Observation of tropospheric δD by IASI over western Siberia: comparison with a general circulation model

This study presents the joint H<sub>2</sub><sup>16</sup>O and HDO retrieval from Infrared Atmospheric Sounding Interferometer (IASI) spectra over western Siberia. IASI is an instrument on board the MetOp-A European satellite. The global coverage of the instrument and the good...

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Bibliographic Details
Main Authors: M. Pommier, J.-L. Lacour, C. Risi, F. M. Bréon, C. Clerbaux, P.-F. Coheur, K. Gribanov, D. Hurtmans, J. Jouzel, V. Zakharov
Format: Article
Language:English
Published: Copernicus Publications 2014-06-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/7/1581/2014/amt-7-1581-2014.pdf
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Summary:This study presents the joint H<sub>2</sub><sup>16</sup>O and HDO retrieval from Infrared Atmospheric Sounding Interferometer (IASI) spectra over western Siberia. IASI is an instrument on board the MetOp-A European satellite. The global coverage of the instrument and the good signal-to-noise ratio allow us to provide information on δD over this remote region. We show that IASI measurements may be used to estimate integrated δD between the surface and 3 km altitude or from 1 to 5 km depending on the thermal contrast, with observational errors lower than 4% and 7%, respectively. The retrieved data are compared to simulations from an isotopic general circulation model, LMDZ-iso for 2011. The satellite measurements and the model agree well and they reproduce well the seasonal and day-to-day variations for δD, presenting a good correlation (<i>r</i> up to 0.8 with the smoothed data in summer). The IASI-based retrievals also show the seasonal variation of the specific humidity in both altitude ranges.
ISSN:1867-1381
1867-8548