Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurements

This study describes the retrieval of water vapor vertical distributions in the upper troposphere and lower stratosphere (UTLS) altitude range from space-borne observations of the scattered solar light made in limb viewing geometry. First results using measurements from SCIAMACHY (Scanning Imaging A...

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Main Authors: A. Rozanov, K. Weigel, H. Bovensmann, S. Dhomse, K.-U. Eichmann, R. Kivi, V. Rozanov, H. Vömel, M. Weber, J. P. Burrows
Format: Article
Language:English
Published: Copernicus Publications 2011-05-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/4/933/2011/amt-4-933-2011.pdf
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spelling doaj-21e6f9a3d21040b7843044df36ff1cb42020-11-24T23:05:44ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482011-05-014593395410.5194/amt-4-933-2011Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurementsA. RozanovK. WeigelH. BovensmannS. DhomseK.-U. EichmannR. KiviV. RozanovH. VömelM. WeberJ. P. BurrowsThis study describes the retrieval of water vapor vertical distributions in the upper troposphere and lower stratosphere (UTLS) altitude range from space-borne observations of the scattered solar light made in limb viewing geometry. First results using measurements from SCIAMACHY (Scanning Imaging Absorption spectroMeter for Atmospheric CHartographY) aboard ENVISAT (Environmental Satellite) are presented here. In previous publications, the retrieval of water vapor vertical distributions has been achieved exploiting either the emitted radiance leaving the atmosphere or the transmitted solar radiation. In this study, the scattered solar radiation is used as a new source of information on the water vapor content in the UTLS region. A recently developed retrieval algorithm utilizes the differential absorption structure of the water vapor in 1353–1410 nm spectral range and yields the water vapor content in the 11–25 km altitude range. In this study, the retrieval algorithm is successfully applied to SCIAMACHY limb measurements and the resulting water vapor profiles are compared to in situ balloon-borne observations. The results from both satellite and balloon-borne instruments are found to agree typically within 10 %.http://www.atmos-meas-tech.net/4/933/2011/amt-4-933-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Rozanov
K. Weigel
H. Bovensmann
S. Dhomse
K.-U. Eichmann
R. Kivi
V. Rozanov
H. Vömel
M. Weber
J. P. Burrows
spellingShingle A. Rozanov
K. Weigel
H. Bovensmann
S. Dhomse
K.-U. Eichmann
R. Kivi
V. Rozanov
H. Vömel
M. Weber
J. P. Burrows
Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurements
Atmospheric Measurement Techniques
author_facet A. Rozanov
K. Weigel
H. Bovensmann
S. Dhomse
K.-U. Eichmann
R. Kivi
V. Rozanov
H. Vömel
M. Weber
J. P. Burrows
author_sort A. Rozanov
title Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurements
title_short Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurements
title_full Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurements
title_fullStr Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurements
title_full_unstemmed Retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from SCIAMACHY limb measurements
title_sort retrieval of water vapor vertical distributions in the upper troposphere and the lower stratosphere from sciamachy limb measurements
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2011-05-01
description This study describes the retrieval of water vapor vertical distributions in the upper troposphere and lower stratosphere (UTLS) altitude range from space-borne observations of the scattered solar light made in limb viewing geometry. First results using measurements from SCIAMACHY (Scanning Imaging Absorption spectroMeter for Atmospheric CHartographY) aboard ENVISAT (Environmental Satellite) are presented here. In previous publications, the retrieval of water vapor vertical distributions has been achieved exploiting either the emitted radiance leaving the atmosphere or the transmitted solar radiation. In this study, the scattered solar radiation is used as a new source of information on the water vapor content in the UTLS region. A recently developed retrieval algorithm utilizes the differential absorption structure of the water vapor in 1353–1410 nm spectral range and yields the water vapor content in the 11–25 km altitude range. In this study, the retrieval algorithm is successfully applied to SCIAMACHY limb measurements and the resulting water vapor profiles are compared to in situ balloon-borne observations. The results from both satellite and balloon-borne instruments are found to agree typically within 10 %.
url http://www.atmos-meas-tech.net/4/933/2011/amt-4-933-2011.pdf
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