Validation of MIPAS ClONO 2 measurements

International audience Altitude profiles of ClONO 2 retrieved with the IMK (Institut für Meteorologie und Klimaforschung) science-oriented data processor from MIPAS/Envisat (Michelson Interferometer for Passive Atmospheric Sounding on Envisat) mid-infrared limb emission measurements between July 200...

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Main Authors: Höpfner, M., von Clarmann, T., Fischer, H., Funke, B., Glatthor, N., Grabowski, U., Kellmann, S., Kiefer, M., Linden, A., Milz, M., Steck, T., Stiller, G. P., Bernath, P., Blom, C. E., Blumenstock, Th., Boone, C., Chance, K., Coffey, M. T., Friedl-Vallon, F., Griffith, D., Hannigan, J. W., Hase, F., Jones, N., Jucks, K. W., Keim, C., Kleinert, A., Kouker, W., Liu, G. Y., Mahieu, E., Mellqvist, J., Mikuteit, S., Notholt, J., Oelhaf, H., Piesch, C., Reddmann, T., Ruhnke, R., Schneider, M., Strandberg, A., Toon, G., Walker, K. A., Warneke, T., Wetzel, G., Wood, S., Zander, R.
Other Authors: Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Instituto de Astrofísica de Andalucía (IAA), Consejo Superior de Investigaciones Científicas Madrid (CSIC), Department of Chemistry, Harvard-Smithsonian Center for Astrophysics (CfA), Harvard University Cambridge -Smithsonian Institution, Atmospheric Chemistry Division Boulder, National Center for Atmospheric Research Boulder (NCAR), Institut d'Astrophysique et de Géophysique Liège, Université de Liège, Department of Radio and Space Science Göteborg, Chalmers University of Technology Göteborg, Institut für Umweltphysik Bremen (IUP), Universität Bremen, Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Institut für Umweltphysik Heidelberg, Universität Heidelberg Heidelberg, National Institute of Water and Atmospheric Research Wellington (NIWA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2006
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00303952
https://hal.archives-ouvertes.fr/hal-00303952/document
https://hal.archives-ouvertes.fr/hal-00303952/file/acpd-6-9765-2006.pdf
id ftunivnantes:oai:HAL:hal-00303952v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Höpfner, M.
von Clarmann, T.
Fischer, H.
Funke, B.
Glatthor, N.
Grabowski, U.
Kellmann, S.
Kiefer, M.
Linden, A.
Milz, M.
Steck, T.
Stiller, G. P.
Bernath, P.
Blom, C. E.
Blumenstock, Th.
Boone, C.
Chance, K.
Coffey, M. T.
Friedl-Vallon, F.
Griffith, D.
Hannigan, J. W.
Hase, F.
Jones, N.
Jucks, K. W.
Keim, C.
Kleinert, A.
Kouker, W.
Liu, G. Y.
Mahieu, E.
Mellqvist, J.
Mikuteit, S.
Notholt, J.
Oelhaf, H.
Piesch, C.
Reddmann, T.
Ruhnke, R.
Schneider, M.
Strandberg, A.
Toon, G.
Walker, K. A.
Warneke, T.
Wetzel, G.
Wood, S.
Zander, R.
Validation of MIPAS ClONO 2 measurements
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience Altitude profiles of ClONO 2 retrieved with the IMK (Institut für Meteorologie und Klimaforschung) science-oriented data processor from MIPAS/Envisat (Michelson Interferometer for Passive Atmospheric Sounding on Envisat) mid-infrared limb emission measurements between July 2002 and March 2004 have been validated by comparison with balloon-borne (Mark IV, FIRS2, MIPAS-B), airborne (MIPAS-STR), ground-based (Spitsbergen, Thule, Kiruna, Harestua, Jungfraujoch, Izaña, Wollongong, Lauder), and spaceborne (ACE-FTS) observations. With few exceptions we found very good agreement between these instruments and MIPAS with no evidence for any bias in most cases and altitude regions. For balloon-borne measurements typical absolute mean differences are below 0.05 ppbv over the whole altitude range from 10 to 39 km. In case of ACE-FTS observations mean differences are below 0.03 ppbv for observations below 26 km. Above this altitude the comparison with ACE-FTS is affected by the photochemically induced diurnal variation of ClONO 2 . Correction for this by use of a chemical transport model led to an overcompensation of the photochemical effect by up to 0.1 ppbv at altitudes of 30?35 km in case of MIPAS-ACE-FTS comparisons while for the balloon-borne observations no such inconsistency has been detected. The comparison of MIPAS derived total column amounts with ground-based observations revealed no significant bias in the MIPAS data. Mean differences between MIPAS and FTIR column abundances are 0.11±0.12×10 14 cm ?2 (1.0±1.1%) and ?0.09±0.19×10 14 cm ?2 (?0.8±1.7%), depending on the coincidence criterion applied. ? 2 tests have been performed to assess the combined precision estimates of MIPAS and the related instruments. When no exact coincidences were available as in case of MIPAS ? FTIR or MIPAS ? ACE-FTS comparisons it has been necessary to take into consideration a coincidence error term to account for ? 2 deviations. From the resulting ? 2 profiles there is no evidence for a systematic ...
