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An investigation of solar wind effects on the evolution of the Martian atmosphereThis investigation concentrated on the question of how atmosphere escape, related to both photochemistry and the Mars solar wind interaction, may have affected the evolution of Mars' atmosphere over time. The principal investigator and postdoctoral researcher adopted the premise that contemporary escape processes have dominated the losses to space over the past 3.5 billion years, but that the associated loss rates have been modified by solar evolution. A model was constructed for the contemporary escape scenario based on knowledge gained from both Venus in-situ measurements from Pioneer Venus Orbiter and Mars measurements from Phobos-2. Venus provided a valuable second example of a weakly magnetized planet having a similar solar wind interaction where we have more knowledge from observations. The model included photochemical losses from recombining ionospheric molecular ions, scavenging Martian upper atmosphere ('pickup') ions by the solar wind, and sputtering of the atmosphere by reentering pickup ions. The existence of the latter mechanism was realized during the course of the supported investigation, and is now thought by Jakosky and Pepin to explain some of the Martian noble gas isotope ratios.
Document ID
19940032504
Acquisition Source
Legacy CDMS
Document Type
Contractor Report (CR)
Authors
Luhmann, Janet G.
(California Univ. Los Angeles, CA, United States)
Date Acquired
September 6, 2013
Publication Date
January 1, 1994
Subject Category
Solar Physics
Report/Patent Number
NAS 1.26:193424
NASA-CR-193424
Accession Number
94N37012
Funding Number(s)
CONTRACT_GRANT: NAGW-2295
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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