Broadband water vapor transmission functions for atmospheric IR flux computations

Transmission functions associated with water vapor molecular line and e-type absorption in the IR spectra regions are presented in the form of simple analytical functions and small tables, from which atmospheric IR fluxes and cooling rates can be easily computed. For typical clear atmospheres rangin...

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Main Author: Chou, M.-D.
Format: Other/Unknown Material
Language:unknown
Published: 1984
Subjects:
46
Subarctic
Online Access:http://ntrs.nasa.gov/search.jsp?R=19840061771
id ftnasantrs:oai:casi.ntrs.nasa.gov:19840061771
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19840061771 2023-05-15T18:28:13+02:00 Broadband water vapor transmission functions for atmospheric IR flux computations Chou, M.-D. Unclassified, Unlimited, Publicly available May 15, 1984 http://ntrs.nasa.gov/search.jsp?R=19840061771 unknown http://ntrs.nasa.gov/search.jsp?R=19840061771 Accession ID: 84A44558 Copyright Other Sources 46 Journal of the Atmospheric Sciences; 41; 1775-177 1984 ftnasantrs 2012-02-15T15:56:04Z Transmission functions associated with water vapor molecular line and e-type absorption in the IR spectra regions are presented in the form of simple analytical functions and small tables, from which atmospheric IR fluxes and cooling rates can be easily computed. For typical clear atmospheres ranging from the tropics to the subarctic region, the difference with respect to line-by-line calculations is less than 0.15 C/day in the cooling rate and approximately equal to or less than 1 percent in fluxes. Other/Unknown Material Subarctic NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic 46
spellingShingle 46
Chou, M.-D.
Broadband water vapor transmission functions for atmospheric IR flux computations
topic_facet 46
description Transmission functions associated with water vapor molecular line and e-type absorption in the IR spectra regions are presented in the form of simple analytical functions and small tables, from which atmospheric IR fluxes and cooling rates can be easily computed. For typical clear atmospheres ranging from the tropics to the subarctic region, the difference with respect to line-by-line calculations is less than 0.15 C/day in the cooling rate and approximately equal to or less than 1 percent in fluxes.
format Other/Unknown Material
author Chou, M.-D.
author_facet Chou, M.-D.
author_sort Chou, M.-D.
title Broadband water vapor transmission functions for atmospheric IR flux computations
title_short Broadband water vapor transmission functions for atmospheric IR flux computations
title_full Broadband water vapor transmission functions for atmospheric IR flux computations
title_fullStr Broadband water vapor transmission functions for atmospheric IR flux computations
title_full_unstemmed Broadband water vapor transmission functions for atmospheric IR flux computations
title_sort broadband water vapor transmission functions for atmospheric ir flux computations
publishDate 1984
url http://ntrs.nasa.gov/search.jsp?R=19840061771
op_coverage Unclassified, Unlimited, Publicly available
genre Subarctic
genre_facet Subarctic
op_source Other Sources
op_relation http://ntrs.nasa.gov/search.jsp?R=19840061771
Accession ID: 84A44558
op_rights Copyright
_version_ 1766210607538765824

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