Home > Publications database > Cross comparison of O3 and NO2 measured by the atmospheric ENVISAT instruments GOMOS, MIPAS, and SCIAMACHY > print

001     41265
005     20240911115615.0
024 7 _ |2 DOI
|a 10.1016/j.asr.2005.04.005
024 7 _ |2 WOS
|a WOS:000235478400012
037 _ _ |a PreJuSER-41265
041 _ _ |a eng
082 _ _ |a 520
084 _ _ |2 WoS
|a Engineering, Aerospace
084 _ _ |2 WoS
|a Astronomy & Astrophysics
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |a Bracher, A.
|b 0
|0 P:(DE-HGF)0
245 _ _ |a Cross comparison of O3 and NO2 measured by the atmospheric ENVISAT instruments GOMOS, MIPAS, and SCIAMACHY
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2005
300 _ _ |a 855 - 867
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
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336 7 _ |a Output Types/Journal article
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336 7 _ |a Journal Article
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336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |a Advances in Space Research
|x 0273-1177
|0 9884
|y 5
|v 36
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Vertical profiles Of O-3 and NO2 abundances from the atmospheric instruments GOMOS (Global Ozone Monitoring by the Occultation of Stars), MIPAS (Michelson Interferometer for Passive Atmospheric Sounding) and SCIAMACHY (Scanning Imaging Spectrometer for Atmospheric Chartography) all on-board the recently launched European Space Agency (ESA) Environmental Satellite (ENVISAT) are intercompared. These comparisons contribute to the validation of these data products by detecting systematic deviations, for example, wrong tangent height determinations, spectroscopic errors, and others. The cross comparison includes GOMOS data products retrieved by the GOMOS prototype processor from ACRI (Sophia Antipolis, France), the scientific SCIAMACHY data products from the Institute of Environmental Physics at University of Bremen (IUP) and the scientific MIPAS data products from the Institute for Meteorology and Climate Research in Karlsruhe (IMK) and Institute of Astrophysics in Andalusia (IAA). Coincident measurements were identified by limiting the time difference to 100 min (duration of one orbit) and less than 500 km between two observation points. When lower stratospheric ozone is strongly depleted during polar spring, a homogeneity condition was further imposed on the satellite measurements by requiring an upper limit on the potential vorticity difference at the 475 K isentrope between both observations. Since geographically coincident NO2 measurements of the three instruments are performed during different times of the day and NO2 has a rather strong diurnal variability, matches of NO2 profiles were compared only where the solar zenith angle difference was below 5 degrees. First results of the cross comparison show an agreement within 15% between 21 and 40 km altitude for O-3 profiles and an agreement within 20% between 27 and 40 km altitude for NO2 profiles among the GOMOS, MIPAS and SCIAMACHY measurements. (c) 2005 COSPAR. Published by Elsevier Ltd. All rights reserved.
536 _ _ |a Chemie und Dynamik der Geo-Biosphäre
|c U01
|2 G:(DE-HGF)
|0 G:(DE-Juel1)FUEK257
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588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a S
|2 WoSType
653 2 0 |2 Author
|a ENVISAT
653 2 0 |2 Author
|a stratosphere
653 2 0 |2 Author
|a ozone
653 2 0 |2 Author
|a NO2
653 2 0 |2 Author
|a satellite cross comparison
700 1 _ |a Bovensmann, H.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Bramsted, K.
|b 2
|0 P:(DE-HGF)0
700 1 _ |a Burrows, J. P.
|b 3
|0 P:(DE-HGF)0
700 1 _ |a von Clarmann, T.
|b 4
|0 P:(DE-HGF)0
700 1 _ |a Eichmann, K.-U.
|b 5
|0 P:(DE-HGF)0
700 1 _ |a Fischer, H.
|b 6
|0 P:(DE-HGF)0
700 1 _ |a Funke, B.
|b 7
|0 P:(DE-HGF)0
700 1 _ |a Gil-Lopez, S.
|b 8
|u FZJ
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700 1 _ |a Glatthor, G. P.
|b 9
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700 1 _ |a Grabowski, U.
|b 10
|0 P:(DE-HGF)0
700 1 _ |a Höpfner, M.
|b 11
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700 1 _ |a Kaufmann, M.
|b 12
|u FZJ
|0 P:(DE-Juel1)129128
700 1 _ |a Kellmann, S.
|b 13
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700 1 _ |a Kiefer, M.
|b 14
|0 P:(DE-HGF)0
700 1 _ |a Koukouli, M. E.
|b 15
|0 P:(DE-HGF)0
700 1 _ |a Linden, A.
|b 16
|0 P:(DE-HGF)0
700 1 _ |a Lopez-Puertas, M. L.
|b 17
|0 P:(DE-HGF)0
700 1 _ |a Mengistu-Tsidu, G.
|b 18
|0 P:(DE-HGF)0
700 1 _ |a Milz, M.
|b 19
|0 P:(DE-HGF)0
700 1 _ |a Noel, S.
|b 20
|0 P:(DE-HGF)0
700 1 _ |a Rohen, G.
|b 21
|0 P:(DE-HGF)0
700 1 _ |a Rozanov, A.
|b 22
|0 P:(DE-HGF)0
700 1 _ |a Rozanov, V. V.
|b 23
|0 P:(DE-HGF)0
700 1 _ |a von Savigny, C.
|b 24
|0 P:(DE-HGF)0
700 1 _ |a Sinnhuber, M.
|b 25
|0 P:(DE-HGF)0
700 1 _ |a Skupin, J.
|b 26
|0 P:(DE-HGF)0
700 1 _ |a Steck, T.
|b 27
|0 P:(DE-HGF)0
700 1 _ |a Stiller, G. P.
|b 28
|0 P:(DE-HGF)0
700 1 _ |a Wang, D.-Y.
|b 29
|0 P:(DE-HGF)0
700 1 _ |a Weber, M.
|b 30
|0 P:(DE-HGF)0
700 1 _ |a Wuttke, M. W.
|b 31
|0 P:(DE-HGF)0
773 _ _ |a 10.1016/j.asr.2005.04.005
|g Vol. 36, p. 855 - 867
|p 855 - 867
|q 36<855 - 867
|0 PERI:(DE-600)2023311-5
|t Advances in space research
|v 36
|y 2005
|x 0273-1177
856 7 _ |u http://dx.doi.org/10.1016/j.asr.2005.04.005
909 C O |o oai:juser.fz-juelich.de:41265
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913 1 _ |k U01
|v Chemie und Dynamik der Geo-Biosphäre
|l Chemie und Dynamik der Geo-Biosphäre
|b Environment (Umwelt)
|0 G:(DE-Juel1)FUEK257
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914 1 _ |y 2005
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-I
|l Stratosphäre
|d 31.12.2006
|g ICG
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980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)ICE-4-20101013
981 _ _ |a I:(DE-Juel1)IEK-7-20101013

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