Issue |
A&A
Volume 490, Number 2, November I 2008
|
|
---|---|---|
Page(s) | L11 - L14 | |
Section | Letters | |
DOI | https://doi.org/10.1051/0004-6361:200810530 | |
Published online | 23 September 2008 |
Letter to the Editor
Prograde and retrograde atmospheric rotation of cloud-covered terrestrial planets*
Significance of astronomical parameters in the middle atmosphere
1
Research Institute for Applied Mechanics, Kyushu University, 6-1 Kasugakouen, Kasuga 816-8580, Japan e-mail: yamakatu@riam.kyushu-u.ac.jp
2
Center for Climate System Research, University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa 277-8568, Japan e-mail: masaaki@ccsr.u-tokyo.ac.jp
Received:
7
July
2008
Accepted:
19
September
2008
Context. Cloud-covered middle-atmospheric dynamics are important in the strong prograde rotation (i.e. superrotation) observed in some terrestrial-planet atmospheres, such as Venus and Titan. In addition, the unified theory and the mechanism driving the general circulation could be extended to as yet unknown extrasolar Earth-sized habitable planet atmospheres.
Aims. We elucidate the dynamical process controlling prograde and retrograde atmospheric rotation induced by cloud heating in the middle atmosphere of terrestrial planets.
Methods. The terrestrial middle-atmospheric circulation is examined using a general circulation model in which astronomical parameters are varied.
Results. Middle-atmospheric circulation is strongly controlled by seasonal variation of the meridional circulation. Prograde and retrograde atmospheric rotation is determined by the direction of vertical angular momentum transport due to the meridional circulation resulting from tilting of the planetary rotation axis. The retrograde rotation rate is limited to for slowly rotating planets (where Ω is the planetary rotation rate).
Key words: hydrodynamics / Earth / planets and satellites: individual: Titan, Venus
© ESO, 2008
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