Validation of MIPAS IMK/IAA V5R_O3_224 ozone profiles
We present the results of an extensive validation program of the most recent version of ozone vertical profiles retrieved with the IMK/IAA (Institute for Meteorology and Climate Research/Instituto de Astrofísica de Andalucía) MIPAS (Michelson Interferometer for Passive Atmospheric Sounding)...
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Format: | Article |
Language: | English |
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Copernicus Publications
2014-11-01
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Series: | Atmospheric Measurement Techniques |
Online Access: | https://www.atmos-meas-tech.net/7/3971/2014/amt-7-3971-2014.pdf |
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author | A. Laeng U. Grabowski T. von Clarmann G. Stiller N. Glatthor M. Höpfner S. Kellmann M. Kiefer A. Linden S. Lossow V. Sofieva I. Petropavlovskikh D. Hubert T. Bathgate P. Bernath C. D. Boone C. Clerbaux P. Coheur R. Damadeo D. Degenstein S. Frith L. Froidevaux J. Gille K. Hoppel M. McHugh Y. Kasai J. Lumpe N. Rahpoe G. Toon T. Sano M. Suzuki J. Tamminen J. Urban J. Urban K. Walker M. Weber J. Zawodny |
author_facet | A. Laeng U. Grabowski T. von Clarmann G. Stiller N. Glatthor M. Höpfner S. Kellmann M. Kiefer A. Linden S. Lossow V. Sofieva I. Petropavlovskikh D. Hubert T. Bathgate P. Bernath C. D. Boone C. Clerbaux P. Coheur R. Damadeo D. Degenstein S. Frith L. Froidevaux J. Gille K. Hoppel M. McHugh Y. Kasai J. Lumpe N. Rahpoe G. Toon T. Sano M. Suzuki J. Tamminen J. Urban J. Urban K. Walker M. Weber J. Zawodny |
author_sort | A. Laeng |
collection | DOAJ |
description | We present the results of an extensive validation program of the
most recent version of ozone vertical profiles retrieved with the
IMK/IAA (Institute for Meteorology and Climate Research/Instituto de Astrofísica de Andalucía)
MIPAS (Michelson Interferometer for Passive Atmospheric Sounding) research level 2 processor from version 5 spectral
level 1 data. The time period covered corresponds to the reduced
spectral resolution period of the MIPAS instrument, i.e., January
2005–April 2012. The comparison with satellite instruments includes
all post-2005 satellite limb and occultation sensors that have measured
the vertical profiles of tropospheric and stratospheric ozone:
ACE-FTS, GOMOS, HALOE, HIRDLS, MLS, OSIRIS, POAM, SAGE II,
SCIAMACHY, SMILES, and SMR. In addition, balloon-borne MkIV solar
occultation measurements and ground-based Umkehr measurements have
been included, as well as two nadir sensors: IASI and SBUV. For
each reference data set, bias determination and precision assessment
are performed. Better agreement with reference instruments than for the previous
data version, V5R_O3_220 (Laeng et al., 2014), is found: the known
high bias around the ozone vmr (volume mixing ratio) peak is significantly reduced and the
vertical resolution at 35 km has been improved. The agreement
with limb and solar occultation reference instruments
that have a known small bias vs. ozonesondes is within 7% in
the lower and middle stratosphere and 5% in the upper
troposphere. Around the ozone vmr peak, the agreement with most of
the satellite reference instruments is within 5%; this bias is as
low as 3% for ACE-FTS, MLS, OSIRIS, POAM and SBUV. |
first_indexed | 2024-12-21T22:18:15Z |
format | Article |
id | doaj.art-43b6a9e007d84e43bf22ad6b25da5012 |
institution | Directory Open Access Journal |
issn | 1867-1381 1867-8548 |
language | English |
last_indexed | 2024-12-21T22:18:15Z |
publishDate | 2014-11-01 |
publisher | Copernicus Publications |
record_format | Article |
series | Atmospheric Measurement Techniques |
