HIGH-ALTITUDE CO2 CLOUDS ON MARS: OMEGA AND HRSC OBSERVATIONS. A. Määttänen 1, F.

Introduction: The Martian climate hosts a rare phenomenon of condensation of the bulk atmosphere. CO2 condenses on the polar ice caps, but also forms clouds in the atmosphere. The existence of low-level, convective CO2 clouds in the polar night was

Bibliographic Details
Main Authors: B. Gondet, H. Hoffmann, F. Scholten, E. Hauber, F. Gonzalez-galindo, F. Forget, J. -p, J. -l. Bertaux, G. Neukum
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
polar night
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.184.2039
http://www.lpi.usra.edu/meetings/mpeb2009/pdf/7023.pdf
Description
Summary:Introduction: The Martian climate hosts a rare phenomenon of condensation of the bulk atmosphere. CO2 condenses on the polar ice caps, but also forms clouds in the atmosphere. The existence of low-level, convective CO2 clouds in the polar night was

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