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A simplified model of the Martian atmosphere -- Part 2: a POD-Galerkin analysis

Abstract:

In Part I of this study Whitehouse et al. (2005) performed a diagnostic analysis of a simplied model of the Martian atmosphere, in which topography was absent and in which heating was modelled as Newtonian relaxation towards a zonally symmetric equilibrium temperature field. There we derived a reduced-order approximation to the vertical and the horizonal structure of the baroclinically unstable Martian atmosphere, retaining only the barotropic mode and the leading order baroclinic modes. Our ...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Publisher's version

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Institution:
University of Oxford
Department:
Mathematical,Physical & Life Sciences Division - Mathematical Institute
Role:
Author
More by this author
Institution:
University of Oxford
Department:
Mathematical,Physical & Life Sciences Division - Physics - Atmospheric,Oceanic and Planetary Physics
Role:
Author
More by this author
Institution:
University of Oxford
Department:
Mathematical,Physical & Life Sciences Division - Mathematical Institute
Role:
Author
More by this author
Institution:
University of Oxford
Research group:
Geophysical and Planetary Fluid Dynamics group
Oxford college:
Trinity College
Department:
Mathematical,Physical & Life Sciences Division - Physics - Atmospheric,Oceanic and Planetary Physics
Role:
Author
Publisher:
European Geosciences Union Publisher's website
Journal:
Nonlinear Processes in Geophysics Journal website
Volume:
12
Issue:
5
Pages:
625-642
Publication date:
2005-06-05
EISSN:
1607-7946
ISSN:
1023-5809
URN:
uuid:64e8a802-0694-46e4-902a-cb00b45c3dd4
Local pid:
ora:2926

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