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Dynamics of the Equatorial Ocean

  • Book
  • © 2018

Overview

  • 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 differences between the phenomenon in different latitudes

  • Includes supplementary material: sn.pub/extras

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Table of contents (17 chapters)

Keywords

About this book

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.

Authors and Affiliations

  • CLaSP Department, University of Michigan College of Engineering, Ann Arbor, USA

    John P. Boyd

Bibliographic Information

  • Book Title: Dynamics of the Equatorial Ocean

  • Authors: John P. Boyd

  • DOI: https://doi.org/10.1007/978-3-662-55476-0

  • Publisher: Springer Berlin, Heidelberg

  • eBook Packages: Earth and Environmental Science, Earth and Environmental Science (R0)

  • Copyright Information: Springer-Verlag GmbH Germany 2018

  • Hardcover ISBN: 978-3-662-55474-6Published: 06 October 2017

  • Softcover ISBN: 978-3-662-57235-1Published: 15 August 2018

  • eBook ISBN: 978-3-662-55476-0Published: 25 September 2017

  • Edition Number: 1

  • Number of Pages: XXIV, 517

  • Number of Illustrations: 132 b/w illustrations, 27 illustrations in colour

  • Topics: Oceanography, Geophysics/Geodesy, Climatology

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