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The early Martian atmosphere: Investigating the role of the dust cycle in the possible maintenance of two stable climate states
Author(s) -
Kahre Melinda A.,
Vines Sarah K.,
Haberle Robert M.,
Hollingsworth Jeffery L.
Publication year - 2013
Publication title -
journal of geophysical research: planets
Language(s) - English
Resource type - Journals
eISSN - 2169-9100
pISSN - 2169-9097
DOI - 10.1002/jgre.20099
Subject(s) - mars exploration program , atmosphere (unit) , martian , atmosphere of mars , atmospheric sciences , albedo (alchemy) , astrobiology , environmental science , general circulation model , climate change , physics , meteorology , geology , art , oceanography , performance art , art history
C. Leovy (personal communication, 2007) speculated that two stable climate states on early Mars could have resulted from interactions between the dust and CO 2 cycles. In one state, a highly active dust cycle would prevent atmospheric collapse, and in the second, the collapsed atmosphere would not maintain an active dust cycle. An initial assessment of this idea is presented based on a Mars general circulation model parameter study. A range of global dust loadings, CO 2 ice albedos, and obliquities are investigated to explore conditions in which increasing the atmospheric dust content stabilizes an otherwise unstable atmosphere. We find that dust only stabilizes the atmosphere at high obliquity and when the CO 2 ice albedo is high. Although results suggest that two stable states could have existed on early Mars under limited conditions, further work is needed to know if the conditions necessary are physically plausible.