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Improvement of hail detection and nowcasting by synergistic combination of information from polarimetric radar, model predictions, and in-situ observations

dc.contributor.advisorTrömel, Silke
dc.contributor.authorSchmidt, Mari Luna
dc.date.accessioned2020-10-21T09:41:31Z
dc.date.available2020-10-21T09:41:31Z
dc.date.issued21.10.2020
dc.identifier.urihttps://hdl.handle.net/20.500.11811/8701
dc.description.abstractLarge hail can pose a major threat to people, infrastructure, and property. While polarimetric radar observations enable us to reliably detect hail, discrimination of hail size and strategies to nowcast and predict hail and its size are still subject of research. At S band hail size discrimination algorithms do already exist, while retrievals from C-band radars, which are more widespread in Europe, remain challenging due to resonance scattering effects from large raindrops which tend to interfere with large hail signatures.
Advanced nowcasting tools capable of detecting hail and discriminating its size at C band are required to enable earlier and more precise severe weather warnings being issued by weather services in Europe. In this thesis 16 severe hail events monitored with the polarimetric C-band radar network of the German national meteorological service (Deutscher Wetterdienst, DWD) are investigated together with hail reports from the European Severe Weather Database (ESWD; https://www.eswd.eu/) for precursory information. This data set includes the largest hailstone (14.1 cm in diameter) reported so far in Germany hitting the ground in Undingen on August 6, 2013.
First, an algorithm for correcting anomalously high attenuation in hail-bearing thunderstorms is evaluated using four overlapping C-band radars. Post-processing of polarimetric moments, like spike-filtering of differential phase, is done to reduce noise and improve attenuation corrections. Results illustrate the capability to mitigate attenuation of up to 15 db km-1 but only small overcorrection in precipitation without hail.
Second, T-matrix scattering simulations for dry and wet hail are conducted to adjust a fuzzy logic based hail size discrimination algorithm (HSDA) developed for S band for usage at C band. Hereby, dual-layered spheroids are simulated to mimic melting hail. The revised fuzzy logic utilizes an ad-hoc weighting of input variables to improve performance through self-adjustment similar to other unsupervised learning techniques.
Finally, hail precursors and storm dynamics are investigated in an object-based, precipitation system oriented analysis to develop and evaluate nowcasting tools to detect hail growth and predict the hail's terminal diameter. This analysis utilizes a custom-made cell tracker and exploits the results of the attenuation correction algorithm.
Results show that sudden increases of the vertical extent of columns of enhanced differential reflectivity ZDR, so called ZDR-columns, precede peaks of strong signal attenuation most probably linked to hail. Also, strong attenuation was often accompanied by specific differential phase KDP above 10 ° km-1. It is demonstrated that the intensity of ZDR-columns, described e.g. by their maximum ZDR value, and the height of ZDR-columns above the melting layer, allow for nowcasting hail size at the ground with lead times between 10 and 20 minutes, which can be exploited for warnings.
en
dc.language.isoeng
dc.relation.ispartofseriesBonner Meteorologische Abhandlungen ; 91
dc.rightsIn Copyright
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectHagel
dc.subjectRadar
dc.subjectUnwetter
dc.subjectPolarimetrie
dc.subjectKürzestfristvorhersage
dc.subjectDämpfung
dc.subjectPolarimetric
dc.subjectNowcasting
dc.subjectHail
dc.subjectSevere Weather
dc.subjectAttenuation
dc.subject.ddc550 Geowissenschaften
dc.titleImprovement of hail detection and nowcasting by synergistic combination of information from polarimetric radar, model predictions, and in-situ observations
dc.typeDissertation oder Habilitation
dc.publisher.nameUniversitäts- und Landesbibliothek Bonn
dc.publisher.locationBonn
dc.rights.accessRightsopenAccess
dc.identifier.urnhttps://nbn-resolving.org/urn:nbn:de:hbz:5-59784
dc.relation.eissn0006-7156
ulbbn.pubtypeErstveröffentlichung
ulbbnediss.affiliation.nameRheinische Friedrich-Wilhelms-Universität Bonn
ulbbnediss.affiliation.locationBonn
ulbbnediss.thesis.levelDissertation
ulbbnediss.dissID5978
ulbbnediss.date.accepted21.08.2020
ulbbnediss.instituteMathematisch-Naturwissenschaftliche Fakultät : Fachgruppe Erdwissenschaften / Institut für Geowissenschaften
ulbbnediss.fakultaetMathematisch-Naturwissenschaftliche Fakultät
dc.contributor.coRefereeSimmer, Clemens


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