Wave dispersion in a rotating, differentially-heated fluid model
Author:
Publisher
Elsevier BV
Subject
Atmospheric Science,Computers in Earth Sciences,Geology,Oceanography
Reference31 articles.
1. Transition to geostrophic turbulence in a rotating differentially heated annulus of fluid;Buzyna;J. Fluid Mech.,1984
2. Downstream development of baroclinic waves as inferred from regression analysis;Chang;J. Atmos. Sci.,1993
3. Nonlinear baroclinic instability of a continuous zonal flow of viscous fluid;Drazin;J. Fluid Mech.,1972
4. On the change in the spectral distribution of kinetic energy for two-dimensional, non-divergent flow;Fjörtoft;Tellus,1953
5. Thermal convection in a rotating fluid subject to a horizontal temperature gradient: spatial and temporal characteristics of fully developed baroclinic waves;Hide;J. Atmos. Sci.,1977
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1. Primary Flow Transitions in the Baroclinic Annulus;Modeling Atmospheric and Oceanic Flows;2014-11-14
2. The influence of a sloping bottom endwall on the linear stability in the thermally driven baroclinic annulus with a free surface;Theoretical and Computational Fluid Dynamics;2012-10-31
3. Mixed-mode solutions in an air-filled differentially heated rotating annulus;Physica D: Nonlinear Phenomena;2010-10
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