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Polarimetric Radar Convective Cell Tracking Reveals Large Sensitivity of Cloud Precipitation and Electrification Properties to CCN
Author(s) -
Hu Jiaxi,
Rosenfeld Daniel,
Ryzhkov Alexander,
Zrnic Dusan,
Williams Earle,
Zhang Pengfei,
Snyder Jeffrey C.,
Zhang Renyi,
Weitz Richard
Publication year - 2019
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1029/2019jd030857
Subject(s) - cloud condensation nuclei , cloud base , radar , convective available potential energy , convection , precipitation , environmental science , meteorology , atmospheric sciences , lightning (connector) , cloud computing , aerosol , geology , geography , physics , aerospace engineering , computer science , engineering , power (physics) , quantum mechanics , operating system
Hypotheses have been proposed for decades about the effect of activated cloud condensation nuclei (CCN) on delaying the warm rain process, invigorating deep convective cloud vertical development, and enhancing mixed‐phase processes. Observational support has been only qualitative with mixed results due to the lack of regional measurements of CCN concentration (N CCN ), while simulations have not produced a robust consensus. Quantitative assessments of these relationships became possible with the advent of N CCN retrievals from satellites; when combined with measurements by polarimetric radar and Lightning Mapping Array (LMA), tracking convective cells observed on radar and examining precipitation properties throughout the cells' life cycle has permitted the study of the impact of N CCN on cloud and precipitation characteristics. We composited more than 2,800 well‐tracked cells in the Houston region and stratified them by N CCN , convective available potential energy (CAPE), and urban/rural locations. The results show that increased N CCN invigorates the convection until saturation near N CCN = 1,000 cm 3 ; increasing N CCN from ~400 to an optimum of ~1,000 cm 3 increases lightning activity by an order of magnitude. A further increase in CCN decreases lightning rates. Adding CAPE enhances lightning only under low N CCN (e.g., less than 500 cm 3 ). The presence of the urban area enhances lightning for similar N CCN concentrations, although this applies mainly under low N CCN conditions. The urban heat island as manifested by cloud base height cannot explain this observation. It is suspected that the urban ultrafine aerosols contribute to the storm electrification.