Description
The seasonal deposition of CO2 on the polar caps is one of the most dynamic processes on Mars and is a dominant driver of the global climate. Remote sensing temperature and albedo data were used to estimate the subliming mass of CO2 ice on south polar gullies near Sisyphi Cavi. Results showed that column mass abundances range from 400 - 1000 kg.m2 in an area less than 60 km2 in late winter.
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Contributors
- Mount, Christopher (Author)
- Christensen, Philip R. (Thesis advisor)
- Desch, Steven J (Committee member)
- Bell, James F. (Committee member)
- Clarke, Amanda B (Committee member)
- Whipple, Kelin X (Committee member)
- Arizona State University (Publisher)
Date Created
The date the item was original created (prior to any relationship with the ASU Digital Repositories.)
2019
Resource Type
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Note
- Doctoral Dissertation Geological Sciences 2019