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Gemma T. Narisma and Andrew J. Pitman

heat fluxes over snow to land-cover changes. J. Hydrometeorol. 4 : 24 – 42 . Texier , D. , N. de Noblet , S. P. Harrison , A. Haxeltine , D. Jolly , S. Joussaume , and F. Laarif . 1997 . Quantifying the role of biosphere–atmosphere feedbacks in climate change: Coupled model simulations for 6000 years BP and comparison with palaeodata for northern Eurasia and northern Africa. Clim. Dyn. 13 : 865 – 882 . Tremback , C. J. 1990 . Numerical simulation of a mesoscale

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Martin-Pierre Lavigne, Alain N. Rousseau, Richard Turcotte, Anne-Marie Laroche, Jean-Pierre Fortin, and Jean-Pierre Villeneuve

al., 2003 ; Fortin et al., 1995 ; Fortin et al., 2001a ; Fortin et al., 2001b ). HYDROTEL, a semidistributed physically based model, integrates six computational modules that are run in a cascade (i.e., in a decoupled manner): weather data interpolation, snow cover dynamic, potential evapotranspiration, soil moisture balance, surface runoff, and streamflow. Each module offers more than one computational algorithm based on the availability of data for the studied watershed. Some algorithms

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Christopher Potter, Pusheng Zhang, Steven Klooster, Vanessa Genovese, Shashi Shekhar, and Vipin Kumar

–98) interannual pattern and intrabasin differences in monthly river discharge rates? To what extent does water use associated with current land cover and land use along a river drainage system explain the contemporary intrabasin differences in monthly river discharge rates? 2. Review of previous regional studies of historical river discharge There have been several previous studies of the potential impacts of CIs on river discharge rates in the world’s large hydrologic drainage basins. Major results from

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