Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations

International audience The Infrared Atmospheric Sounding Interferometer (IASI) flying on-board MetOpA and MetOpB is able to capture fine isotopic variations of the HDO to H2O ratio (δD) in the troposphere. Such observations at the high spatio temporal resolution of the sounder are of great interest...

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Published in:Atmospheric Measurement Techniques
Main Authors: Lacour, Jean-Lionel, Clarisse, L., Worden, J., Schneider, M., Barthlott, S., Hase, F., Risi, C., Clerbaux, Cathy, Hurtmans, Daniel, Coheur, Pierre-François
Other Authors: Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique, Université libre de Bruxelles (ULB), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2015
Subjects:
Online Access:https://hal.science/hal-01082620
https://hal.science/hal-01082620/document
https://hal.science/hal-01082620/file/amt-8-1447-2015.pdf
https://doi.org/10.5194/amt-8-1447-2015
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record_format openpolar
institution Open Polar
collection École Polytechnique, Université Paris-Saclay: HAL
op_collection_id ftepunivpsaclay
language English
topic [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
spellingShingle [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
Lacour, Jean-Lionel
Clarisse, L.
Worden, J.
Schneider, M.
Barthlott, S.
Hase, F.
Risi, C.
Clerbaux, Cathy
Hurtmans, Daniel
Coheur, Pierre-François
Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience The Infrared Atmospheric Sounding Interferometer (IASI) flying on-board MetOpA and MetOpB is able to capture fine isotopic variations of the HDO to H2O ratio (δD) in the troposphere. Such observations at the high spatio temporal resolution of the sounder are of great interest to improve our understanding of the mechanisms controlling humidity in the troposphere. In this study we aim to empirically assess the validity of our error estimation previously evaluated theoretically. To achieve this, we compare IASI δD retrieved profiles with other available profiles of δD, from the TES infrared sounder onboard AURA and from three ground-based FTIR stations produced within the MUSICA project: the NDACC (Network for the Detection of Atmospheric Composition Change) sites Kiruna and Izana, and the TCCON site Karlsruhe, which in addition to near-infrared TCCON spectra also records mid-infrared spectra. We describe the achievable level of agreement between the different retrievals and show that these theoretical errors are in good agreement with empirical differences. The comparisons are made at different locations from tropical to Arctic latitudes, above sea and above land. Generally IASI and TES are similarly sensitive to δD in the free troposphere which allows to compare their measurements directly. At tropical latitudes where IASI's sensitivity is lower than that of TES, we show that the agreement improves when taking into account the sensitivity of IASI in the TES retrieval. For the comparison IASI-FTIR only direct comparisons are performed because of similar sensitivities. We identify a quasi negligible bias in the free troposphere (−3‰) between IASI retrieved δD with the TES one, which are bias corrected, but an important with the ground-based FTIR reaching −47‰. We also suggest that model-satellite observations comparisons could be optimized with IASI thanks to its high spatial and temporal sampling.
author2 Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique
Université libre de Bruxelles (ULB)
Jet Propulsion Laboratory (JPL)
NASA-California Institute of Technology (CALTECH)
Institute for Meteorology and Climate Research (IMK)
Karlsruhe Institute of Technology (KIT)
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
TROPO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Lacour, Jean-Lionel
Clarisse, L.
Worden, J.
Schneider, M.
Barthlott, S.
Hase, F.
Risi, C.
Clerbaux, Cathy
Hurtmans, Daniel
Coheur, Pierre-François
author_facet Lacour, Jean-Lionel
Clarisse, L.
Worden, J.
Schneider, M.
Barthlott, S.
Hase, F.
Risi, C.
