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

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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被引頻次學科排名




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書目名稱Geophysical Fluid Dynamics讀者反饋學科排名

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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