Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Jan Weinkaemmerer"'
Publikováno v:
Journal of the Atmospheric Sciences. 79:2685-2701
The vertical heat and moisture exchange in the convective boundary layer over mountainous terrain is investigated using large-eddy simulation. Both turbulent and advective transport mechanisms are evaluated over the simple orography of a quasi-two-di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d2aa1cec5cbb547ef16a98282b3bbb5
https://doi.org/10.1175/jas-d-21-0195.1
https://doi.org/10.1175/jas-d-21-0195.1
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
Publikováno v:
Quarterly Journal of the Royal Meteorological Society, 148 (749)
The formation of low stratus cloud over idealized hills is investigated using numerical model simulations. The main driver for the cloud formation is radiative cooling due to outgoing longwave radiation. Despite a purely horizontal flow, the advectio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b3ceb361ae34d37e1609fd3faaf6db2
Orography induced gravity waves are investigated in a Multi Scale Gravity Wave Model (MS-GWaM) over idealized topography. MS-GWaM is a prognostic gravity-wave model, which parametrizes both the propagation and dissipation of subgrid-scale GWs. It is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13ad0089b12300fa4bafeed2d42c63b6
https://doi.org/10.5194/egusphere-egu2020-10957
https://doi.org/10.5194/egusphere-egu2020-10957
In the convective boundary layer over mountainous regions, the mean values and the fluxes of quantities like heat, mass, and momentum are strongly influenced by thermally induced flows. Several studies have pointed out that the enhanced warming of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63a1812530ac8b64ddf8fecfb44babd0
https://doi.org/10.5194/egusphere-egu2020-8101
https://doi.org/10.5194/egusphere-egu2020-8101