Titlebook: Geophysical Fluid Dynamics II; Stratified / Rotatin Emin ?zsoy Textbook 2021 Springer Nature Switzerland AG 2021 Coastal Seas.Geophysical F

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




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




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




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




書目名稱Geophysical Fluid Dynamics II被引頻次




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




書目名稱Geophysical Fluid Dynamics II年度引用




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




書目名稱Geophysical Fluid Dynamics II讀者反饋




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

cyanosis

Textbook 2021erning equations for a stratified fluid starting from basic principles of physics..2. review of thermodynamics, equations of state, isothermal, adiabatic, isentropic changes..3. scaling of the equations, Boussinesq approximation, applied to the ocean and the atmosphere..4. examples of stratified flo

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癡呆

https://doi.org/10.1007/978-3-030-74934-7Coastal Seas; Geophysical Fluid Dynamics; Internal Waves; Inertio-Gravity Waves; Quasi-Geostrophic Dynam

瑪瑙

https://doi.org/10.1007/978-3-662-00601-6Continuity and momentum equations were developed in the first volume GFD-I.

挫敗

Die Abh?ngigkeit der Felder vom BezugssystemContinuity and momentum equations (.), (.) applied to inhomogenous fluids were introduced in Chapter

挫敗

裝勇敢地做

Engpassmanagement und Allokationssignale,Having developed basic theory of stratified geophysical flows in Chap.?1, perturbations around basic states of the atmosphere and ocean have been considered in Chap.?2. Quasi-geostrophic equations of motion have been developed and applied to the ocean and atmosphere in Chap.?3.

offense

,Z?hler für besondere Verwendungszwecke,Introductory theory of fluid dynamics applied to homogeneous density fluids reviewed?in GFD-I have been extended to stratified ones in the present volume.

irritation

,Z?hler für besondere Verwendungszwecke,We present a much idealized theory of jets and plumes in this chapter. Jet flows are very similar to boundary layers considered in the last chapter. Free jets and wakes can be created away from solid boundaries by a momentum source, while buoyant plumes involve effects of density.