Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Davide Panosetti"'
Hail is by far the greatest contributor to insured losses from severe convective storms on an annual basis. Individual severe convective storm outbreaks can cause hail losses well above EUR 1 bn. In May and June 2022 a series of such events impacted
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e67a7bead70303331275152bc213d7ea
https://doi.org/10.5194/egusphere-egu23-10212
https://doi.org/10.5194/egusphere-egu23-10212
Hail is by far the greatest contributor to insured losses from severe convective storms on an annual basis. Individual severe convective storm outbreaks can cause hail losses well above EUR 1 bn. On 19-22 June 2022 a series of such events impacted Fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::882ac7e3c991960436e9bc9ed228122f
https://doi.org/10.5194/ecss2023-69
https://doi.org/10.5194/ecss2023-69
Publikováno v:
Monthly Weather Review, 148 (6)
Currently, major efforts are under way to refine the horizontal resolution of weather and climate models to kilometer-scale grid spacing (Dx). Besides refining the representation of the atmospheric dynamics and enabling the use of explicit convection
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::789ee16599706022b2f5772f18a2e5a6
https://doi.org/10.1175/mwr-d-19-0247.1
https://doi.org/10.1175/mwr-d-19-0247.1
Publikováno v:
Journal of Climate. 33:1915-1933
The “gray zone” of convection is defined as the range of horizontal grid-space resolutions at which convective processes are partially but not fully resolved explicitly by the model dynamics (typically estimated from a few kilometers to a few hun
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e98a1871318c018b9fe28f197c9c9200
https://doi.org/10.1175/jcli-d-19-0286.1
https://doi.org/10.1175/jcli-d-19-0286.1
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 145:1427-1443
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::285c25b02fdfbcb692592a4b00108e21
https://doi.org/10.1002/qj.3502
https://doi.org/10.1002/qj.3502
Autor:
Heini Wernli, Stefano Ubbiali, Salvatore Di Girolamo, Xavier Lapillonne, Nikolina Ban, Torsten Hoefler, Christophe Charpilloz, Andrea Arteaga, David Leutwyler, Oliver Fuhrer, Christoph Schär, Katherine Osterried, Davide Panosetti, Stefan Rüdisühli, Linda Schlemmer, Thomas C. Schulthess, Michael Sprenger, Laureline Hentgen
Publikováno v:
Bulletin of the American Meteorological Society, 101 (5)
Bulletin of the American Meteorological Society
Bulletin of the American Meteorological Society
Currently major efforts are underway toward refining the horizontal resolution (or grid spacing) of climate models to about 1 km, using both global and regional climate models (GCMs and RCMs). Several groups have succeeded in conducting kilometer-sca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::12e754fffa78ced1eb4de449bda967a2
https://hdl.handle.net/20.500.11850/389770
https://hdl.handle.net/20.500.11850/389770
Autor:
Davide Panosetti, Stephen Cusack
Ten years ago, we studied 101 years (1910-2010) of wind observations at five stations spread throughout the Netherlands, and representative of a wider area in Europe containing regions of dense exposure. The raw wind speed data were homogenised using
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8ef15aca22fc3ea362e8321b2d89fe1e
https://doi.org/10.5194/egusphere-egu2020-7462
https://doi.org/10.5194/egusphere-egu2020-7462
Publikováno v:
Climate Dynamics. 55:215-234
Convection-resolving models (CRMs) can explicitly simulate deep convection and resolve interactions between convective updrafts. They are thus increasingly used in numerous weather and climate applications. However, the truncation of the continuous e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a9f904bbeb2b9c32840373d07ee746d
https://doi.org/10.1007/s00382-018-4229-9
https://doi.org/10.1007/s00382-018-4229-9
On summertime fair-weather days, thermally driven wind systems play an important role in determining the initiation of convection and the occurrence of localized precipitation episodes over mountainous terrain. This study compares the mechanisms of c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c1e24562496256982a6d5a341faa03ce