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Titlebook: Meteorological Fluid Dynamics; Asymptotic Modelling Radyadour K. Zeytounian Book 1991 Springer-Verlag Berlin Heidelberg 1991 Navier-Stokes

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書目名稱Meteorological Fluid Dynamics
副標(biāo)題Asymptotic Modelling
編輯Radyadour K. Zeytounian
視頻videohttp://file.papertrans.cn/632/631785/631785.mp4
叢書名稱Lecture Notes in Physics Monographs
圖書封面Titlebook: Meteorological Fluid Dynamics; Asymptotic Modelling Radyadour K. Zeytounian Book 1991 Springer-Verlag Berlin Heidelberg 1991 Navier-Stokes
描述.The author considers meteorology as a part of fluid dynamics. He tries to derive the properties of atmospheric flows from a rational analysis of the Navier-Stokes equations, at the same time analyzing various types of initial and boundary problems. This approach to simulate nature by models from fluid dynamics will be of interest to both scientists and students of physics and theoretical meteorology..
出版日期Book 1991
關(guān)鍵詞Navier-Stokes equation; Navier-Stokes equations; dynamics; fluid dynamics; meteorology; physics; fluid- an
版次1
doihttps://doi.org/10.1007/978-3-540-38386-4
isbn_softcover978-3-662-13842-7
isbn_ebook978-3-540-38386-4Series ISSN 0940-7677
issn_series 0940-7677
copyrightSpringer-Verlag Berlin Heidelberg 1991
The information of publication is updating

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Deterministic Chaotic Behaviour of Atmospheric Motions,small-scale) modes are strongly damped due to frictional force and dissipation function and only replicate with decreased amplitude the fundamental modes of oscillation (in particular, they have the same kind of spectrum).
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Book 1991Navier-Stokes equations, at the same time analyzing various types of initial and boundary problems. This approach to simulate nature by models from fluid dynamics will be of interest to both scientists and students of physics and theoretical meteorology..
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https://doi.org/10.1007/978-3-540-38386-4Navier-Stokes equation; Navier-Stokes equations; dynamics; fluid dynamics; meteorology; physics; fluid- an
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Dynamical and Thermodynamical Equations for Atmospheric Motions,In a coordinate frame rotating with the earth the momentum equations is ., where, . is the velocity vector as observed in the earth frame and ., is the material (or convective) derivative.
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Filtering of Internal Waves,We have already noted that the basic model equations (see, the Chapter II) are formulated a view to . out of the solutions of “exact” equations for atmospheric motions, because such waves are of ..
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