Polarimetric radar identification of frozen hydrometeors in thunderstorm precipitation: 6 August 2010


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CSU-CHILL radar data indicating that both hail (positive Hail Differential Reflectivity; HDR) and heavy rain (large specific differential propagation phase; Kdp) are present in a low elevation PPI sweep through a thunderstorm. A series of plots documenting the time evolution of this hail / rain mixture have been prepared.

6aug2010 2234 HDR Kdp anot.png



An isolated thunderstorm that passed over the northern portions of Denver was observed during the afternoon hours of 6 August 2010. The CSU-CHILL data that was collected in a series of low elevation angle PPI scans was processed using the methods of Cifelli et al (JTEC 2010) to estimate specific differential propagation phase (Kdp) and to identify range gates where hail was a significant precipitation component. The grey shades in the following plot show an example of the three hydrometeor categories that were identified in a 0.5 deg PPI scan at 2234 UTC:

Anot 2234 web.png

Hydrometeor classification loop

The following loop shows the evolution of these hydrometeor classifications during the 2226 - 2246 UTC time period. The diagnosed level of ice contamination becomes insignificant by the end of the loop.

Click play to begin animation

Delay: ms


CSU-CHILL 2234:11 UTC 0.5 deg elevation PPI plots

Since hailstones generally have larger backscattering cross sections than raindrops, the presence of hail complicates the estimation of rain rates from the co-polar reflectivity level. The CHILL radar observed reflectivity levels reaching the 50 - 60 dBZ range at 2234 UTC. As shown in the preceding loop, hail contamination was also detected at this time:

SP2 CHILL 223411 z anot.png

Using the CSU HIDRO methods of Cifelli et al (JTEC 2010), reflectivity-based rain rate formulations are not used at locations where ice contamination has been diagnosed; Kdp-based rate estimates are used in these areas. The CSU-HIDRO rain rate field is shown in the next plot. Rain rates peak at values of ~120 mm / hr:

SP2 CHILL 223411 HIDRO anot.png

KFTG 2233:01 UTC 0.5 deg elevation PPI plots

The next two plots were generated from data collected by the NWS KFTG WSR-88D radar at 2233:01 UTC (approximately one minute earlier than the CHILL scan shown above). Due to the shorter range (~30 km vs. ~80 km), the NWS 0.5 deg PPI data was collected closer to the ground with smaller pulse volume widths in the azimuthal direction. Nevertheless, similar echo patterns are evident:

SP2 KFTG 223301 z anot.png

Current (i.e., before the polarimetric upgrade) NWS rain rate estimations are based only on co-polar reflectivity. To reduce over estimates due to hail, a reflectivity limit of 53 dBZ is applied before the "Z(R)" rain rate calculation is done. This translates into a maximum rate of 103 mm / hr. The effect of this artificial limit can be seen in the following plot. The Kdp-based rate estimations provided by dual-polarization data improve the remote sensing of rain rates in the presence of hail contamination.

SP2 KFTG 223301 Z88 anot.png