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
Moist orographic convection: Physical mechanisms and links to surface-exchange processes
- Autor(en)
- D.J. Kirshbaum, Bianca Adler, N. Kalthoff, C. Barthlott, S. Serafin
- Abstrakt
This paper reviews the current understanding of moist orographic convection and its regulation by surface-exchange processes. Such convection tends to develop when and where moist instability coincides with sufficient terrain-induced ascent to locally overcome convective inhibition. The terrain-induced ascent can be owing to mechanical (airflow over or around an obstacle) and/or thermal (differential heating over sloping terrain) forcing. For the former, the location of convective initiation depends on the dynamical flow regime. In "unblocked" flows that ascend the barrier, the convection tends to initiate over the windward slopes, while in "blocked" flows that detour around the barrier, the convection tends to initiate upstream and/or downstream of the high terrain where impinging flows split and rejoin, respectively. Processes that destabilize the upstream flow for mechanically forced moist convection include large-scale moistening and ascent, positive surface sensible and latent heat fluxes, and differential advection in baroclinic zones. For thermally forced flows, convective initiation is driven by thermally direct circulations with sharp updrafts over or downwind of the mountain crest (daytime) or foot (nighttime). Along with the larger-scale background flow, local evapotranspiration and transport of moisture, as well as thermodynamic heterogeneities over the complex terrain, regulate moist instability in such events. Longstanding limitations in the quantitative understanding of related processes, including both convective preconditioning and initiation, must be overcome to improve the prediction of this convection, and its collective effects, in weather and climate models.
- Organisation(en)
- Institut für Meteorologie und Geophysik
- Externe Organisation(en)
- Karlsruher Institut für Technologie
- Journal
- Atmosphere
- Band
- 9
- ISSN
- 2073-4433
- DOI
- https://doi.org/10.3390/atmos9030080
- Publikationsdatum
- 02-2018
- Peer-reviewed
- Ja
- ÖFOS 2012
- 105206 Meteorologie, 105207 Gebirgsmeteorologie
- Schlagwörter
- ASJC Scopus Sachgebiete
- Environmental Science (miscellaneous)
- Link zum Portal
- https://ucrisportal.univie.ac.at/de/publications/37ac8535-46cf-45d1-8c16-3c8ae49b6e45
