18th Symposium on Boundary Layers and Turbulence
    

Session 13B

 

BOUNDARY LAYERS AT HIGH LATITUDES—II

 Chair: Peter A. Taylor, York University, Toronto, ON Canada
10:30 AM13B.1The effect of leads in the sea-ice on the Antarctic boundary layer: a high-resolution study using a parallelized LES model  
Björn Witha, Leibniz University, Hannover, Germany; and S. Raasch
10:45 AM13B.2Arctic boundar-layer inversions from SHEBA observations and ERA-40 reanalysis data  
Michael Tjernström, University of Stockholm, Stockholm, Sweden; and R. G. Graversen
11:00 AM13B.3Cloud and inversion characteristics over the Arctic pack ice  
Joseph Sedlar, Stockholm University, Stockholm, Sweden; and M. Tjernström
11:15 AM13B.4Downward sensible heat flux and decoupling over snow-covered surfaces  
Timo Vihma, Finnish Meteorological Institute, Helsinki, Finland
11:30 AM13B.5Effect of surface heterogeneity on energy fluxes during the SHEBA winter  extended abstract
P. O. G. Persson, CIRES/Univ. of Colorado and NOAA/ESRL/PSD, Boulder, CO; and E. L. Andreas, C. W. Fairall, A. A. Grachev, P. S. Guest, and J. A. Maslanik
11:45 AM13B.6Effect of microphysical parameterization on the simulation of high-latitude surface energy budget and boundary-layer structure  
P. O. G. Persson, CIRES/Univ. of Colorado and NOAA/ESRL/PSD, Boulder, CO; and A. B. Solomon, M. Shupe, H. Morrison, and J. -. W. Bao
12:00 PM13B.7Characteristics of near-surface atmospheric flow and turbulent heat fluxes under highly stable conditions over a snow-covered alpine glacier  
Hendrik Huwald, Ecole Polytechnique Fédérale de Lausanne, Lausanne, Switzerland; and M. B. Parlange, C. Higgins, E. Bou-Zeid, M. Calaf-Bracons, and C. Meneveau
12:15 PM13B.8Surface-layer properties on the eastern Antarctic plateau and its adjacent slopes  
Mingyu Zhou, Polar Research Institute of China, Pudong, Shanghai, China; and S. Zhong, Z. Zhang, D. H. Lenschow, H. -. M. Hsu, W. -. Q. Yao, Z. Gao, S. Li, and B. Sun

Thursday, 12 June 2008: 10:30 AM-12:15 PM, Aula Magna Höger

* - Indicates paper has been withdrawn from meeting

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