; S. J. Neshyba,Ch. N. K. Mooers,R. T. Barber Book 1989 Springer-Verlag New York, Inc. 1989 A

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書目名稱Poleward Flows Along Eastern Ocean Boundaries
編輯S. J. Neshyba,Ch. N. K. Mooers,R. T. Barber
視頻videohttp://file.papertrans.cn/750/749797/749797.mp4
叢書名稱Coastal and Estuarine Studies
圖書封面Titlebook: Poleward Flows Along Eastern Ocean Boundaries;  S. J. Neshyba,Ch. N. K. Mooers,R. T. Barber Book 1989 Springer-Verlag New York, Inc. 1989 A
描述In this paper differences and anomalies in west coast seasonal flow structures have been highlighted. In particular, it was emphasized that flow off Washington has significant differences from that of Oregon; namely, during summer, flow at mid-shelf is more poleward off Washington, and during winter, flow on the inner-shelf is more equatorward off Washington than off Oregon. The former result may be related to the poleward decrease in the longshelf wind stress; the latter result may be related to the presence of the Columbia River plume. Off southern California the near-surface flow over the shelf is more persistently equatorward than that off Washington . Conversely, the flow over the slope in the upper 100 m of the water column is more persistently poleward than that off washington. Also, the undercurrent structure, that is, a subsurface maximum, is maintained at least from summer to early winter off southern California (no data are yet available from spring), but only during summer and early fall off washington. We note that the seasonal cycle of vertical shear in the two locations is similar, although a reversal in sign sometimes occurs off Washington. ACKNOWLEDGEMZNTS This wor
出版日期Book 1989
關(guān)鍵詞Atlantic Ocean; Coast; Indian Ocean; Meere; Meeresbiologie; Ozeanographie; Pacific Ocean; biology; marine bi
版次1
doihttps://doi.org/10.1007/978-1-4613-8963-7
isbn_softcover978-1-4613-8965-1
isbn_ebook978-1-4613-8963-7Series ISSN 0724-5890
issn_series 0724-5890
copyrightSpringer-Verlag New York, Inc. 1989
The information of publication is updating

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