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
- 2024-2028: FWF (Austrian Science Fund) Stand-alone project P 37259, "DEmonstrating Parameter Estimation with eNsemble-based Data Assimilation for Boundary-Layer modElling over mountains"
- 2018-present: TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains – Programme and experiment)
- 2018-2022: FWF (Austrian Science Fund) Stand-alone project P 30808, "Multiscale Interactions in Convection Initiation in the Alps"
- 2012-2015: FWF (Austrian Science Fund) Stand-alone project P 24726, "STABLEST: Stable boundary layer separation and turbulence"
Links
- ORCID / ResearcherID / Scopus profiles
- Department of Atmospheric and Cryospheric Sciences (ACINN), University of Innsbruck
- Department of Civil, Environmental and Mechanical Engineering, University of Trento
- CETEMPS, University of L'Aquila
Publications
Boundary-layer plumes over mountainous terrain in idealized large-eddy simulations
- Author(s)
- Jan Weinkaemmerer, Matthias Göbel, Stefano Serafin, Ivan Bašták Ďurán, Jürg Schmidli
- Abstract
Coherent plume structures in the convective boundary layer over non-flat terrain are investigated using large-eddy simulation. A conditional sampling method based on the concentration of a decaying passive tracer is implemented in order to identify the boundary-layer plumes objectively. Conditional sampling allows quantification of the contribution of plume structures to the vertical transport of heat and moisture. A first set of simulations analyzes the flow over an idealized valley, where the terrain elevation only varies along one horizontal coordinate axis. In this case, vertical transport by coherent structures is the dominant contribution to the turbulent components of both heat and moisture flux. It is comparable in magnitude to the advective transport by the mean slope-wind circulation, although it is more important for heat than for moisture transport. A second set of simulations considers flow over terrain with a complex texture, drawn from an actual digital elevation model. In this case, conditional sampling is carried out by using a simple domain-decomposition approach. We demonstrate that thermal updrafts are generally more frequent on hill tops than over the surroundings, but they are less persistent on the windward sides when large-scale winds are present in the free atmosphere. Large-scale upper level winds tend to reduce the vertical moisture transport by the slope winds.
- Organisation(s)
- Department of Meteorology and Geophysics
- External organisation(s)
- Johann Wolfgang Goethe-Universität Frankfurt am Main, European Centre for Medium-Range Weather Forecasts (ECMWF), Leopold-Franzens-Universität Innsbruck
- Journal
- Quarterly Journal of the Royal Meteorological Society
- Volume
- 149
- Pages
- 3183-3197
- No. of pages
- 15
- ISSN
- 0035-9009
- DOI
- https://doi.org/10.1002/qj.4551
- Publication date
- 08-2023
- Peer reviewed
- Yes
- Austrian Fields of Science 2012
- 105207 Mountain meteorology, 105206 Meteorology
- Keywords
- ASJC Scopus subject areas
- Atmospheric Science
- Portal url
- https://ucrisportal.univie.ac.at/en/publications/dd8d8d36-d3ff-493d-9341-35b60eadaaf7