Oceans and Atmospheres

  • Andrew Fowler
Part of the Interdisciplinary Applied Mathematics book series (IAM, volume 36)


Chapter 3 deals with a selection of phenomena in classical GFD. The first part of the chapter is largely bound up with the derivation of the quasi-geostrophic potential vorticity equation in the troposphere, following Pedlosky’s derivation, but in addition providing a self-consistent recipe for the determination of the stratification parameter. The interesting possibility of atmospheric overturn arises as a consequence. The chapter concludes with discussion of some oceanic topics, in particular western boundary currents and the tides.


Gravity Wave Rossby Wave Planetary Boundary Layer Short Wave Radiation Thermal Boundary Condition 
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© Springer-Verlag London Limited 2011

Authors and Affiliations

  1. 1.MACSI, Department of Mathematics & StatisticsUniversity of LimerickLimerickIreland

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