Ahmet Ãztopal, Albero Mugnai, Daniele Casella, Marco ... - H-SAF
Ahmet Ãztopal, Albero Mugnai, Daniele Casella, Marco ... - H-SAF
Ahmet Ãztopal, Albero Mugnai, Daniele Casella, Marco ... - H-SAF
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Figure 5.8. 91.66 GHz vs. 150 GHz scatterplot of SSMIS simulated and measured TBs.Figure 5.9 presents intense water vapor line absorption frequencies at 183.31 GHz.Herein, the surface emissivity impact is negligible, but overall simulation consistencyshows the ice contents, which are simulated by the UW-NMS model. Accordingly,appropriate ice scattering parameterizations are adopted especially at higher cloudportions.Figure 5.9. 183.31±3 GHz vs. 183.31±7 GHz scatterplot of SSMIS simulated andmeasured TBs.5.2. Applications of the CDRD Algorithm5.2.1. Comparisions of Radar and RetrievalIn Figure 5.12a, scatter diagrams are obtained by considerations of 1x1 and 3x3resolution rain rate retrivals versus radar values, respectively. According to 45 degree line,the overall regression line indicates overestimation results with a very significant variability19