spelling | doaj.art-43b6a9e007d84e43bf22ad6b25da50122022-12-21T18:48:23ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482014-11-0173971398710.5194/amt-7-3971-2014Validation of MIPAS IMK/IAA V5R_O3_224 ozone profilesA. Laeng0U. Grabowski1T. von Clarmann2G. Stiller3N. Glatthor4M. Höpfner5S. Kellmann6M. Kiefer7A. Linden8S. Lossow9V. Sofieva10I. Petropavlovskikh11D. Hubert12T. Bathgate13P. Bernath14C. D. Boone15C. Clerbaux16P. Coheur17R. Damadeo18D. Degenstein19S. Frith20L. Froidevaux21J. Gille22K. Hoppel23M. McHugh24Y. Kasai25J. Lumpe26N. Rahpoe27G. Toon28T. Sano29M. Suzuki30J. Tamminen31J. Urban32J. Urban33K. Walker34M. Weber35J. Zawodny36Institut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyInstitut für Meteorologie und Klimaforschung, Karlsruhe Institute of Technology (IMK KIT), Karlsruhe, GermanyFinnish Meteorological Institute, Helsinki, FinlandNOAA, Boulder, CO, USABelgian Institute for Space Aeronomy (BIRA-IASB), Brussels, BelgiumUniversity of Saskatchevan, Saskatoon, Saskatchewan, CanadaOld Dominion University, Norfolk, VA, USAUniversity of Toronto, Toronto, CanadaSorbonne Université, UPMC Univ. Paris 06, Université Versailles St-Quentin, CNRS/INSU, LATMOS-IPSL, France and ULB, Brussels, BelgiumSpectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles (ULB), Brussels, BelgiumNASA Langley Research Center, Hampton, USAUniversity of Saskatchevan, Saskatoon, Saskatchewan, CanadaScience Systems and Applications Inc., Lanham, MD, USAJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USAUniversity of Colorado, Boulder, CO, USANaval Research Laboratory, Washington DC, USASpectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles (ULB), Brussels, BelgiumNICT, Koganei, Tokyo, JapanComputational Physics, Inc., Boulder, CO, USAInstitut für Umweltphysik, University of Bremen, Bremen, GermanyJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USAJAXA, Tsukuba, JapanJAXA, Tsukuba, JapanFinnish Meteorological Institute, Helsinki, FinlandUniversity of Chalmers, Göteborg, SwedendeceasedUniversity of Toronto, Toronto, CanadaInstitut für Umweltphysik, University of Bremen, Bremen, GermanyNASA Langley Research Center, Hampton, USAWe present the results of an extensive validation program of the most recent version of ozone vertical profiles retrieved with the IMK/IAA (Institute for Meteorology and Climate Research/Instituto de Astrofísica de Andalucía) MIPAS (Michelson Interferometer for Passive Atmospheric Sounding) research level 2 processor from version 5 spectral level 1 data. The time period covered corresponds to the reduced spectral resolution period of the MIPAS instrument, i.e., January 2005–April 2012. The comparison with satellite instruments includes all post-2005 satellite limb and occultation sensors that have measured the vertical profiles of tropospheric and stratospheric ozone: ACE-FTS, GOMOS, HALOE, HIRDLS, MLS, OSIRIS, POAM, SAGE II, SCIAMACHY, SMILES, and SMR. In addition, balloon-borne MkIV solar occultation measurements and ground-based Umkehr measurements have been included, as well as two nadir sensors: IASI and SBUV. For each reference data set, bias determination and precision assessment are performed. Better agreement with reference instruments than for the previous data version, V5R_O3_220 (Laeng et al., 2014), is found: the known high bias around the ozone vmr (volume mixing ratio) peak is significantly reduced and the vertical resolution at 35 km has been improved. The agreement with limb and solar occultation reference instruments that have a known small bias vs. ozonesondes is within 7% in the lower and middle stratosphere and 5% in the upper troposphere. Around the ozone vmr peak, the agreement with most of the satellite reference instruments is within 5%; this bias is as low as 3% for ACE-FTS, MLS, OSIRIS, POAM and SBUV.https://www.atmos-meas-tech.net/7/3971/2014/amt-7-3971-2014.pdf |
spellingShingle | A. Laeng U. Grabowski T. von Clarmann G. Stiller N. Glatthor M. Höpfner S. Kellmann M. Kiefer A. Linden S. Lossow V. Sofieva I. Petropavlovskikh D. Hubert T. Bathgate P. Bernath C. D. Boone C. Clerbaux P. Coheur R. Damadeo D. Degenstein S. Frith L. Froidevaux J. Gille K. Hoppel M. McHugh Y. Kasai J. Lumpe N. Rahpoe G. Toon T. Sano M. Suzuki J. Tamminen J. Urban J. Urban K. Walker M. Weber J. Zawodny Validation of MIPAS IMK/IAA V5R_O3_224 ozone profiles Atmospheric Measurement Techniques |
title | Validation of MIPAS IMK/IAA V5R_O3_224 ozone profiles |
title_full | Validation of MIPAS IMK/IAA V5R_O3_224 ozone profiles |
title_fullStr | Validation of MIPAS IMK/IAA V5R_O3_224 ozone profiles |
title_full_unstemmed | Validation of MIPAS IMK/IAA V5R_O3_224 ozone profiles |
title_short | Validation of MIPAS IMK/IAA V5R_O3_224 ozone profiles |
title_sort | validation of mipas imk iaa v5r o3 224 ozone profiles |
url | https://www.atmos-meas-tech.net/7/3971/2014/amt-7-3971-2014.pdf |
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