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Titlebook: Geophysical Fluid Dynamics; Joseph Pedlosky Book 1982 Springer Science+Business Media New York 1982 Potential.circulation.dynamics.fluid d

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书目名称Geophysical Fluid Dynamics
编辑Joseph Pedlosky
视频videohttp://file.papertrans.cn/384/383892/383892.mp4
丛书名称Springer Study Edition
图书封面Titlebook: Geophysical Fluid Dynamics;  Joseph Pedlosky Book 1982 Springer Science+Business Media New York 1982 Potential.circulation.dynamics.fluid d
描述The content of this book is based, largely, on the core curriculum in geophys­ ical fluid dynamics which land my colleagues in the Department of Geophysical Sciences at The University of Chicago have taught for the past decade. Our purpose in developing a core curriculum was to provide to advanced undergraduates and entering graduate students a coherent and systematic introduction to the theory of geophysical fluid dynamics. The curriculum and the outline of this book were devised to form a sequence of courses of roughly one and a half academic years (five academic quarters) in length. The goal of the sequence is to help the student rapidly advance to the point where independent study and research are practical expectations. It quickly became apparent that several topics (e. g. , some aspects of potential theory) usually thought of as forming the foundations of a fluid-dynamics curriculum were merely classical rather than essential and could be, however sadly, dispensed with for our purposes. At the same time, the diversity of interests of our students is so great that no curriculum can truly be exhaust­ ive in such a curriculum period. It seems to me that the best that can be achi
出版日期Book 1982
关键词Potential; circulation; dynamics; fluid dynamics; stability; fluid- and aerodynamics
版次1
doihttps://doi.org/10.1007/978-3-662-25730-2
isbn_softcover978-3-540-90745-9
isbn_ebook978-3-662-25730-2Series ISSN 0172-6234
issn_series 0172-6234
copyrightSpringer Science+Business Media New York 1982
The information of publication is updating

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https://doi.org/10.1007/978-3-663-04792-6eral pattern of the oceanic circulation began to emerge. It is clear now that a time-averaged circulation pattern exists in all oceans, although its observations may be significantly distorted by the presence of energetic fluctuations.
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Inviscid Shallow-Water Theory,mework adequate for the calculation of motions of large time and space scales. Furthermore, the method of analysis to be presented also can be generalized to the study of thermodynamically active fluids. The key technique of the analysis is the formulation of a . approximation scheme in which the geostrophic approximation is merely the first step.
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Book 1982ysical Sciences at The University of Chicago have taught for the past decade. Our purpose in developing a core curriculum was to provide to advanced undergraduates and entering graduate students a coherent and systematic introduction to the theory of geophysical fluid dynamics. The curriculum and th
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https://doi.org/10.1007/978-3-7091-7776-1ical motion and strongly affects the nature of the dynamics. It is also clear from the discussion in Section 2.9 that the vertical structure of the winds and currents is directly related to the presence and strength of horizontal density gradients by the thermal wind relation.
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