Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Stefano Serafin"'
Autor:
Stefano Serafin, Bianca Adler, Joan Cuxart, Stephan F. J. De Wekker, Alexander Gohm, Branko Grisogono, Norbert Kalthoff, Daniel J. Kirshbaum, Mathias W. Rotach, Jürg Schmidli, Ivana Stiperski, Željko Večenaj, Dino Zardi
Publikováno v:
Atmosphere, Vol 9, Iss 3, p 102 (2018)
The exchange of heat, momentum, and mass in the atmosphere over mountainous terrain is controlled by synoptic-scale dynamics, thermally driven mesoscale circulations, and turbulence. This article reviews the key challenges relevant to the understandi
Externí odkaz:
https://doaj.org/article/9e857df1428f43ab8131844961a66987
Publikováno v:
Atmosphere, Vol 9, Iss 3, p 80 (2018)
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 locall
Externí odkaz:
https://doaj.org/article/204cd1e4b2274c8296f5dc2c91ae4e8f
Autor:
Ivana Stiperski, Stefano Serafin, Alexandre Paci, Hálfdán Ágústsson, Anne Belleudy, Radiance Calmer, Kristian Horvath, Christoph Knigge, Johannes Sachsperger, Lukas Strauss, Vanda Grubišić
Publikováno v:
Atmosphere, Vol 8, Iss 1, p 13 (2017)
In this article, we present an overview of the HyIV-CNRS-SecORo (Hydralab IV-CNRS-Secondary Orography and Rotors Experiments) laboratory experiments carried out in the CNRM (Centre National de Recherches Météorologiques) large stratified water flum
Externí odkaz:
https://doaj.org/article/0059115526954937a8896f38e9c15166
Publikováno v:
eISSN
Diurnal mountain winds precondition the environment for deep moist convection through horizontal and vertical transport of heat and moisture. They also play a key role in convection initiation, especially in strongly inhibited environments, by liftin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ba0f541ec709747109c65c5dcbd51d0
https://doi.org/10.5194/egusphere-2023-648
https://doi.org/10.5194/egusphere-2023-648
Publikováno v:
Geoscientific Model Development, Vol 15, Pp 669-681 (2022)
Numerically accurate budgeting of the forcing terms in the governing equations of a numerical weather prediction model is hard to achieve. Because individual budget terms are generally 2 to 3 orders of magnitude larger than the resulting tendency, ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1db5e7e4cbba5badbd061c2fd9b2ed8e
https://doi.org/10.5194/gmd-15-669-2022
https://doi.org/10.5194/gmd-15-669-2022
Autor:
Agostino Manzato, Stefano Serafin, Mario Marcello Miglietta, Daniel Kirshbaum, Wolfgang Schulz
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::05f4d9f9a33808ce1c5fce97a9a241a9
https://doi.org/10.5194/egusphere-plinius17-37
https://doi.org/10.5194/egusphere-plinius17-37
Local thermal circulations developing over heated valley slopes strongly influence the convective boundary layer (CBL) over mountainous terrain. For this study, large-eddy simulations are carried out both over idealized valleys and semi-idealized com
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aba20b9643a814a91824dc87cf9ca4e0
https://doi.org/10.5194/ems2022-621
https://doi.org/10.5194/ems2022-621
Processes on the meso-gamma scale play an essential role in triggering deep moist convection. In mountainous terrain, thermally-driven circulations–such as slope, valley, and plain-to-mountain winds–can provide the necessary trigger mechanism to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c8a24d472f1012a7a9ff4d89938f33e
https://doi.org/10.5194/ems2022-478
https://doi.org/10.5194/ems2022-478
Autor:
Wolfgang Schöner, Nicholas Pepin, Enrico Arnone, Andreas Gobiet, Klaus Haslinger, Sven Kotlarski, Claudia Notarnicola, Elisa Palazzi, Petra Seibert, Stefano Serafin, Silvia Terzago, James M. Thornton, Mathias Vuille, Carolina Adler
Mountains and high elevation regions are often viewed as climate change “hotspots” which are responding particularly rapid to global climate forcing and may anticipate or amplify what is occurring elsewhere. Accelerating mountain climate change h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ecccbd08e0eeb17d1cbd45f73e5eb2a5
https://doi.org/10.5194/egusphere-egu22-11304
https://doi.org/10.5194/egusphere-egu22-11304
Autor:
Stefano Serafin, Emily Potter
The climatological frequency of deep moist convection is enhanced in the vicinity of mountainous regions. Most studies to date focus on convection initiation (CI) on the windward side of mountains, but uplift and CI can also occur on their lee side.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cc3cefeb637b85a48fc2e28fb35fb84
https://doi.org/10.5194/egusphere-egu22-9456
https://doi.org/10.5194/egusphere-egu22-9456