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

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書目名稱Geophysical Fluid Dynamics影響因子(影響力)




書目名稱Geophysical Fluid Dynamics影響因子(影響力)學(xué)科排名




書目名稱Geophysical Fluid Dynamics網(wǎng)絡(luò)公開度




書目名稱Geophysical Fluid Dynamics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Geophysical Fluid Dynamics被引頻次




書目名稱Geophysical Fluid Dynamics被引頻次學(xué)科排名




書目名稱Geophysical Fluid Dynamics年度引用




書目名稱Geophysical Fluid Dynamics年度引用學(xué)科排名




書目名稱Geophysical Fluid Dynamics讀者反饋




書目名稱Geophysical Fluid Dynamics讀者反饋學(xué)科排名

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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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