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TZID:Europe/Berlin
TZUNTIL:20050327T010000Z
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TZNAME:CET
DTSTART:20021027T030000
TZOFFSETFROM:+0200
TZOFFSETTO:+0100
RDATE:20031026T030000
RDATE:20041031T030000
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DTSTART:20030330T020000
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RDATE:20040328T020000
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BEGIN:VEVENT
UID:www.bayceer.uni-bayreuth.de-bayceer-t53258id
DTSTAMP:20260817T070752Z
DESCRIPTION:Experimental data during last ten years show imbalances of the 
 energy budget  . Measurements of all components of the balance equation of
  heat\, averaged over half hour periods\, show that\, within the framework
  of the used measuring techniques\, the heat balance is not closed. The su
 m of fluxes of heat   which is going into the atmosphere is less than  . T
 he main cause of this systematic imbalance is not the experimental methodo
 logy but a conceptual deficiency. It is related to the fact that the energ
 y-mass exchange between the complex (horizontally inhomogeneous) land surf
 ace and the atmosphere is determined by applying theories that are based o
 n the hypothesis of stationary and horizontal homogeneity (SHH). \nUsing t
 he experimental results  it was detected that the underestimation of the t
 urbulent fluxes is related to the terrain inhomogeneity. To systematize th
 e correction for this effect a parameterization is suggested which empiric
 ally makes use of the involved inhomogenity scale in the environment of a 
 site. For parameterization of the energy imbalance the coefficient   is us
 ed. The average value   is in line with the data of FIFE\, KUREX TARTEX\, 
 SADE\, Cabouw and Anchor data. \nThe paper aims to serve as a contribution
  to the ongoing discussion on how to account for different types and scale
 s of land surface inhomogeneities inside cells of models such as global cl
 imate models\, as well as mesoscale models. \n\n
DTSTART;TZID=Europe/Berlin:20030626T161500
DTEND;TZID=Europe/Berlin:20030626T235959
LOCATION:H6
SUMMARY:Prof. Dr. G.N. Panin\, Institute of Water Problem\, Moscow: Interac
 tion between Atmosphere and Natural Land Surface: Analysis of Data\, Param
 etrization of Surface Fluxes and Applications for local Climate Models
TRANSP:TRANSPARENT
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