Electron cooling by carbon monoxide in the atmospheres of Mars and Venus

dc.contributor.author Campbell, Laurence
dc.contributor.author Brunger, Michael James
dc.date.accessioned 2008-08-01T04:22:00Z
dc.date.available 2008-08-01T04:22:00Z
dc.date.issued 2008-02-04
dc.description PACS Codes: 34.80.Gs, 96.12.Jt en
dc.description.abstract Electron cooling, in which free electrons lose energy to vibrational excitation of gases, has been identified as a significant process in the atmospheres of Mars and Venus for electron impact on CO2. This process does not appear to have been evaluated for CO, although the density of CO exceeds that of CO2 in the upper atmospheres of these planets. In this paper electron cooling rates for CO are calculated and compared with existing rates for CO2. It is found that electron cooling by CO becomes more significant than by CO2 above altitudes of about 300 km on Mars and about 168 km on Venus. The sensitivity of the calculated cooling rates to different measurements of the integral cross sections for electron-impact vibrational excitation of CO is also investigated. en
dc.identifier.citation Campbell, L. and Brunger, M. 2008 Electron cooling by carbon monoxide in the atmospheres of Mars and Venus PMC Physics B, 1:3 en
dc.identifier.issn 1754-0429
dc.identifier.uri http://hdl.handle.net/2328/2963
dc.language.iso en
dc.oaire.license.condition.license CC-BY
dc.publisher BioMed Central - http://www.biomedcentral.com en
dc.subject Molecular excitation and ionization en
dc.subject Atmospheres en
dc.title Electron cooling by carbon monoxide in the atmospheres of Mars and Venus en
dc.type Article en
local.contributor.authorOrcidLookup Brunger, Michael James: https://orcid.org/0000-0002-7743-2990 en_US
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