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Performance of high resolution X band radar for rainfall measurement in The Netherlands

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Figure

Fig. 1. Range and coverage of SOLIDAR. The white line indicatesthe line array of rain gauges, located from 3.75 to 10 km from theradar
Fig. 2b there is no clear trend in the radar event sums com-pared to that measured by the gauge, although there are morecases with underestimation than overestimation by the radar.
Fig. 2. (a) Rainfall accumulations larger than 1 mm of the gaugenearest to the radar (95 events in total)
Table 2. Bias [mm] and RMSE [mm] of the presented clutter cor-rection methods for different clutter area sizes.
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