Gairola, R. M. ; Gohil, B. S. ; Pandey, P. C. (1985) Retrieval of precipitable water from Bhaskara-II microwave measurements and its comparison with NOAA-7 and radiosonde data Remote Sensing of Environment, 18 (2). pp. 125-135. ISSN 0034-4257
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Official URL: http://linkinghub.elsevier.com/retrieve/pii/003442...
Related URL: http://dx.doi.org/10.1016/0034-4257(85)90043-4
Abstract
The Satellite Microwave Radiometer (SAMIR-II) on board the second Indian remote sensing satellite, Bhaskara-II, measured microwave radiation at 19.35, 22.235, and 31.4 GHz. These measurements are primarily influenced by water vapor, cloud liquid water, and wind speed. The effect of collinearity among SAMIR-II channels has been examined to determine the effectiveness of a two- or three-channel subset for retrieving precipitable water (PW). The analysis indicated a decreasing correlation coefficient value from 0.87 to 0.65 with increasing frequency separation due to dynamical interdependence of meteorological variables on brightness temperature measurements. A correlation coefficient of 0.65 between two window channels, 19.35 and 31.4 GHz, is suggestive of using either of the two channels for water vapor retrieval. Performance of SAMIR-II channels has therefore been evaluated by retrieving (PW) using regression technique with all the three channels of SAMIR-II and its subset of the two channels, 19.35/22.235 and 22.235/31.4 GHz and comparing the results from NOAA-7 supplied PW and limited radiosonde derived PW. Comparison of PW derived from the regression models and NOAA-7 gave an rms difference of 0.7 to 1.0 g/cm2. Retrievals of PW using 19.35 and 22.235 GHz channels and its comparison with near concurrent coastal radiosonde observations gave an rms difference of 0.32 g/cm2, comparable to the accuracy (0.2-0.4 g/cm2) obtained from previous satellite-borne microwave radiometers.
Item Type: | Article |
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Source: | Copyright of this article belongs to Elsevier Science. |
ID Code: | 57036 |
Deposited On: | 25 Aug 2011 12:57 |
Last Modified: | 25 Aug 2011 12:57 |
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