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    Zonally Symmetric Response to Atmospheric Tidal Forcing in the Dusty Martian Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 018:;page 2469
    Author(s): Zurek, Richard W.; Haberle, Robert M.
    Publisher: American Meteorological Society
    Abstract: We have computed a steady state, zonally symmetric response of an atmospheric circulation to the combined efffects of the very large zonal-mean diabatic heating and thermotidal forcing thought to exist in the dusty Martian ...
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    The Martian Zonal-Mean Circulation: Angular Momentum and Potential Vorticity Structure in GCM Simulations 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 021:;page 3143
    Author(s): Barnes, Jeffrey R.; Haberle, Robert M.
    Publisher: American Meteorological Society
    Abstract: Analysis of simulations performed with the NASA/Ames Mars GCM shows that under dusty conditions the Northern Hemisphere winter solstice circulation becomes characterized by a zonally averaged state in which the potential ...
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    A Boundary-Layer Model for Mars: Comparison with Viking Lander and Entry Data 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 011:;page 1544
    Author(s): Haberle, Robert M.; Houben, Howard C.; Hertenstein, Rolf; Herdtle, Tomas
    Publisher: American Meteorological Society
    Abstract: A one-dimensional boundary-layer model for Mars is described, and its results are compared with Viking data. The model equations are similar to Earth boundary-layer models in that they include contributions from Coriolis, ...
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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