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TZID:Europe/Berlin
TZUNTIL:20190331T010000Z
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DTSTART:20161030T030000
TZOFFSETFROM:+0200
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RDATE:20181028T030000
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UID:www.bayceer.uni-bayreuth.de-bayceer-t137486id
DTSTAMP:20260805T053934Z
DESCRIPTION:- Due to illness the talk had to be cancelled. It will probably
  take place in the winter semester -\n*****\nFog as a meteorological pheno
 menon in the atmospheric boundary layer can have a high impact on the econ
 omy but also on personal safety. The total economic loss that is associate
 d with fog events on aviation\, marine and land transportation are compara
 ble to those of winter storms. Despite improvements in numerical weather p
 rediction models over the last years\, fog forecasting is still highly ina
 ccurate. The main reason for this is the fog's considerable variability in
  space and time as a result of the nonlinear interaction between several p
 rocesses\, including radiative cooling/warming\, turbulent mixing\, cloud 
 microphysics\, and the atmosphere-surface-soil interaction - processes tha
 t are only partly resolved by state-of-the-art forecasting models.\nIn thi
 s presentation\, the typical life cycle of a radiation fog event is convey
 ed. The key processes relevant for radiation fog that forms in the nocturn
 al atmospheric stable boundary layer are outlined and their interaction is
  analyzed by using a comprehensive set of high-resolution turbulence-resol
 ving large-eddy simulations using the model PALM\, which has been develope
 d at the Institute of Meteorology and Climatology at Leibniz Universität H
 annover. Special focus will be given on the importance of the adequate rep
 resentation of all revelant processes in the modeling system and the inter
 action between atmosphere\, surface\, and underlying soil.\n \n*** Invited
  by Christoph Thomas\, Micrometeorology
DTSTART;TZID=Europe/Berlin:20170504T120000
DTEND;TZID=Europe/Berlin:20170504T133000
LOCATION:S 21\, GEO
SUMMARY:Dr. Bjoern Maronga\, Institute of Meteorology and Climatology\, Uni
 versität Hannover (Homepage):  Cancelled: Simulation of radiation fog in t
 he nocturnal atmospheric boundary layer using a turbulence-resolving model
TRANSP:TRANSPARENT
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