An estimation of the mass dragged by the solar wind from Mars’s 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 solar wind. A model for describing the loss of atmosphere in geologic time is presented. The amount of volatiles degassed from Mars was in the order of 193.7 Terrestrial Atmospher...
| Váldodahkki: | |
|---|---|
| Materiálatiipa: | Artihkal |
| Giella: | English |
| Almmustuhtton: |
Universidad Nacional Autónoma de México, Instituto de Geofísica
2001-06-01
|
| Ráidu: | Geofísica Internacional |
| Fáttát: | |
| Liŋkkat: | http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2001/04/durand2.pdf |