Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations

Abstract High‐spectral‐resolution thermal infrared radiance observations made with the Airborne Research Interferometer Evaluation System instrument on the Met Office C130 aircraft in tropical and sub‐arctic atmospheres are used to evaluate the water vapour continuum and line absorption. Coincident...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Taylor, Jonathan P., Newman, Stuart M., Hewison, Tim J., McGrath, Andrew
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2003
Subjects:
Online Access:http://dx.doi.org/10.1256/qj.03.08
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1256%2Fqj.03.08
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spelling crwiley:10.1256/qj.03.08 2023-12-03T10:17:02+01:00 Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations Taylor, Jonathan P. Newman, Stuart M. Hewison, Tim J. McGrath, Andrew 2003 http://dx.doi.org/10.1256/qj.03.08 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1256%2Fqj.03.08 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1256/qj.03.08 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 129, issue 594, page 2949-2969 ISSN 0035-9009 1477-870X Atmospheric Science journal-article 2003 crwiley https://doi.org/10.1256/qj.03.08 2023-11-09T14:29:12Z Abstract High‐spectral‐resolution thermal infrared radiance observations made with the Airborne Research Interferometer Evaluation System instrument on the Met Office C130 aircraft in tropical and sub‐arctic atmospheres are used to evaluate the water vapour continuum and line absorption. Coincident microwave radiometer measurements at 183 GHz are used to help constrain the water vapour profile. Through careful selection of wavelengths where the water vapour continuum has varying impacts on the observed radiances, analysis shows that the continuum is too strong; this is using the General Line‐by‐line Atmospheric Transmittance and Radiance Model with the CKD2.4 water vapour continuum and High Resolution Transmission Molecular Absorption 2000 spectral database. Zenith observations from low altitude indicate that the continuum requires reducing by between 6% and 15% depending on the frequency, which is in good agreement with recent laboratory data. A modified continuum is presented and used in modelling to compare against upper‐troposphere nadir measurements obtained in tropical and sub‐arctic atmospheres. Copyright © Crown copyright, 2003 Article in Journal/Newspaper Arctic Wiley Online Library (via Crossref) Arctic Quarterly Journal of the Royal Meteorological Society 129 594 2949 2969
institution Open Polar
collection Wiley Online Library (via Crossref)
op_collection_id crwiley
language English
topic Atmospheric Science
spellingShingle Atmospheric Science
Taylor, Jonathan P.
Newman, Stuart M.
Hewison, Tim J.
McGrath, Andrew
Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations
topic_facet Atmospheric Science
description Abstract High‐spectral‐resolution thermal infrared radiance observations made with the Airborne Research Interferometer Evaluation System instrument on the Met Office C130 aircraft in tropical and sub‐arctic atmospheres are used to evaluate the water vapour continuum and line absorption. Coincident microwave radiometer measurements at 183 GHz are used to help constrain the water vapour profile. Through careful selection of wavelengths where the water vapour continuum has varying impacts on the observed radiances, analysis shows that the continuum is too strong; this is using the General Line‐by‐line Atmospheric Transmittance and Radiance Model with the CKD2.4 water vapour continuum and High Resolution Transmission Molecular Absorption 2000 spectral database. Zenith observations from low altitude indicate that the continuum requires reducing by between 6% and 15% depending on the frequency, which is in good agreement with recent laboratory data. A modified continuum is presented and used in modelling to compare against upper‐troposphere nadir measurements obtained in tropical and sub‐arctic atmospheres. Copyright © Crown copyright, 2003
format Article in Journal/Newspaper
author Taylor, Jonathan P.
Newman, Stuart M.
Hewison, Tim J.
McGrath, Andrew
author_facet Taylor, Jonathan P.
Newman, Stuart M.
Hewison, Tim J.
McGrath, Andrew
author_sort Taylor, Jonathan P.
title Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations
title_short Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations
title_full Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations
title_fullStr Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations
title_full_unstemmed Water vapour line and continuum absorption in the thermal infrared—reconciling models and observations
title_sort water vapour line and continuum absorption in the thermal infrared—reconciling models and observations
publisher Wiley
publishDate 2003
url http://dx.doi.org/10.1256/qj.03.08
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1256%2Fqj.03.08
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1256/qj.03.08
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Quarterly Journal of the Royal Meteorological Society
volume 129, issue 594, page 2949-2969
ISSN 0035-9009 1477-870X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1256/qj.03.08
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 129
container_issue 594
container_start_page 2949
op_container_end_page 2969
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