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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union

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Atmos. Meas. Tech., 8, 1447-1466, 2015
© Author(s) 2015. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
20 Mar 2015
Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations
J.-L. Lacour1, L. Clarisse1, J. Worden2, M. Schneider3, S. Barthlott3, F. Hase3, C. Risi4, C. Clerbaux1,5, D. Hurtmans1, and P.-F. Coheur1 1Spectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles, Brussels, Belgium
2Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
3Institute for Meteorology and Climate Research (IMK-ASF), Karlsruhe Institute of Technology, Karlsruhe, Germany
4UPMC Univ. Paris 06, CNRS/INSU – UMR8539, LMD-IPSL, Paris, France
5UPMC Univ. Paris 06; Université Versailles St-Quentin, CNRS/INSU, LATMOS-IPSL, Paris, France
Abstract. The Infrared Atmospheric Sounding Interferometer (IASI) flying onboard 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 Izaña, 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 one 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 the sensitivity profiles of the two observing systems do not allow to take into account their differences of sensitivity. We identify a quasi negligible bias in the free troposphere (−3‰) between IASI retrieved δD with the TES, which are bias corrected, but important with the ground-based FTIR reaching −47‰. We also suggest that model-satellite observation comparisons could be optimized with IASI thanks to its high spatial and temporal sampling.

Citation: Lacour, J.-L., Clarisse, L., Worden, J., Schneider, M., Barthlott, S., Hase, F., Risi, C., Clerbaux, C., Hurtmans, D., and Coheur, P.-F.: Cross-validation of IASI/MetOp derived tropospheric δD with TES and ground-based FTIR observations, Atmos. Meas. Tech., 8, 1447-1466, doi:10.5194/amt-8-1447-2015, 2015.
Publications Copernicus
Short summary
This paper describes a cross-validation study of tropospheric δD (HDO/H2O ratio) profiles retrieved from IASI spectra (retrieval performed at ULB). We document how these profiles compare to profiles derived from TES/AURA sounder and from three ground-based FTIRs of the NDACC network (produced within the MUSICA project). We show that empirical differences are in agreement with the theoretical expected differences which are dominated by IASI observational and the smoothing error components.
This paper describes a cross-validation study of tropospheric δD (HDO/H2O ratio) profiles...