Validation of ozone monitoring instrument level 1b data products

被引:81
作者
Dobber, M. [1 ]
Kleipool, Q. [1 ]
Dirksen, R. [1 ]
Levelt, P. [1 ]
Jaross, G. [3 ]
Taylor, S. [3 ]
Kelly, T. [3 ]
Flynn, L. [2 ]
Leppelmeier, G. [4 ]
Rozemeijer, N. [1 ,5 ]
机构
[1] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands
[2] NOAA, Camp Springs, MD 20746 USA
[3] Sci Syst & Applicat Inc, Greenbelt, MD 20706 USA
[4] G&S Associates, FIN-02360 Espoo, Finland
[5] TriOpSys BV, Utrecht, Netherlands
关键词
D O I
10.1029/2007JD008665
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The validation of the collection 2 level 1b radiance and irradiance data measured with the Ozone Monitoring Instrument (OMI) on NASA's Earth Observing System (EOS) Aura satellite is investigated and described. A number of improvements from collection 2 data to collection 3 data are identified and presented. It is shown that with these improvements in the calibration and in the data processing the accuracy of the geophysically calibrated level 1b radiance and irradiance is improved in the collection 3 data. It is shown that the OMI level 1b irradiance product can be reproduced from a high-resolution solar reference spectrum convolved with the OMI spectral slit functions within 3% for the Fraunhofer structure and within 0.5% for the offset. The agreement of the OMI level 1b irradiance data product with other available literature irradiance spectra is within 4%. The viewing angle dependence of the irradiance and the irradiance goniometry are discussed, and improvements in the collection 3 data are described. The in-orbit radiometric degradation since launch is shown to be smaller than 0.5% above 310 nm and increases to about 1.2% at 270 nm. It is shown how the viewing angle dependence of the radiance is improved in the collection 3 data. The calculation of the surface albedo from OMI measurement data is discussed, and first results are presented. The OMI surface albedo values are compared to literature values from the Total Ozone Mapping Spectrometer (TOMS) and the Global Ozone Monitoring Experiment (GOME). Finally, improvements in the spectral and spatial stray light corrections from collection 2 data to collection 3 data are presented and discussed.
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页数:12
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