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Titlebook: Dynamic Meteorology; Lectures Delivered a P. Morel Book 1973 D. Reidel Publishing Company, Dordrecht, Holland 1973 Meteorology.Orbit.Scale.

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發(fā)表于 2025-3-21 20:00:07 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Dynamic Meteorology
副標題Lectures Delivered a
編輯P. Morel
視頻videohttp://file.papertrans.cn/284/283642/283642.mp4
圖書封面Titlebook: Dynamic Meteorology; Lectures Delivered a P. Morel Book 1973 D. Reidel Publishing Company, Dordrecht, Holland 1973 Meteorology.Orbit.Scale.
描述The development of numerical integration techniques and the pioneering efforts of Von Neumann and his associates at the Institute for Advanced Studies (Princeton) have spurred the renewed interest of many leading fluid dynamicists and meteorologists in the theory and numerical simulation of planetary atmosphere and oceans circulations. Their work during the last 15 years, now culminating in the Global Atmospheric Research Program, has led to the possibility of vastly improved weather forecasts as wei I as the development of a ful I fledged branch of the physical sciences: geophysical fluid dynamics. Simultaneously, great strides have been made in developing new instruments, operating from earth orbiting satel I ites, to powerful observe the meteorological phenomena and to determine the state of motion of the atmosphere. Centre National d‘Etudes Spatiales (CNES) of France has very significantly contributed to this effort by developing the EOLE navigation and data collection satell ite, launched on 16 August 1971 to interrogate 500 instrumented platforms measuring meteorological para- meters. It is fitting then, that CNES should have brought together lead- ing scientists in the field
出版日期Book 1973
關鍵詞Meteorology; Orbit; Scale; atmosphere
版次1
doihttps://doi.org/10.1007/978-94-010-2599-7
isbn_softcover978-94-010-2601-7
isbn_ebook978-94-010-2599-7
copyrightD. Reidel Publishing Company, Dordrecht, Holland 1973
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Planetary Fluid Dynamics,ed. Such motions have properties which are not to be found in nonrotating systems. For example, the action of external forces such as gravity invariably bring into being Coriolis forces which in turn produce circulatory motions. If a stone is thrown into an infinite resting ocean, the gravitational
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Lectures in Sub-Synoptic Scales of Motion and Two-Dimensional Turbulence,y on many scales combined with long term statistical order are just about what one would expect to observe if he were, say, an ant dwelling amongst the eddies of a turbulent pipe flow. Until recently, however, little use has been made of this sort of analogy except in the case of the surface boundar
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Space and Time Meteorological Data Analysis and Initialization, specified state of motion at some initial time t.. The previous speakers, particularly Professor PHILLIPS, showed that this initial value problem is approximately solved by replacing the continuous meteorological fields by a finite set of discrete values and integrating numerically the correspondin
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978-94-010-2601-7D. Reidel Publishing Company, Dordrecht, Holland 1973
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Orarat Mongkolporn,Paul W. J. Taylorto the forces, the thermodynamic law relating the rate of change of internal energy to the rate of heating, the principle of conservation of mass, the thermodynamic state relations, detailed mathematical formulations of the forces and rates of heating, and, finally, appropriate conditions at the bou
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