1. Radiance and Jacobian intercomparison of radiative transfer models applied to HIRS and AMSU channels
- Author
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Godelieve Deblonde, Harold M. Woolf, D. S. Turner, Richard Engelen, Louis Garand, M. Hollingshead, Eric P. Salathé, J. R. Pardo, Jean-Luc Moncet, John J. Bates, Frédéric Chevallier, Larry M. McMillin, N.A. Scott, Sid-Ahmed Boukabara, P. Van Delst, D. S. McKague, P. J. Rayer, Joanna Joiner, Darren L. Jackson, Pascal Brunel, M. Larocque, Thomas J. Kleespies, R. Saunders, Gary J. Jedlovec, and European Centre for Medium-Range Weather Forecasts (ECMWF)
- Subjects
Atmospheric Science ,010504 meteorology & atmospheric sciences ,Meteorology ,Soil Science ,Aquatic Science ,Oceanography ,01 natural sciences ,010309 optics ,Geochemistry and Petrology ,0103 physical sciences ,Earth and Planetary Sciences (miscellaneous) ,Advanced Microwave Sounding Unit ,Radiative transfer ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,0105 earth and related environmental sciences ,Earth-Surface Processes ,Water Science and Technology ,Remote sensing ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,Ecology ,Atmospheric models ,Paleontology ,Forestry ,Atmospheric temperature ,Numerical weather prediction ,Depth sounding ,Geophysics ,13. Climate action ,Space and Planetary Science ,Brightness temperature ,Radiance ,Environmental science - Abstract
The goals of this study are the evaluation of current fast radiative transfer models (RTMs) and line-by-line (LBL) models. The intercomparison focuses on the modeling of 11 representative sounding channels routinely used at numerical weather prediction centers: seven HIRS (High-resolution Infrared Sounder) and four AMSU (Advanced Microwave Sounding Unit) channels. Interest in this topic was evidenced by the participation of 24 scientists from 16 institutions. An ensemble of 42 diverse atmospheres was used and results compiled for 19 infrared models and 10 microwave models, including several LBL RTMs. For the first time, not only radiances, but also Jacobians (of temperature, water vapor, and ozone) were compared to various LBL models for many channels. In the infrared, LBL models typically agree to within 0.05-0.15 K (standard deviation) in terms of top-of-the-atmosphere brightness temperature (BT). Individual differences up to 0.5 K still exist, systematic in some channels, and linked to the type of atmosphere in others. The best fast models emulate LBL BTs to within 0.25 K, but no model achieves this desirable level of success for all channels. The ozone modeling is particularly challenging. In the microwave, fast models generally do quite well against the LBL model to which they were tuned. However significant differences were noted among LBL models. Extending the intercomparison to the Jacobians proved very useful in detecting subtle and more obvious modeling errors. In addition, total and single gas optical depths were calculated, which provided additional insight on the nature of differences. Recommendations for future intercomparisons are suggested.
- Published
- 2001