First results of the TRMM Microwave Imager (TMI) monthly oceanic rain rate: comparison with SSM/I
We evaluated the performance of the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) at‐launch algorithm for monthly oceanic rain rate using six months (January–June 1998) of TMI data. Comparison with oceanic monthly rain rates derived from the Special Sensor Microwave Imager (SSM/I...
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Veröffentlicht in: | Geophysical research letters 1999-08, Vol.26 (15), p.2379-2382 |
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creator | Chang, A. T. C. Chiu, L. S. Kummerow, C. Meng, J. Wilheit, T. T. |
description | We evaluated the performance of the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) at‐launch algorithm for monthly oceanic rain rate using six months (January–June 1998) of TMI data. Comparison with oceanic monthly rain rates derived from the Special Sensor Microwave Imager (SSM/I) data shows statistically significant differences. The TMI rain rates are lower than the SSM/I rain rates by about 10% overall, except for rain rates lower than 1.4 mm/day. The low TMI bias may be due to an overestimate of the columnar water vapor as indicated by the estimated rain layer thickness. The superior sampling by the TMI improves the algorithm statistics at the low rain rates. The averaged monthly rain rates over the latitudes between 40°S and 40°N are 2.78 and 3.17 mm/day, respectively for TMI and SSM/I, with RMS difference of 1.35 mm/day and correlation coefficient of 0.94. |
doi_str_mv | 10.1029/1998GL900452 |
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T. C. ; Chiu, L. S. ; Kummerow, C. ; Meng, J. ; Wilheit, T. T.</creator><creatorcontrib>Chang, A. T. C. ; Chiu, L. S. ; Kummerow, C. ; Meng, J. ; Wilheit, T. T.</creatorcontrib><description>We evaluated the performance of the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) at‐launch algorithm for monthly oceanic rain rate using six months (January–June 1998) of TMI data. Comparison with oceanic monthly rain rates derived from the Special Sensor Microwave Imager (SSM/I) data shows statistically significant differences. The TMI rain rates are lower than the SSM/I rain rates by about 10% overall, except for rain rates lower than 1.4 mm/day. The low TMI bias may be due to an overestimate of the columnar water vapor as indicated by the estimated rain layer thickness. The superior sampling by the TMI improves the algorithm statistics at the low rain rates. 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T. C.</creatorcontrib><creatorcontrib>Chiu, L. S.</creatorcontrib><creatorcontrib>Kummerow, C.</creatorcontrib><creatorcontrib>Meng, J.</creatorcontrib><creatorcontrib>Wilheit, T. T.</creatorcontrib><title>First results of the TRMM Microwave Imager (TMI) monthly oceanic rain rate: comparison with SSM/I</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>We evaluated the performance of the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) at‐launch algorithm for monthly oceanic rain rate using six months (January–June 1998) of TMI data. Comparison with oceanic monthly rain rates derived from the Special Sensor Microwave Imager (SSM/I) data shows statistically significant differences. The TMI rain rates are lower than the SSM/I rain rates by about 10% overall, except for rain rates lower than 1.4 mm/day. The low TMI bias may be due to an overestimate of the columnar water vapor as indicated by the estimated rain layer thickness. The superior sampling by the TMI improves the algorithm statistics at the low rain rates. The averaged monthly rain rates over the latitudes between 40°S and 40°N are 2.78 and 3.17 mm/day, respectively for TMI and SSM/I, with RMS difference of 1.35 mm/day and correlation coefficient of 0.94.</description><subject>Algorithms</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Geophysics</subject><subject>Geophysics. 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The TMI rain rates are lower than the SSM/I rain rates by about 10% overall, except for rain rates lower than 1.4 mm/day. The low TMI bias may be due to an overestimate of the columnar water vapor as indicated by the estimated rain layer thickness. The superior sampling by the TMI improves the algorithm statistics at the low rain rates. The averaged monthly rain rates over the latitudes between 40°S and 40°N are 2.78 and 3.17 mm/day, respectively for TMI and SSM/I, with RMS difference of 1.35 mm/day and correlation coefficient of 0.94.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/1998GL900452</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Algorithms Earth, ocean, space Exact sciences and technology External geophysics Geophysics Geophysics. Techniques, methods, instrumentation and models Latitude Microwaves Rain Sampling Special Sensor Microwave Imager Statistics |
title | First results of the TRMM Microwave Imager (TMI) monthly oceanic rain rate: comparison with SSM/I |
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