Near‐pure vapor condensation in the Martian atmosphere: CO<sub>2</sub> ice crystal growth

Constantino Listowski(Centre National de la Recherche Scientifique), F. Lefèvre(Centre National de la Recherche Scientifique), Anni Määttänen(Centre National de la Recherche Scientifique), I. Riipinen(Stockholm University), Franck Montmessin(Centre National de la Recherche Scientifique)
Journal of Geophysical Research Planets
September 7, 2013
10.1002/jgre.20149
Cited by 17

Related Papers

Formation of Glaciers on Mars by Atmospheric Precipitation at High Obliquity
|Science|2006|480
Origin and role of water ice clouds in the Martian water cycle as inferred from a general circulation model
|Journal of Geophysical Research Atmospheres|2004|381
Amazonian northern mid-latitude glaciation on Mars: A proposed climate scenario
|Icarus|2009|298
The atmosphere of Mars as observed by InSight
|Nature Geoscience|2020|264
Density and temperatures of the upper Martian atmosphere measured by stellar occultations with Mars Express SPICAM
|Journal of Geophysical Research Atmospheres|2009|259