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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Volume 2, issue 1
Atmos. Meas. Tech., 2, 287–298, 2009
https://doi.org/10.5194/amt-2-287-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Meas. Tech., 2, 287–298, 2009
https://doi.org/10.5194/amt-2-287-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  22 Jun 2009

22 Jun 2009

The benefit of limb cloud imaging for infrared limb sounding of tropospheric trace gases

S. Adams1,2, R. Spang1, P. Preusse1, and G. Heinemann2 S. Adams et al.
  • 1Institute of Chemistry and Dynamics of the Geosphere (ICG) I, Forschungszentrum Jülich, Jülich, Germany
  • 2Department of Environmental Meteorology, University of Trier, Trier, Germany

Abstract. Advances in detector technology enable a new generation of infrared limb sounders to measure 2-D images of the atmosphere. A proposed limb cloud imager (LCI) mode will detect clouds with a spatial resolution unprecedented for limb sounding. For the inference of temperature and trace gas distributions, detector pixels of the LCI have to be combined into super-pixels which provide the required signal-to-noise and information content for the retrievals. This study examines the extent to which tropospheric coverage can be improved in comparison to limb sounding using a fixed field of view with the size of the super-pixels, as in conventional limb sounders. The study is based on cloud topographies derived from (a) IR brightness temperatures (BT) of geostationary weather satellites in conjunction with ECMWF temperature profiles and (b) ice and liquid water content data of the Consortium for Small-scale Modeling-Europe (COSMO-EU) of the German Weather Service. Limb cloud images are simulated by matching the cloud topography with the limb sounding line of sight (LOS). The analysis of the BT data shows that the reduction of the spatial sampling along the track has hardly any effect on the gain in information. The comparison between BT and COSMO-EU data identifies the strength of both data sets, which are the representation of the horizontal cloud extent for the BT data and the reproduction of the cloud amount for the COSMO-EU data. The results of the analysis of both data sets show the great advantage of the cloud imager. However, because both cloud data sets do not present the complete fine structure of the real cloud fields in the atmosphere it is assumed that the results tend to underestimate the increase in information. In conclusion, real measurements by such an instrument may result in an even higher benefit for tropospheric limb retrievals.

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