Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz

Results are presented of the field measurements of atmospheric opacity at 278 GHz (9.3/cm) conducted at the McMurdo Station (Antarctica) during the austral springs of 1986 and 1987, in conjunction with balloon measurements of water vapor profile and total column density, showing a strong inverse tem...

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Main Authors: Emmons, Louisa K., De Zafra, Robert L.
Format: Other/Unknown Material
Language:unknown
Published: 1990
Subjects:
Online Access:http://ntrs.nasa.gov/search.jsp?R=19900049387
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author Emmons, Louisa K.
De Zafra, Robert L.
author_facet Emmons, Louisa K.
De Zafra, Robert L.
author_sort Emmons, Louisa K.
collection NASA Technical Reports Server (NTRS)
description Results are presented of the field measurements of atmospheric opacity at 278 GHz (9.3/cm) conducted at the McMurdo Station (Antarctica) during the austral springs of 1986 and 1987, in conjunction with balloon measurements of water vapor profile and total column density, showing a strong inverse temperature dependence when normalized to precipitable water vapor. The value of measured opacity per mm of precipitable water vapor (PWV) is roughly two times greater at -35 C than at -10 C and three times greater than measurements at +25 C reported by Zammit and Ade (1981). Various theories proposed to explain excess absorption in continuum regions are reviewed.
format Other/Unknown Material
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
geographic Austral
McMurdo Station
geographic_facet Austral
McMurdo Station
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institution Open Polar
language unknown
long_lat ENVELOPE(166.667,166.667,-77.850,-77.850)
op_collection_id ftnasantrs
op_coverage Unclassified, Unlimited, Publicly available
op_relation http://ntrs.nasa.gov/search.jsp?R=19900049387
Accession ID: 90A36442
op_rights Copyright
op_source Other Sources
publishDate 1990
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19900049387 2025-01-16T19:26:06+00:00 Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz Emmons, Louisa K. De Zafra, Robert L. Unclassified, Unlimited, Publicly available Apr 1, 1990 http://ntrs.nasa.gov/search.jsp?R=19900049387 unknown http://ntrs.nasa.gov/search.jsp?R=19900049387 Accession ID: 90A36442 Copyright Other Sources 47 International Journal of Infrared and Millimeter Waves; 11; 469-488 1990 ftnasantrs 2012-02-15T18:30:50Z Results are presented of the field measurements of atmospheric opacity at 278 GHz (9.3/cm) conducted at the McMurdo Station (Antarctica) during the austral springs of 1986 and 1987, in conjunction with balloon measurements of water vapor profile and total column density, showing a strong inverse temperature dependence when normalized to precipitable water vapor. The value of measured opacity per mm of precipitable water vapor (PWV) is roughly two times greater at -35 C than at -10 C and three times greater than measurements at +25 C reported by Zammit and Ade (1981). Various theories proposed to explain excess absorption in continuum regions are reviewed. Other/Unknown Material Antarc* Antarctica NASA Technical Reports Server (NTRS) Austral McMurdo Station ENVELOPE(166.667,166.667,-77.850,-77.850)
spellingShingle 47
Emmons, Louisa K.
De Zafra, Robert L.
Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz
title Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz
title_full Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz
title_fullStr Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz
title_full_unstemmed Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz
title_short Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz
title_sort observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 ghz
topic 47
topic_facet 47
url http://ntrs.nasa.gov/search.jsp?R=19900049387