期刊
ATMOSPHERIC CHEMISTRY AND PHYSICS
卷 12, 期 5, 页码 2513-2532出版社
COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-12-2513-2012
关键词
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资金
- French Space Agency (Centre National d'Etudes Spatiales - CNES, France)
- IASI-TOSCA
- FP7 MACC (Monitoring Atmospheric Composition Change) project
- French LEFE program (CHAT/ASSIM) part of the SMOQA
- CHAT/ASSIM
- European Commission, Airbus and airlines - Lufthansa, Air France, Austrian
- INSU-CNRS
- Meteo-France
- FZJ (Forschungszentrum Julich, Germany)
Partial lower tropospheric ozone columns provided by the IASI (Infrared Atmospheric Sounding Interferometer) instrument have been assimilated into a chemistry-transport model at continental scale (CHIMERE) using an Ensemble Square Root Kalman Filter (EnSRF). Analyses are made for the month of July 2007 over the European domain. Launched in 2006, aboard the MetOp-A satellite, IASI shows high sensitivity for ozone in the free troposphere and low sensitivity at the ground; therefore it is important to evaluate if assimilation of these observations can improve free tropospheric ozone, and possibly surface ozone. The analyses are validated against independent ozone observations from sondes, MOZAIC(1) aircraft and ground based stations (AIRBASE - the European Air quality dataBase) and compared with respect to the free run of CHIMERE. These comparisons show a decrease in error of 6 parts-per-billion (ppb) in the free troposphere over the Frankfurt area, and also a reduction of the root mean square error (respectively bias) at the surface of 19% (33%) for more than 90% of existing ground stations. This provides evidence of the potential of data assimilation of tropospheric IASI columns to better describe the tropospheric ozone distribution, including surface ozone, despite the lower sensitivity. The changes in concentration resulting from the observational constraints were quantified and several geophysical explanations for the findings of this study were drawn. The corrections were most pronounced over Italy and the Mediterranean region, we noted an average reduction of 8-9 ppb in the free troposphere with respect to the free run, and still a reduction of 5.5 ppb at ground, likely due to a longer residence time of air masses in this part associated to the general circulation pattern (i.e. dominant western circulation) and to persistent anticyclonic conditions over the Mediterranean basin. This is an important geophysical result, since the ozone burden is large over this area, with impact on the radiative balance and air quality.
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