Radar reflectivity signatures and possible lead times of warnings for very large hail in Poland based on data from 2007-2015
Author:
Affiliation:
1. Institute of Earth Sciences , Faculty of Natural Sciences , University of Silesia in Katowice , Będzińska Str. 60, 41-200 Sosnowiec , Poland
2. Skywarn Poland Association , 29 Listopada Str. 18/19, 00-465 Warsaw , Poland
Abstract
Publisher
Walter de Gruyter GmbH
Subject
Management, Monitoring, Policy and Law,Nature and Landscape Conservation,Urban Studies,Pollution,Geography, Planning and Development
Link
https://www.sciendo.com/pdf/10.2478/environ-2020-0016
Reference57 articles.
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2. Bieringer P., Ray P.S. 1996. A Comparison of Tornado Warning Lead Times with and without NEXRAD Doppler Radar. Weather and Forecasting, 11: 47–52.
3. Brotzge J., Erickson S. 2009. NWS Tornado Warnings with Zero or Negative Lead Times. Weather and Forecasting, 24: 140–154.
4. Chisholm A.J., Renick J.H. 1972. The kinematics of multicell and supercell Alberta hailstorms. Alberta hail studies 1972. Research Council of Alberta Hail Studies Report, 72, 2: 24–31.
5. Czernecki B., Taszarek M., Kolendowicz L., Konarski J. 2016. Relationship between human observations of thunderstorms and the PERUN lightning detection network in Poland. Atmospheric Research, 167: 118–128.
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