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The next-order corrections to quasigeostrophic theory

Journal Article · · Journal of the Atmospheric Sciences
 [1]; ;  [2]
  1. New York Univ., NY (United States). Courant Inst.
  2. National Center for Atmospheric Research, Boulder, CO (United States)
Quasigeostrophic theory is an approximation of the primitive equations in which the dynamics of geostrophically balanced motions are described by the advection of potential vorticity. Quasigeostrophy also represents a leading-order theory in the sense that it is derivable from the full primitive equations in the asymptotic limit of zero Rossby number. Building upon quasigeostrophy, and the centrality of potential vorticity, a systematic asymptotic framework is developed from which balanced, next-order corrections in Rossby number are obtained. The simplicity of the approach is illustrated by explicit construction of the next-order corrections to a finite-amplitude Eady edge wave.
Sponsoring Organization:
USDOE, Washington, DC (United States)
DOE Contract Number:
FG02-88ER25053
OSTI ID:
355576
Journal Information:
Journal of the Atmospheric Sciences, Journal Name: Journal of the Atmospheric Sciences Journal Issue: 11 Vol. 56; ISSN 0022-4928; ISSN JAHSAK
Country of Publication:
United States
Language:
English

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