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Titlebook: General Circulation of the Ocean; Henry D. I. Abarbanel,W. R. Young Book 1987 Springer-Verlag New York Inc. 1987 Atlantic Ocean.Coast.Diss

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书目名称General Circulation of the Ocean
编辑Henry D. I. Abarbanel,W. R. Young
视频video
丛书名称Topics in Atmospheric and Oceanic Sciences
图书封面Titlebook: General Circulation of the Ocean;  Henry D. I. Abarbanel,W. R. Young Book 1987 Springer-Verlag New York Inc. 1987 Atlantic Ocean.Coast.Diss
描述The ocean has entranced mankind for as long as we have gazed upon it, traversed it, dived into it, and studied it. It remains ever changing and seemingly never changing. Each wave that progresses through the. imme­ diate surf zone on every coast is strikingly different, yet the waves come again and again, as if never to end. The seasons come with essential reg­ ularity, and· yet each is individual-whatever did happen to that year of the normal rainfall or tidal behavior? This fascination with the currents of the ocean has always had a most immediate practical aspect: shipping, transportation, commerce, and war have depended upon our knowledge, when we had it, and floundered on our surprising ignorance more often than we wish to reflect. These important practical issues have commanded attention from commercial, academic, and military research scientists and engineers from the earliest era of organized scientific investigation. The matter of direct and insistent investigation was from the outset the behavior of ocean currents with long time scales; namely, those varying on annual or at least seasonal cycles. Planning for all the named enterprises depended, as they still do, of course
出版日期Book 1987
关键词Atlantic Ocean; Coast; Dissipation; Ocean; Potential; Scale; wind; fluid- and aerodynamics
版次1
doihttps://doi.org/10.1007/978-1-4612-4636-7
isbn_softcover978-1-4612-9093-3
isbn_ebook978-1-4612-4636-7Series ISSN 1431-9314
issn_series 1431-9314
copyrightSpringer-Verlag New York Inc. 1987
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Thermocline Theories,The main objective of thermocline theory is to explain the phenomenon of the strong, vertical temperature gradient in relatively shallow water (200 – 800 m) where the transition occurs from the ocean’s surface temperature to the colder, more uniform waters of the abyss.
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Coastal Sedimentary Environmentsrepresent the upper thermocline waters rather than the full depth of the ocean, is used throughout. The emphasis is on interior solutions and the role of mesoscale eddies. Western boundary layers, which close the flow patterns, are ignored. This heavily idealized model is a convenient expository veh
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R. M. Browne,J. P. Mercer,M. J. Duncanuggested that the latitudinal variation of the Coriolis parameter so strongly constrained ocean flows that a great deal could be learned about them by isolating horizontal processes in a single layer model of the circulation and thus having to solve only two dimensional rather than three dimensional
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Herman G. Gade,Anton Edwards,Harald Svendsenrstanding general ocean circulation. The first is from a 1912 National Geographic Magazine article by Capt. John Elliott Pillsbury, U.S.C.G. a pioneer in measuring ocean currents from moored ships in the latter part of the 19th Century.
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