author2 Institute for Meteorology and Climate Research (IMK)
Karlsruhe Institute of Technology (KIT)
Instituto de Astrofísica de Andalucía (IAA)
Consejo Superior de Investigaciones Científicas Madrid (CSIC)
Department of Chemistry
Harvard-Smithsonian Center for Astrophysics (CfA)
Harvard University Cambridge -Smithsonian Institution
Atmospheric Chemistry Division Boulder
National Center for Atmospheric Research Boulder (NCAR)
Institut d'Astrophysique et de Géophysique Liège
Université de Liège
Department of Radio and Space Science Göteborg
Chalmers University of Technology Göteborg
Institut für Umweltphysik Bremen (IUP)
Universität Bremen
Jet Propulsion Laboratory (JPL)
NASA-California Institute of Technology (CALTECH)
Institut für Umweltphysik Heidelberg
Universität Heidelberg Heidelberg
National Institute of Water and Atmospheric Research Wellington (NIWA)
format Article in Journal/Newspaper
author Höpfner, M.
von Clarmann, T.
Fischer, H.
Funke, B.
Glatthor, N.
Grabowski, U.
Kellmann, S.
Kiefer, M.
Linden, A.
Milz, M.
Steck, T.
Stiller, G. P.
Bernath, P.
Blom, C. E.
Blumenstock, Th.
Boone, C.
Chance, K.
Coffey, M. T.
Friedl-Vallon, F.
Griffith, D.
Hannigan, J. W.
Hase, F.
Jones, N.
Jucks, K. W.
Keim, C.
Kleinert, A.
Kouker, W.
Liu, G. Y.
Mahieu, E.
Mellqvist, J.
Mikuteit, S.
Notholt, J.
Oelhaf, H.
Piesch, C.
Reddmann, T.
Ruhnke, R.
Schneider, M.
Strandberg, A.
Toon, G.
Walker, K. A.
Warneke, T.
Wetzel, G.
Wood, S.
Zander, R.
author_facet Höpfner, M.
von Clarmann, T.
Fischer, H.
Funke, B.
Glatthor, N.
Grabowski, U.
Kellmann, S.
Kiefer, M.
Linden, A.
Milz, M.
Steck, T.
Stiller, G. P.
Bernath, P.
Blom, C. E.
Blumenstock, Th.
Boone, C.
Chance, K.
Coffey, M. T.
Friedl-Vallon, F.
Griffith, D.
Hannigan, J. W.
Hase, F.
Jones, N.
Jucks, K. W.
Keim, C.
Kleinert, A.
Kouker, W.
Liu, G. Y.
Mahieu, E.
Mellqvist, J.
Mikuteit, S.
Notholt, J.
Oelhaf, H.
Piesch, C.
Reddmann, T.
Ruhnke, R.
Schneider, M.
Strandberg, A.
Toon, G.
Walker, K. A.
Warneke, T.
Wetzel, G.
Wood, S.
Zander, R.
author_sort Höpfner, M.