Clerbaux, Cathy
Hurtmans, Daniel
Coheur, Pierre-François
author_sort Lacour, Jean-Lionel
title Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations
title_short Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations
title_full Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations
title_fullStr Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations
title_full_unstemmed Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations
title_sort cross-validation of iasi/metop derived tropospheric δd with tes and ground-based ftir observations
publisher HAL CCSD
publishDate 2015
url https://hal.science/hal-01082620
https://hal.science/hal-01082620/document
https://hal.science/hal-01082620/file/amt-8-1447-2015.pdf
https://doi.org/10.5194/amt-8-1447-2015
geographic Arctic
Kiruna
geographic_facet Arctic
Kiruna
genre Arctic
Kiruna
genre_facet Arctic
Kiruna
op_source ISSN: 1867-1381
EISSN: 1867-8548
Atmospheric Measurement Techniques
https://hal.science/hal-01082620
Atmospheric Measurement Techniques, 2015, 8, pp.1447-1466. ⟨10.5194/amt-8-1447-2015⟩
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container_title Atmospheric Measurement Techniques
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spelling ftepunivpsaclay:oai:HAL:hal-01082620v1 2024-06-09T07:44:25+00:00 Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations Lacour, Jean-Lionel Clarisse, L. Worden, J. Schneider, M. Barthlott, S. Hase, F. Risi, C. Clerbaux, Cathy Hurtmans, Daniel Coheur, Pierre-François Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique Université libre de Bruxelles (ULB) Jet Propulsion Laboratory (JPL) NASA-California Institute of Technology (CALTECH) Institute for Meteorology and Climate Research (IMK) Karlsruhe Institute of Technology (KIT) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) TROPO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 2015 https://hal.science/hal-01082620 https://hal.science/hal-01082620/document https://hal.science/hal-01082620/file/amt-8-1447-2015.pdf https://doi.org/10.5194/amt-8-1447-2015 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/amt-8-1447-2015 hal-01082620 https://hal.science/hal-01082620 https://hal.science/hal-01082620/document https://hal.science/hal-01082620/file/amt-8-1447-2015.pdf doi:10.5194/amt-8-1447-2015 info:eu-repo/semantics/OpenAccess ISSN: 1867-1381 EISSN: 1867-8548 Atmospheric Measurement Techniques https://hal.science/hal-01082620 Atmospheric Measurement Techniques, 2015, 8, pp.1447-1466. ⟨10.5194/amt-8-1447-2015⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2015 ftepunivpsaclay https://doi.org/10.5194/amt-8-1447-2015 2024-05-16T12:40:51Z International audience The Infrared Atmospheric Sounding Interferometer (IASI) flying on-board MetOpA and MetOpB is able to capture fine isotopic variations of the HDO to H2O ratio (δD) in the troposphere. Such observations at the high spatio temporal resolution of the sounder are of great interest to improve our understanding of the mechanisms controlling humidity in the troposphere. In this study we aim to empirically assess the validity of our error estimation previously evaluated theoretically. To achieve this, we compare IASI δD retrieved profiles with other available profiles of δD, from the TES infrared sounder onboard AURA and from three ground-based FTIR stations produced within the MUSICA project: the NDACC (Network for the Detection of Atmospheric Composition Change) sites Kiruna and Izana, and the TCCON site Karlsruhe, which in addition to near-infrared TCCON spectra also records mid-infrared spectra. We describe the achievable level of agreement between the different retrievals and show that these theoretical errors are in good agreement with empirical differences. The comparisons are made at different locations from tropical to Arctic latitudes, above sea and above land. Generally IASI and TES are similarly sensitive to δD in the free troposphere which allows to compare their measurements directly. At tropical latitudes where IASI's sensitivity is lower than that of TES, we show that the agreement improves when taking into account the sensitivity of IASI in the TES retrieval. For the comparison IASI-FTIR only direct comparisons are performed because of similar sensitivities. We identify a quasi negligible bias in the free troposphere (−3‰) between IASI retrieved δD with the TES one, which are bias corrected, but an important with the ground-based FTIR reaching −47‰. We also suggest that model-satellite observations comparisons could be optimized with IASI thanks to its high spatial and temporal sampling. Article in Journal/Newspaper Arctic Kiruna École Polytechnique, Université Paris-Saclay: HAL Arctic Kiruna Atmospheric Measurement Techniques 8 3 1447 1466