Operational application of combined radar and raingauges precipitation estimation at the CHMI
Md Fahim Salek, Petr Novák, D. Seo
Abstract
Md Fahim Salek, Petr Novák, D. Seo
Abstract
The Czech Hydrometeorological Institute (CHMI) runs two C-band Doppler weather radars which provide good coverage of precipitation over the area of the Czech Repub- lic. For the quantitative precipitation estimation (QPE), re- flectivity from pseudoCAPPI level of 2 km above sea level is used and the rainfall rate is then obtained by a constant Z-R relationship. Since the radar-only-based QPE is not consid- ered satisfactory, some corrections have been introduced in order to achieve better accuracy of the instant precipitation estimates. The corrections include the algorithm using verti- cal profile of reflectivity which reduces the range-dependent underestimation of single radar estimates, raingauge-based adjustment and combination with available raingauge mea- surements. The adjustment using single coefficient over the radar domains is based on collocated radar and raingauge measurements in a time-moving window whose length is an adaptable parameter. The combination of the adjusted radar QPE with available raingauge measurements is achieved by a simplified method of double optimal estimation. The sys- tem is in routine operation for precipitation accumulation of 1, 6 and 24 h and the results are available in HTML format. It serves for warning purposes, for NWP model verification and hydrological applications at the CHMI. The visualiza- tion allows for quick comparison of radar, radar-adjusted, raingauge-only and combined estimates along with mean areal QPE for predefined catchments using all mentioned es- timates. The instant comparisons and some additional diag- nostic information allows to see better the deficiencies and errors of the two complementary estimation systems.
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The Czech Hydrometeorological Institute (CHMI) runs two C-band Doppler weather radars which provide good coverage of precipitation over the area of the Czech Repub- lic. For the quantitative precipitation estimation (QPE), re- flectivity from pseudoCAPPI level of 2 km above sea level is used and the rainfall rate is then obtained by a constant Z-R relationship. Since the radar-only-based QPE is not consid- ered satisfactory, some corrections have been introduced in order to achieve better accuracy of the instant precipitation estimates. The corrections include the algorithm using verti- cal profile of reflectivity which reduces the range-dependent underestimation of single radar estimates, raingauge-based adjustment and combination with available raingauge mea- surements. The adjustment using single coefficient over the radar domains is based on collocated radar and raingauge measurements in a time-moving window whose length is an adaptable parameter. The combination of the adjusted radar QPE with available raingauge measurements is achieved by a simplified method of double optimal estimation. The sys- tem is in routine operation for precipitation accumulation of 1, 6 and 24 h and the results are available in HTML format. It serves for warning purposes, for NWP model verification and hydrological applications at the CHMI. The visualiza- tion allows for quick comparison of radar, radar-adjusted, raingauge-only and combined estimates along with mean areal QPE for predefined catchments using all mentioned es- timates. The instant comparisons and some additional diag- nostic information allows to see better the deficiencies and errors of the two complementary estimation systems.
Key concepts: Quantitative precipitation estimation, Radar, Rain gauge, Precipitation, Environmental science, Remote sensing, Quantitative precipitation forecast, Meteorology