Titlebook: Dynamics of the Equatorial Ocean; John P. Boyd Book 2018 Springer-Verlag GmbH Germany 2018 El Nino/Southern Oscillation.Coastally Trapped

Taft

書目名稱Dynamics of the Equatorial Ocean影響因子(影響力)




書目名稱Dynamics of the Equatorial Ocean影響因子(影響力)學科排名




書目名稱Dynamics of the Equatorial Ocean網(wǎng)絡(luò)公開度




書目名稱Dynamics of the Equatorial Ocean網(wǎng)絡(luò)公開度學科排名




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書目名稱Dynamics of the Equatorial Ocean被引頻次學科排名




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書目名稱Dynamics of the Equatorial Ocean年度引用學科排名




書目名稱Dynamics of the Equatorial Ocean讀者反饋




書目名稱Dynamics of the Equatorial Ocean讀者反饋學科排名

山崩

crucial

GRATE

,The “Long Wave” Approximation & Geostrophy,t that has been extremely useful in low latitude dynamics. The “l(fā)ong wave” approximation, which might equally well be dubbed the “l(fā)ow frequency” or “meridional geostrophy” approximation, filters gravity waves while retaining Kelvin and Rossby waves. The key assumption is that there is geostrophic ba

Emg827

菊花

Response of the Equatorial Ocean to Periodic Forcing, the theory of the ocean response to a periodically-varying wind stress. Special emphasis is given to low frequency forcing and the use of the low frequency/meridional geostrophy approximation to analyze it.

菊花

Impulsive Forcing and Spin-Up,be formally solved by Laplace transform integrals (multiplied by the usual Hermite functions). Although these transform integrals must evaluated numerically, it is still possible to analyze the oceanic response to jumps in the wind. The work of Anderson and Rowlands (J Mar Res 34(3):295–312, 1976) [

intertwine

Yoshida Jet and Theories of the Undercurrent,he f-plane and then on the equatorial plane. In contrast to the midlatitudes where the steady-state flow is a geostrophically balanced jet . to the wind, Yoshida showed, through an infinite Hermite series with explicit, analytical coefficients, that a zonal wind stress would yield a zonal equatorial

要素

Stratified Models of Mean Currents,tion theorists. In this chapter, stratification and viscosity are added to the shallow water jets found by Yoshida. The models of McCreary and McPhaden are ancient and cannot fit observations as well as the ever-changing succession of ocean general circulation models. Yet they are well worth a caref

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