Comparing the linear and nonlinear buoyancy-driven circulation
The buoyancy-driven circulation is studied in an idealized domain using two models, one based on the linearized planetary geostrophic equations and a fully nonlinear GCM. The surface buoyancy is specified (relaxed) to a chosen function of latitude in the linear (nonlinear) model. The models yield si...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Stockholm University Press
2017-01-01
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Series: | Tellus: Series A, Dynamic Meteorology and Oceanography |
Subjects: | |
Online Access: | http://dx.doi.org/10.1080/16000870.2017.1299282 |