Dr. Stefano SERAFIN


stefano.serafin(at)univie.ac.at

Josef-Holaubek-Platz 2 (UZA II), 1090 Vienna
Roomnumber: 2G556
T: +43-1-4277-537 13


  • 2020: Senior Scientist, University of Vienna
  • 2018: National scientific qualification (Italy), disciplines 04/A4 (Geophysics) and 02/C1 (Astronomy, Astrophysics, Earth and Planetary Sciences)
  • 2018: Project leader, University of Innsbruck
  • 2010: Assistant professor, University of Vienna
  • 2006: Doctorate in Environmental Engineering, University of Trento (Italy)
  • 2002: Project scientist, CETEMPS/University of L'Aquila (Italy)
  • 2002: Degree in Environmental Science, University of Milano-Bicocca (Italy)
  • Complete curriculum vitae

Research Interests

  • Mountain meteorology
  • Dynamic meteorology
  • Numerical weather prediction
  • Boundary-layer meteorology

Projects

Publications

Moist orographic convection: Physical mechanisms and links to surface-exchange processes

Author(s)
D.J. Kirshbaum, Bianca Adler, N. Kalthoff, C. Barthlott, S. Serafin
Abstract

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(s)
Department of Meteorology and Geophysics
External organisation(s)
Karlsruher Institut für Technologie
Journal
Atmosphere
Volume
9
ISSN
2073-4433
DOI
https://doi.org/10.3390/atmos9030080
Publication date
02-2018
Peer reviewed
Yes
Austrian Fields of Science 2012
105206 Meteorology, 105207 Mountain meteorology
Keywords
ASJC Scopus subject areas
Environmental Science (miscellaneous)
Portal url
https://ucrisportal.univie.ac.at/en/publications/37ac8535-46cf-45d1-8c16-3c8ae49b6e45