Zobrazeno 1 - 10
of 32
pro vyhledávání: '"V. Kuell"'
Autor:
V. Kuell, Andreas Bott
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 148:117-140
With increasing resolution of numerical weather prediction (NWP) models, classical subgrid‐scale processes become increasingly resolved on the model grid. In particular, turbulence in the planetary boundary layer (PBL) is vertically already partial
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d120473b593054dafa48570fc1ed9cf7
https://doi.org/10.1002/qj.4195
https://doi.org/10.1002/qj.4195
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 146:2689-2716
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55e52aff5e19ca3e3d0daa8fec885137
https://doi.org/10.1002/qj.3812
https://doi.org/10.1002/qj.3812
Autor:
Andreas Bott, V. Kuell
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 145:767-783
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f06c649da4831e131971dc3c89a10a5a
https://doi.org/10.1002/qj.3464
https://doi.org/10.1002/qj.3464
Akademický článek
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Autor:
V. Kuell, Andreas Bott
Publikováno v:
Atmospheric Research. 143:176-197
For a long time, classical ensemble forecasts have concentrated on simulating the uncertainties of the observations by variations of the initial and boundary conditions. To supplement this with inherent contributions from the forecast model itself, s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae1159a6ddd3c96e574e5f54613573c9
https://doi.org/10.1016/j.atmosres.2014.01.027
https://doi.org/10.1016/j.atmosres.2014.01.027
Autor:
Andreas Bott, V. Kuell
Publikováno v:
Meteorologische Zeitschrift. 20:227-241
The hybrid mass flux convection scheme HYMACS has been proposed to simulate moist convection in non-hydrostatic numerical weather prediction models with grid sizes at which convection is partially resolved. Different to classical mass flux schemes HY
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e70c0854dca65f9debe5238acd7d383f
https://doi.org/10.1127/0941-2948/2011/0212
https://doi.org/10.1127/0941-2948/2011/0212
Autor:
V. Kuell, Andreas Bott
Publikováno v:
Atmospheric Research. 94:743-753
Convection can cause severe precipitation events and is thus of major interest for quantitative precipitation forecasts. Due to its small horizontal scale convection usually has to be parameterized in numerical weather prediction (NWP) models as a su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19c92fcce54f0a57ea5e412ba0c081f5
https://doi.org/10.1016/j.atmosres.2009.04.002
https://doi.org/10.1016/j.atmosres.2009.04.002
Publikováno v:
Advances in Space Research. 43:65-73
Water vapour measurements during the second mission of the CRyogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) instrument are presented in the altitude regime 8–20 km. Mixing ratios are shown on isentropic surfaces (300–50
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3267912d408db2b6b41e01ffab04f39c
https://doi.org/10.1016/j.asr.2008.06.019
https://doi.org/10.1016/j.asr.2008.06.019
Autor:
V. Kuell, Andreas Bott
Publikováno v:
Meteorologische Zeitschrift, Vol 17, Iss 6, Pp 775-783 (2008)
The correct representation of convection in numerical weather prediction (NWP) models is essential for quantitative precipitation forecasts. Due to its small horizontal scale convection usually has to be parameterized, e.g. by mass flux convection sc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e5b7a50dc4041d3eade7eb23c699525d
https://doi.org/10.1127/0941-2948/2008/0342
https://doi.org/10.1127/0941-2948/2008/0342
Autor:
V. Kuell, Hermann Jakobs, B. Schäler, Dirk Offermann, Hendrik Feldmann, Michael Memmesheimer, Adolf Ebel
Publikováno v:
Ecological Modelling. 217:240-254
Transport of atmospheric trace gases during a blocking event in the troposphere and lower stratosphere (UTLS) in August 1997 is studied. Considering the frequency of such events it is obvious that they play a significant role for climate and air chem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2830f8116901ccaea4d314747477054b
https://doi.org/10.1016/j.ecolmodel.2008.06.014
https://doi.org/10.1016/j.ecolmodel.2008.06.014