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TZID:Europe/Berlin
TZUNTIL:20231029T010000Z
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DTSTART:20211031T030000
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BEGIN:VEVENT
UID:www.bayceer.uni-bayreuth.de-bayceer-t155877id
DTSTAMP:20260812T171708Z
DESCRIPTION:Our understanding of the atmospheric boundary layer has improve
 d a lot with the recent advances in the state-of-the-art remote sensing in
 struments and also computational resources. The atmospheric boundary layer
  (ABL) is the lowest part of the atmosphere\, which is influenced by the p
 resence of earth&rsquo\;s surface and its interaction with the surface for
 cings. The turbulent exchange of momentum\, heat\, and moisture between th
 e earth surface and the atmosphere needs to be well understood for proper 
 simulation of the ABL processes in weather and climate models. In addition
  to observations\, large eddy simulation tools are used for the testing an
 d development of boundary layer turbulence parameterization schemes used i
 n the atmospheric numerical weather prediction (NWP) models. While the day
 time convective boundary layers are well represented in the NWP models\, n
 ight-time stable boundary layers are not\, due to the presence of the smal
 ler-sized eddies. Stable boundary layer (SBL)s are governed by processes s
 uch as intermittent turbulence\, gravity waves\, radiative cooling\, katab
 atic flows\, and fog formation. These processes have a direct impact on th
 e society for example\, fog modeling for road safety\, aviation\, frost fo
 r agricultural sector and also air quality modeling. We discuss the evolut
 ion of the SBL over a valley in the Fichtelgebirge mountains from observat
 ions and model simulations. Further we highlight current challenges and ad
 vancements in the SBL modeling over complex terrain using LES.\n&nbsp\;\n*
 **new BayCEER member
DTSTART;TZID=Europe/Berlin:20211118T121500
DTEND;TZID=Europe/Berlin:20211118T134500
LOCATION:hybrid
SUMMARY:Dr. Shravan Kumar Muppa\, Micrometeorology\, BayCEER\, UBT (Homepag
 e): Investigating local topographic effects on the stable boundary layer s
 tructure in mountainous terrain using large eddy simulations
TRANSP:TRANSPARENT
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