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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Main Authors: 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, K. Walker, M. Weber, J. Zawodny
Format: Article
Language:English
Published: Copernicus Publications 2014-11-01
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.
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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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