Gravity wave drag in a global circulation model of the Martian atmosphere: Parameterisation and validation
The effect of orographically generated breaking gravity waves is parametrised in a global circulation model of the Martian atmosphere using schemes adapted from terrestrial models. The schemes are 'tuned' by comparing model integrations with and without gravity wave drag with temperatures...
Príomhchruthaitheoirí: | Collins, M, Lewis, SR, Read, P |
---|---|
Formáid: | Conference item |
Foilsithe / Cruthaithe: |
1997
|
Míreanna comhchosúla
Míreanna comhchosúla
-
Baroclinic wave transitions in the Martian atmosphere
de réir: Collins, M, et al.
Foilsithe / Cruthaithe: (1996) -
Martian atmospheric data assimilation with a simplified general circulation model: Orbiter and lander networks
de réir: Lewis, SR, et al.
Foilsithe / Cruthaithe: (1996) -
Martian atmospheric data assimilation with a simplified general circulation model: Orbiter and lander networks
de réir: Lewis, SR, et al.
Foilsithe / Cruthaithe: (1996) -
Sensitivity of the Freie Universität Berlin Climate Middle Atmosphere Model (FUB-CMAM) to different gravity-wave drag parameterisations
de réir: P. Mieth, et al.
Foilsithe / Cruthaithe: (2004-09-01) -
Equatorial jets in the dusty Martian atmosphere
de réir: Lewis, SR, et al.
Foilsithe / Cruthaithe: (2003)