Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium

Viking spacecraft radio-occultation measurements indicate that, irrespective of substantial differences, the polar ice cap regions on Mars have inversions similar to those of Pluto, and may also share vapor pressure equilibrium characteristics at the surface. This temperature-inversion phenomenon oc...

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Main Author: Eshleman, Von R.
Format: Other/Unknown Material
Language:unknown
Published: 1989
Subjects:
91
Online Access:http://ntrs.nasa.gov/search.jsp?R=19890062445
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19890062445 2023-05-15T16:38:10+02:00 Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium Eshleman, Von R. Unclassified, Unlimited, Publicly available Aug 1, 1989 http://ntrs.nasa.gov/search.jsp?R=19890062445 unknown http://ntrs.nasa.gov/search.jsp?R=19890062445 Accession ID: 89A49816 Copyright Other Sources 91 Icarus; 80; 439-443 1989 ftnasantrs 2012-02-15T18:06:41Z Viking spacecraft radio-occultation measurements indicate that, irrespective of substantial differences, the polar ice cap regions on Mars have inversions similar to those of Pluto, and may also share vapor pressure equilibrium characteristics at the surface. This temperature-inversion phenomenon occurs in a near-surface boundary layer; surface pressure-temperature may correspond to the vapor-pressure equilibrium with CH4 ice, or the temperature may be slightly higher to match the value derived from IRAS data. Other/Unknown Material Ice cap NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic 91
spellingShingle 91
Eshleman, Von R.
Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium
topic_facet 91
description Viking spacecraft radio-occultation measurements indicate that, irrespective of substantial differences, the polar ice cap regions on Mars have inversions similar to those of Pluto, and may also share vapor pressure equilibrium characteristics at the surface. This temperature-inversion phenomenon occurs in a near-surface boundary layer; surface pressure-temperature may correspond to the vapor-pressure equilibrium with CH4 ice, or the temperature may be slightly higher to match the value derived from IRAS data.
format Other/Unknown Material
author Eshleman, Von R.
author_facet Eshleman, Von R.
author_sort Eshleman, Von R.
title Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium
title_short Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium
title_full Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium
title_fullStr Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium
title_full_unstemmed Pluto's atmosphere - Models based on refraction, inversion, and vapor-pressure equilibrium
title_sort pluto's atmosphere - models based on refraction, inversion, and vapor-pressure equilibrium
publishDate 1989
url http://ntrs.nasa.gov/search.jsp?R=19890062445
op_coverage Unclassified, Unlimited, Publicly available
genre Ice cap
genre_facet Ice cap
op_source Other Sources
op_relation http://ntrs.nasa.gov/search.jsp?R=19890062445
Accession ID: 89A49816
op_rights Copyright
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