Titlebook: Atmospheric Tidal and Planetary Waves; Hans Volland Book 1988 Kluwer Academic Publishers 1988 Scale.Southern Oscillation.Storm.Tide.wind

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書目名稱Atmospheric Tidal and Planetary Waves影響因子(影響力)




書目名稱Atmospheric Tidal and Planetary Waves影響因子(影響力)學(xué)科排名




書目名稱Atmospheric Tidal and Planetary Waves網(wǎng)絡(luò)公開度




書目名稱Atmospheric Tidal and Planetary Waves網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Atmospheric Tidal and Planetary Waves被引頻次




書目名稱Atmospheric Tidal and Planetary Waves被引頻次學(xué)科排名




書目名稱Atmospheric Tidal and Planetary Waves年度引用




書目名稱Atmospheric Tidal and Planetary Waves年度引用學(xué)科排名




書目名稱Atmospheric Tidal and Planetary Waves讀者反饋




書目名稱Atmospheric Tidal and Planetary Waves讀者反饋學(xué)科排名

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https://doi.org/10.1007/978-94-007-7091-1at the equations of motion can be solved by separation of the variables (latitude, longitude, height, and time) and that the modal structure becomes an eigenvalue problem. In this chapter, we will discuss the eigenvalues of the individual modes and their horizontal structures.

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Horizontal Modal Structure,at the equations of motion can be solved by separation of the variables (latitude, longitude, height, and time) and that the modal structure becomes an eigenvalue problem. In this chapter, we will discuss the eigenvalues of the individual modes and their horizontal structures.

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GRILL

Book 1988 indicates the preferred prejudice of many ionospheric physicists and geomagneticians in those days toward meteorology as a descriptive rather than an exact science, in spite of the presence of such giants as Carl Rossby and Hans Ertel.

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Internal Energy Sources and Sinks,bypass these difficulties by introducing secondary or internal ‘sources’ (or ‘sinks’). These internal sources are intended to parameterize the otherwise neglected processes like turbulence, latent heat, feedback between ground and atmosphere, etc.

explicit

Nonlinear Wave Propagation,e types with mixed frequencies. Such interference cannot be described by the linear approximation. We want to estimate in this chapter the influence of the nonlinear terms in the wave equations on the excitation and propagation of global-scale waves.