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• W1517201703 abstract "This chapter discusses fundamentals of rotating shallow water model in the geophysical fluid dynamics perspective. The oceans and the atmosphere are thin stratified fluid layers on the rotating sphere with variable bottom topography under the influence of gravity. The effects of sphericity depend on the horizontal scale of the motions of interest. Although the vertical motions may be of considerable intensity in the oceans and the atmosphere such as deep convection, on the synoptic scale average the typical horizontal velocities are at least two orders of magnitude larger than the vertical ones. The chapter reviews some of the shallow-water literature." @default.
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• W1517201703 date "2007-01-01" @default.
• W1517201703 modified "2023-09-26" @default.
• W1517201703 title "Chapter 1 Introduction: Fundamentals of Rotating Shallow Water Model in the Geophysical Fluid Dynamics Perspective" @default.
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• W1517201703 doi "https://doi.org/10.1016/s1574-6909(06)02001-6" @default.
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