APPLICATION OF KDP EVOLUTION ON THE VERY-SHORT-RANGE RAINFALL FORECAST
On 16 October 2021, localized torrential rainfall (> 70 mm h-1) occurred in the slope area of northern Taiwan during an approaching surface front. Flash floods downstream of the catchment area resulted in a severe drowning accident without warning. In this observational study, the newly-established C-band disaster prevention rainfall radar in northern Taiwan is used for analysis and comparison. At 15-18 local time (LST), extreme values of the specific differential phase KDP (> 2° km-1) can be used to identify the heavy rainfall region’s location, intensity, and movement. For flash floods downstream of the catchment area, potentially, there is a priori warning capability. In this event, tracking intense and concentrated KDP on complex terrain has an advantage over radar reflectivity. The direct application of KDP on quantitative precipitation estimates can effectively complement the transmission-delay problem of ground rain gauges.