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TZID:Europe/Berlin
TZUNTIL:20111030T010000Z
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TZNAME:CET
DTSTART:20091025T030000
TZOFFSETFROM:+0200
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RDATE:20101031T030000
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UID:www.bayceer.uni-bayreuth.de-bayceer-t72434id
DTSTAMP:20260828T072411Z
DESCRIPTION:ACHTUNG Vortrag fällt aus. Prof Ma kann aus China NICHT anreise
 n!  invited by Prof Foken As a unique geological and geographical unit\, t
 he Tibetan Plateau dramatically impacts the world’s environment and especi
 ally controls climatic and environmental changes in China\, Asia and even 
 in the Northern Hemisphere. Tibetan Plateau\, therefore\, provides a field
  laboratory for studying global change. With support from various agencies
  in the People’s Republic of China\, a Tibetan Observation and Research Pl
 atform (TORP) is now implementing. Firstly the background of the establish
 ment of the TORP\, the establishing and monitoring plan of long-term scale
  (5-10 years) of the TORP will be introduced. Then the preliminary observa
 tional analysis results\, such as the characteristics of land surface heat
  fluxes and CO2 flux partitioning\, the characteristics of atmospheric and
  soil variables\, the structure of the Atmospheric Boundary Layer (ABL) an
 d the turbulent characteristics will also be shown. The study on the regio
 nal distribution of land surface heat fluxes of paramount importance over 
 heterogeneous landscape of the Tibetan Plateau. Therefore\, here the param
 eterization methods based on satellite data (NOAA/AVHRR\, Landsat-7 ETM\, 
 ASTER and MODIS) and ABL observations have been proposed and tested for de
 riving surface reflectance\, surface temperature\, NDVI\, MSAVI\, vegetati
 on coverage\, LAI\, net radiation flux\, soil heat flux\, sensible heat fl
 ux and latent heat flux over heterogeneous landscape. As cases study\, the
  methods were applied to the experimental area of the CAMP/Tibet (CEOP (Co
 ordinated Enhanced Observing Period) Asia-Australia Monsoon Project (CAMP)
  on the Tibetan Plateau)\, which located at the central Tibetan Plateau an
 d the whole Tibetan Plateau area. Five scenes of Landsat-7 ETM data\, four
  scenes of NOAA/AVHRR data\, three scenes of ASTER data and four MODIS dat
 a were used in this study. To validate the proposed methods\, the ground-m
 easured values are compared to satellite derived values. The results show 
 that the derived surface variables and land surface heat fluxes over the s
 tudy area are in good accordance with the land surface status. It is there
 fore concluded that the proposed methods are successful for the retrieval 
 of land surface variables and land surface heat fluxes over heterogeneous 
 landscape of the Tibetan Plateau area. Further improvement of the methods 
 and its applying field will also be discussed.
DTSTART;TZID=Europe/Berlin:20091207T161500
DTEND;TZID=Europe/Berlin:20091207T174500
LOCATION:H8
SUMMARY:Prof. Yaoming Ma (Vortrag fällt aus!)\, Laboratory of Tibetan Envir
 onment Changes and Land Surface Processes\, Institute of Tibetan Plateau R
 esearch\, CAS\, Beijing: Talk canceled!
TRANSP:TRANSPARENT
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