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Titlebook: Ocean Circulation Theory; Joseph Pedlosky Book 1996 Springer-Verlag Berlin Heidelberg 1996 Equatorial Currents.Ocean.Ocean Circulation.Oce

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书目名称Ocean Circulation Theory
编辑Joseph Pedlosky
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概述Careful synthesis of modern theories hitherto scattered in the literature - A vast amount of material collected and interpreted pedagogically
图书封面Titlebook: Ocean Circulation Theory;  Joseph Pedlosky Book 1996 Springer-Verlag Berlin Heidelberg 1996 Equatorial Currents.Ocean.Ocean Circulation.Oce
描述The waters of the earth are gathered in shallow, irregular, interconnecting basins. Heated by the sun and driven by the wind, the oceans circulate endlessly. The general circulation of the ocean is the persistent pattern of this flow on the scale of the basins. It is the heart and soul of physical oceanography, and the explanation and prediction of the flow from the principles of fluid dynamics is the chief goal of the physical oceanographer. Along with the pattern of the motion, the associated fields of pressure, temperature, salinity, and density are also necessary components of a complete theory for the ocean circulation since they are dynamically linked to the motion of the oceans. The physical problem posed by the general circulation of the oceans is a difficult one both experimentally and theoretically. From the point of view of theoretical fluid mechanics the difficulty springs fundamentally from the recirculating character of the circulation. The fluid is gathered into a single, though highly contorted basin.
出版日期Book 1996
关键词Equatorial Currents; Ocean; Ocean Circulation; Oceanic Gyres; Ozeanzirkulation; Scale; Äquatorialströmunge
版次1
doihttps://doi.org/10.1007/978-3-662-03204-6
isbn_softcover978-3-642-08224-5
isbn_ebook978-3-662-03204-6
copyrightSpringer-Verlag Berlin Heidelberg 1996
The information of publication is updating

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yThe waters of the earth are gathered in shallow, irregular, interconnecting basins. Heated by the sun and driven by the wind, the oceans circulate endlessly. The general circulation of the ocean is the persistent pattern of this flow on the scale of the basins. It is the heart and soul of physical
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Book 1996f the oceans is a difficult one both experimentally and theoretically. From the point of view of theoretical fluid mechanics the difficulty springs fundamentally from the recirculating character of the circulation. The fluid is gathered into a single, though highly contorted basin.
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er bodies, such as radioactive, organic, and inorganic chemical contaminants, heavy metals, biological (microbial) contamination, and pollutants from organic and inorganic nutrient exposures. The introduction of this substance into aquatic environments poses negative effects that hamper the water qu
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Joseph Pedloskyance. These activities include dredging, sand filling, coastal development, and industrialization. The ever-increasing population in coastal areas has also led to the reclamation of swamps and water bodies to build houses to accommodate more people migrating from rural to urban areas. The management
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