stefano.serafin(at)univie.ac.at
Josef-Holaubek-Platz 2 (UZA II), 1090 Wien
Raumnummer: 2G556
T: +43-1-4277-537 13

Curriculum Vitae
- 2020: Senior Scientist, Universität Wien
- 2018: Habilitation (Italien), Fachgebiete 04/A4 (Geophysik) und 02/C1 (Astronomie, Astrophysik, Erdwissenschaften).
- 2018: Projektleiter, Universität Innsbruck
- 2010: Universitätsassistent Post-Doc, Universität Wien
- 2006: Doktorat Umwelttechnik, Universität Trient (Italien)
- 2002: Projektmitarbeiter, CETEMPS/Universität L'Aquila (Italien)
- 2002: Studium Umweltwissenschaften, Universität Milano-Bicocca (Italien)
- Vollständiger Lebenslauf
Forschungsinteressen
- Gebirgsmeteorologie
- Grenzschicht-Meteorologie
- Numerische Wettervorhersage
Projekte
- 2018-heute: TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains – Programme and experiment)
- 2018-2022: FWF-Einzelprojekt P30808-N32, "Multiscale Interactions in Convection Initiation in the Alps"
- 2012-2015: FWF-Einzelprojekt P24726-N27, "STABLEST: Ablösung und Turbulenz der stabilen Grenzschicht"
Links
- ORCID / ResearcherID / Scopus profiles
- Institut für Atmosphären- und Kryosphärenwissenschaften (ACINN), Universität Innsbruck
- Department of Civil and Environmental Engineering, Universität Trient
- CETEMPS, Universität L'Aquila
Publikationen
A pan-Alpine climatology of lightning and convective initiation.
- Autor(en)
- Agostino Manzato, Stefano Serafin, Mario Marcello Miglietta, Daniel J. Kirshbaum, Wolfgang Schulz
- Abstrakt
A new lightning-flash and convective initiation climatology is developed over the Alpine area, one of the hotspots for lightning activity in Europe. The climatology uses cloud-to-ground (CG) data from the European Cooperation for Lightning Detection (EUCLID) network, occurring from 2005 to 2019. The CG lightning data are gridded at a resolution of approximately 2 km and 10 min. A new and simple method of identifying convective initiation (CI) events applies a spatiotemporal mask to the CG data to determine CI timing and location. Although the method depends on a few empirical thresholds, sensitivity tests show the results to be robust. The maximum activity for both CG flashes and CI events is observed from mid-May to mid-September, with a peak at the end of July; the peak in the diurnal cycle occurs in the afternoon. CI is mainly concentrated over and around the Alps, particularly in northern and northeastern Italy. Since many thunderstorms follow the prevailing midlatitude westerly flow, a peak of CG flashes extends from the mountains into the plains and coastal areas of northeastern Italy and Slovenia. CG flashes and CI events over the sea/coast occur less frequently than in plains and mountains, have a weaker diurnal cycle, and have a seasonal maximum in autumn instead of summer.
- Organisation(en)
- Institut für Meteorologie und Geophysik
- Externe Organisation(en)
- ARPA FVG–OSMER, Instituto di Scienze dell'Atmosfera e del Clima, McGill University, Austrian Lightning Detection and Information System
- Journal
- Monthly Weather Review
- Band
- 150
- Seiten
- 2213-2230
- Anzahl der Seiten
- 18
- ISSN
- 0027-0644
- DOI
- https://doi.org/10.1175/MWR-D-21-0149.1
- Publikationsdatum
- 09-2022
- Peer-reviewed
- Ja
- ÖFOS 2012
- 105204 Klimatologie
- Schlagwörter
- ASJC Scopus Sachgebiete
- Atmospheric Science
- Link zum Portal
- https://ucrisportal.univie.ac.at/de/publications/5048c4b3-dba1-401e-b7ae-5a135219dd34
