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To accomplish this, we use a number of computer models. The simplest of these represents the atmosphere by a vertical column stretching up from the surface to some specified height. This model simulates effects such as atmospheric heating by gases and ground-air heat transfer.
The most complex is a 3 dimensional (height, latitude, longitude) model, which represents the processes in the simpler model, as well as large-scale atmospheric motions. The latter is called a GCM (General Circulation Model), and is similar in a lot of ways to the computer models that are used for weather prediction on the Earth.
Visit the links below to learn more about various characteristics of Mars. Mars' low
surface pressure ...or what happens when the atmosphere is so thin? |
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Responsible NASA Official: Robert
Haberle
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Last Updated: 08/29/04
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Designed by: James Schilling
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