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Titlebook: Geophysical Fluid Dynamics; Joseph Pedlosky Book 19791st edition Springer Science+Business Media New York 1979 Dissipation.dynamics.fluid

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书目名称Geophysical Fluid Dynamics
编辑Joseph Pedlosky
视频video
丛书名称Springer Study Edition
图书封面Titlebook: Geophysical Fluid Dynamics;  Joseph Pedlosky Book 19791st edition Springer Science+Business Media New York 1979 Dissipation.dynamics.fluid
描述The content of this book is based, largely, on the core curriculum in geophys­ ical fluid dynamics which I and 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 ach
出版日期Book 19791st edition
关键词Dissipation; dynamics; fluid dynamics; fluid- and aerodynamics
版次1
doihttps://doi.org/10.1007/978-1-4684-0071-7
isbn_ebook978-1-4684-0071-7Series ISSN 0172-6234
issn_series 0172-6234
copyrightSpringer Science+Business Media New York 1979
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Ageostrophic Motion,., that the scaling of the motion is isotropic horizontally. The low-frequency Kelvin wave is not horizontally isotropic, since its offshore scale is the deformation radius, which for low frequencies is small compared with the wavelength. In this chapter we consider some of the refinements to quasig
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https://doi.org/10.1007/978-3-642-50943-8s of years, the surface expression of which is sea-floor spreading and continental drift. All these phenomena can properly be included within the domain of geophysical fluid dynamics. Partly for historical reasons, however, the subject has tended to focus on the dynamics of large-scale phenomena in
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https://doi.org/10.1007/978-3-642-25794-0the persistent but spatially nonuniform solar heating. This input of energy produces a mechanical response, i.e., kinetic energy of the large-scale motion, and eventually this must be dissipated if a steady state—or at least a statistically stable average state of motion—is to be maintained. This re
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0172-6234 s 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 ach978-1-4684-0071-7Series ISSN 0172-6234
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