Publication:
Differential reflectivity columns and hail - linking C-band radar-based estimated column characteristics to crowdsourced hail observation sin Switzerland

cris.virtual.author-orcid0000-0002-8645-4702
cris.virtualsource.author-orcid555b2587-a51d-4e11-aec5-3142afa367df
cris.virtualsource.author-orcidaa27dc00-7048-475b-bdec-36177f27d06f
cris.virtualsource.author-orcidwill be referenced::ORCID::0000-0002-8539-7080
cris.virtualsource.author-orcidwill be referenced::ORCID::0000-0003-2043-3981
dc.contributor.authorAregger, Martin
dc.contributor.authorMartius, Olivia
dc.contributor.authorGermann, Urs
dc.contributor.authorHering Alessandro Michele
dc.date.accessioned2025-05-14T06:26:58Z
dc.date.available2025-05-14T06:26:58Z
dc.date.issued2024-10-14
dc.description.abstractDifferential reflectivity columns (ZDRC) have been shown to provide information about a storm's updraft intensity and size. The updraft's characteristics, in turn, influence a severe storm's propensity to produce hail and the size of said hail. Consequently, there is the potential to use ZDRC for the detection and sizing of hail. In this observational study, we investigate the characteristics of ZDRC (volume, height, area, maximum ZDR within) automatically detected on an operational C-band radar network in Switzerland and relate them to hail on the ground using 173'000 crowdsourced hail reports collected over a period of 3.5 years. We implement an adapted version of an established ZDRC detection algorithm on a 3D composite of ZDR data derived from five Swiss weather radars. The composite, in combination with the dense network of radars located on differing altitudes up to 3000 m.a.s.l, helps to counteract the effects of the complex topography of the study region. The alpine region presents visibility and data quality challenges, which are especially crucial for measuring ZDRC. Our analysis finds ZDRC present in most hail-producing storms, with higher frequencies in storms producing severe hail. Further, when looking at lifetime maximum values, we find significant differences in various ZDRC characteristics between hail-producing and non-hail-producing storms. We also attempt to determine thresholds to differentiate between storm types. The temporal evolution of the ZDRC proves challenging to investigate due to their intermittent nature. Nevertheless, the peak values of the ZDRC characteristics are most often measured 5-10 minutes before the first hail reports on the ground, highlighting the potential for ZDRC to be used in warning applications.
dc.description.numberOfPages21
dc.description.sponsorshipInstitute of Geography, Climatology
dc.description.sponsorshipFederal Office of Meteorology and Climatology MeteoSwiss
dc.description.sponsorshipGeographisches Institut (GIUB) - Klimafolgenforschung
dc.description.sponsorshipOeschger Centre for Climate Change Research (OCCR)
dc.description.sponsorshipOeschger Centre for Climate Change Research (OCCR) - MobiLab
dc.identifier.doi10.48620/88011
dc.identifier.publisherDOI10.48550/arXiv.2410.10499
dc.identifier.urihttps://boris-portal.unibe.ch/handle/20.500.12422/210943
dc.language.isoen
dc.publisherCornell University
dc.relation.fundingSwiss National Science Foundation, SsClim Project
dc.relation.grantnoCRSII5_201792
dc.relation.ispartofseriesarXiv
dc.relation.producthttps://github.com/MartinAregger/ZDRC_Calculator_QJ_2024
dc.subjectDifferential Reflectivity Columns
dc.subjectHail Sizing
dc.subjectC-Band radar
dc.subjectCrowdsourcing
dc.subjectConvetive Storms
dc.subjectAlpine Topography
dc.subjectNowcasting
dc.subject.ddc000 - Computer science, knowledge & systems
dc.subject.ddc500 - Science::530 - Physics
dc.subject.ddc500 - Science
dc.subject.ddc900 - History::910 - Geography & travel
dc.titleDifferential reflectivity columns and hail - linking C-band radar-based estimated column characteristics to crowdsourced hail observation sin Switzerland
dc.typeworking_paper
dspace.entity.typePublication
oairecerif.author.affiliationGeographisches Institut (GIUB) - Klimafolgenforschung
oairecerif.author.affiliationInstitute of Geography, Climatology
oairecerif.author.affiliationFederal Office of Meteorology and Climatology MeteoSwiss
oairecerif.author.affiliationFederal Office of Meteorology and Climatology MeteoSwiss
oairecerif.author.affiliation2Oeschger Centre for Climate Change Research (OCCR)
oairecerif.author.affiliation2Oeschger Centre for Climate Change Research (OCCR) - MobiLab
oairecerif.author.affiliation3Oeschger Centre for Climate Change Research (OCCR)
unibe.additional.sponsorshipOeschger Centre for Climate Change Research (OCCR)
unibe.additional.sponsorshipOeschger Centre for Climate Change Research (OCCR) - MobiLab
unibe.contributor.rolecorresponding author
unibe.contributor.roleauthor
unibe.contributor.roleauthor
unibe.contributor.roleauthor
unibe.description.ispublishedpub
unibe.refereedtrue

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