An estimation of the mass dragged by the solar wind from Marss atmosphere in its geologic history
In the past Mars had a denser atmosphere, but it lacks a magnetic field to protect the ionosphere and exosphere from the solarwind. A model for describing the loss of atmosphere in geologic time is presented. The amount of volatiles degassed from Marswas in the order of 193.7 Terrestrial Atmospheric...
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| Udgivet i: | Geofísica Internacional |
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| Hovedforfatter: | |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Universidad Nacional Autónoma de México
2001
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| Online adgang: | https://www.redalyc.org/articulo.oa?id=56840408 |
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