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

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书目名称Dynamics of the Equatorial Ocean
编辑John P. Boyd
视频video
概述Contains appendices for illustrating special cases.Treats the important semiannual and annual cycles in the tropic sea.Includes complementary information to assist the reader in understanding the diff
图书封面Titlebook: Dynamics of the Equatorial Ocean;  John P. Boyd Book 2018 Springer-Verlag GmbH Germany 2018 El Nino/Southern Oscillation.Coastally Trapped
描述.This book is the first comprehensive introduction to the theory of equatorially-confined waves and currents in the ocean. Among the topics treated are inertial and shear instabilities, wave generation by coastal reflection, semiannual and annual cycles in the tropic sea, transient equatorial waves, vertically-propagating beams, equatorial Ekman layers, the Yoshida jet model, generation of coastal Kelvin waves from equatorial waves by reflection, Rossby solitary waves, and Kelvin frontogenesis. A series of appendices on midlatitude theories for waves, jets and wave reflections add further material to assist the reader in understanding the differences between the same phenomenon in the equatorial zone versus higher latitudes. .
出版日期Book 2018
关键词El Nino/Southern Oscillation; Coastally Trapped Waves; Equatorial Ocean; Nonlinear EquatorialWaves; Deep
版次1
doihttps://doi.org/10.1007/978-3-662-55476-0
isbn_softcover978-3-662-57235-1
isbn_ebook978-3-662-55476-0
copyrightSpringer-Verlag GmbH Germany 2018
The information of publication is updating

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