DR column; KDP column"/> DR arcs and KDP high-value areas were important characteristics of the lower layer. The ZDR arcs matched the high-value region of reflectivity factor gradient on one side of the inflow and correspond to smaller KDP, which were caused by a few large particles. The KDP high-value area in the middle of the storm, corresponding to the smaller ZDR (1-3 dB), larger CC, caused by the high concentration of smaller particles, was the heavy rainfall area. (3) TheZDR ring around BWER, corresponding to smaller KDP, indicate that a small number of large droplets were distributed around BWER. The deep and wide ZDR and KDP columns above the BWER indicate that the higher concentration of large droplets was distributed above the BWER. (4) Abundant liquid particles under the -20 ℃ layer and abundant graupel and ice crystal particles above the -20 ℃ layer were the typical vertical characteristics of the microphysics of the Gaomi supercell."/>
Archive > Volume 50 Issue 6 > 2022,50(6):830-841. DOI:10.19517/j.1671-6345.20220040 Prev Next

Polarimetric Signatures of a Supercell Thunderstorm Occourred in Gaomi on 3 August 2020

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