title Validation of MIPAS ClONO 2 measurements
title_short Validation of MIPAS ClONO 2 measurements
title_full Validation of MIPAS ClONO 2 measurements
title_fullStr Validation of MIPAS ClONO 2 measurements
title_full_unstemmed Validation of MIPAS ClONO 2 measurements
title_sort validation of mipas clono 2 measurements
publisher HAL CCSD
publishDate 2006
url https://hal.archives-ouvertes.fr/hal-00303952
https://hal.archives-ouvertes.fr/hal-00303952/document
https://hal.archives-ouvertes.fr/hal-00303952/file/acpd-6-9765-2006.pdf
geographic Kiruna
geographic_facet Kiruna
genre Kiruna
Spitsbergen
genre_facet Kiruna
Spitsbergen
op_source ISSN: 1680-7367
EISSN: 1680-7375
Atmospheric Chemistry and Physics Discussions
https://hal.archives-ouvertes.fr/hal-00303952
Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2006, 6 (5), pp.9765-9821
op_relation hal-00303952
https://hal.archives-ouvertes.fr/hal-00303952
https://hal.archives-ouvertes.fr/hal-00303952/document
https://hal.archives-ouvertes.fr/hal-00303952/file/acpd-6-9765-2006.pdf
op_rights info:eu-repo/semantics/OpenAccess
_version_ 1766058410638311424
spelling ftunivnantes:oai:HAL:hal-00303952v1 2023-05-15T17:04:20+02:00 Validation of MIPAS ClONO 2 measurements Höpfner, M. von Clarmann, T. Fischer, H. Funke, B. Glatthor, N. Grabowski, U. Kellmann, S. Kiefer, M. Linden, A. Milz, M. Steck, T. Stiller, G. P. Bernath, P. Blom, C. E. Blumenstock, Th. Boone, C. Chance, K. Coffey, M. T. Friedl-Vallon, F. Griffith, D. Hannigan, J. W. Hase, F. Jones, N. Jucks, K. W. Keim, C. Kleinert, A. Kouker, W. Liu, G. Y. Mahieu, E. Mellqvist, J. Mikuteit, S. Notholt, J. Oelhaf, H. Piesch, C. Reddmann, T. Ruhnke, R. Schneider, M. Strandberg, A. Toon, G. Walker, K. A. Warneke, T. Wetzel, G. Wood, S. Zander, R. Institute for Meteorology and Climate Research (IMK) Karlsruhe Institute of Technology (KIT) Instituto de Astrofísica de Andalucía (IAA) Consejo Superior de Investigaciones Científicas Madrid (CSIC) Department of Chemistry Harvard-Smithsonian Center for Astrophysics (CfA) Harvard University Cambridge -Smithsonian Institution Atmospheric Chemistry Division Boulder National Center for Atmospheric Research Boulder (NCAR) Institut d'Astrophysique et de Géophysique Liège Université de Liège Department of Radio and Space Science Göteborg Chalmers University of Technology Göteborg Institut für Umweltphysik Bremen (IUP) Universität Bremen Jet Propulsion Laboratory (JPL) NASA-California Institute of Technology (CALTECH) Institut für Umweltphysik Heidelberg Universität Heidelberg Heidelberg National Institute of Water and Atmospheric Research Wellington (NIWA) 2006-10-05 https://hal.archives-ouvertes.fr/hal-00303952 https://hal.archives-ouvertes.fr/hal-00303952/document https://hal.archives-ouvertes.fr/hal-00303952/file/acpd-6-9765-2006.pdf en eng HAL CCSD European Geosciences Union hal-00303952 https://hal.archives-ouvertes.fr/hal-00303952 https://hal.archives-ouvertes.fr/hal-00303952/document https://hal.archives-ouvertes.fr/hal-00303952/file/acpd-6-9765-2006.pdf info:eu-repo/semantics/OpenAccess ISSN: 1680-7367 EISSN: 1680-7375 Atmospheric Chemistry and Physics Discussions https://hal.archives-ouvertes.fr/hal-00303952 Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2006, 6 (5), pp.9765-9821 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2006 ftunivnantes 2022-11-16T00:47:48Z International audience Altitude profiles of ClONO 2 retrieved with the IMK (Institut für Meteorologie und Klimaforschung) science-oriented data processor from MIPAS/Envisat (Michelson Interferometer for Passive Atmospheric Sounding on Envisat) mid-infrared limb emission measurements between July 2002 and March 2004 have been validated by comparison with balloon-borne (Mark IV, FIRS2, MIPAS-B), airborne (MIPAS-STR), ground-based (Spitsbergen, Thule, Kiruna, Harestua, Jungfraujoch, Izaña, Wollongong, Lauder), and spaceborne (ACE-FTS) observations. With few exceptions we found very good agreement between these instruments and MIPAS with no evidence for any bias in most cases and altitude regions. For balloon-borne measurements typical absolute mean differences are below 0.05 ppbv over the whole altitude range from 10 to 39 km. In case of ACE-FTS observations mean differences are below 0.03 ppbv for observations below 26 km. Above this altitude the comparison with ACE-FTS is affected by the photochemically induced diurnal variation of ClONO 2 . Correction for this by use of a chemical transport model led to an overcompensation of the photochemical effect by up to 0.1 ppbv at altitudes of 30?35 km in case of MIPAS-ACE-FTS comparisons while for the balloon-borne observations no such inconsistency has been detected. The comparison of MIPAS derived total column amounts with ground-based observations revealed no significant bias in the MIPAS data. Mean differences between MIPAS and FTIR column abundances are 0.11±0.12×10 14 cm ?2 (1.0±1.1%) and ?0.09±0.19×10 14 cm ?2 (?0.8±1.7%), depending on the coincidence criterion applied. ? 2 tests have been performed to assess the combined precision estimates of MIPAS and the related instruments. When no exact coincidences were available as in case of MIPAS ? FTIR or MIPAS ? ACE-FTS comparisons it has been necessary to take into consideration a coincidence error term to account for ? 2 deviations. From the resulting ? 2 profiles there is no evidence for a systematic ... Article in Journal/Newspaper Kiruna Spitsbergen Université de Nantes: HAL-UNIV-NANTES Kiruna