Wednesday Morning 1
Time	Session	Location	Title
0800	C31A	MW 3006	Cold Region Hydrology III: Surface and Subsurface Processes:Frozen Ground Presiding: A W Balser, Institute of Arctic Biology, University of Alaska, Fairbanks; O Frauenfeld, University of Colorado, Boulder    [Abstracts]
0800	C31A-01	MW 3006	Cold-Region Subsurface Hydro-thermal Sensitivity of Physical Land Scheme in Global Climate Model: Idealized Off-Line Evaluation *K Saito    [details]
0815	C31A-02	MW 3006	Permafrost in Iceland – Distribution, Ground Temperatures and Climate Change Impact *B Etzelmuller, H Farbrot, T V Schuler, A Gudmundsson    [details]
0830	C31A-03	MW 3006	Remote sensing of changes in near surface freeze and thaw timing from 1988 to 2006 *N V Smith-Downey, S S Saatchi, J T Randerson    [details]
0845	C31A-04	MW 3006	Frozen Quaternary Deposits of the Laptev Sea Region as a Reservoir of Organic Carbon: Total Content and Composition. *A Kholodov, L Schirrmeister, L Shirshova, B Zolotareva, H Meyer, C Knoblauch, K Fahl    [details]
0900	C31A-05	MW 3006	Exploring the Effectiveness of Alpine Permafrost Model Transfer Between Mountain Environments in Northwestern Canada *P P Bonnaventure, A G Lewkowicz    [details]
0915	C31A-06	MW 3006	Snow and Ground Temperature R N Harris, M G Davis, M G Bartlett, *D S Chapman    [details]
0930	C31A-07	MW 3006	An Increase in Rates of Retrogressive Thaw Slumping and Implications to Lake Water Quality, Western Arctic, Canada. *S V Kokelj, T C Lantz    [details]
0945	C31A-08	MW 3006	Why could Permafrost be sometimes so persistent? *V E Romanovsky    [details]