Science, Volume 291John Michels (Journalist) American Association for the Advancement of Science, 2001 |
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Page 2588
... observed topography but overpredicts the magnitudes of the associated gravity anoma- lies . Because we are interested primarily in the spatial correlation of models to observed Tharsis rise mGal 300 200 100 -100 -200 -300 Fig . 1 ...
... observed topography but overpredicts the magnitudes of the associated gravity anoma- lies . Because we are interested primarily in the spatial correlation of models to observed Tharsis rise mGal 300 200 100 -100 -200 -300 Fig . 1 ...
Page 2589
... Observed martian topography displayed for ( A ) the Tharsis and ( B ) the anti - Tharsis hemispheres compared with modeled topography ( to = 120 ) for ( C ) the Tharsis and ( D ) the anti - Tharsis hemispheres . For the model , actual ...
... Observed martian topography displayed for ( A ) the Tharsis and ( B ) the anti - Tharsis hemispheres compared with modeled topography ( to = 120 ) for ( C ) the Tharsis and ( D ) the anti - Tharsis hemispheres . For the model , actual ...
Page 2590
... observed topography is shown in the Tharsis region . Pole - to - pole slope has been included in the topographic model , which has been referenced to the observed geoid . Role of the Stratospheric Polar Freezing Belt in Denitrification ...
... observed topography is shown in the Tharsis region . Pole - to - pole slope has been included in the topographic model , which has been referenced to the observed geoid . Role of the Stratospheric Polar Freezing Belt in Denitrification ...
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