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    Feedback between the Land Surface and Rainfall at Convective Length Scales 

    Source: Journal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 004:;page 625
    Author(s): Clark, Douglas B.; Taylor, Christopher M.; Thorpe, Alan J.
    Publisher: American Meteorological Society
    Abstract: The surface fluxes of heat and moisture in semiarid regions are sensitive to spatial variability of soil moisture caused by convective rainfall. Under conditions typical of the Sahel, this variability may persist for several ...
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    Evaluating the Simulated Seasonality of Soil Moisture with Earth Observation Data 

    Source: Journal of Hydrometeorology:;2009:;Volume( 010 ):;issue: 006:;page 1548
    Author(s): Ellis, Richard J.; Taylor, Christopher M.; Weedon, Graham P.; Gedney, Nicola; Clark, Douglas B.; Los, Sietse
    Publisher: American Meteorological Society
    Abstract: A critical function of a land surface scheme, used in climate and weather prediction models, is to partition the energy from insolation into sensible and latent heat fluxes. Many use a soil moisture function to control the ...
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    Modeling the Impact of Land Surface Degradation on the Climate of Tropical North Africa 

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 008:;page 1809
    Author(s): Clark, Douglas B.; Xue, Yongkang; Harding, Richard J.; Valdes, Paul J.
    Publisher: American Meteorological Society
    Abstract: Degradation of the land surface has been suggested as a cause of persistent drought in tropical north Africa. A general circulation model is used to assess the impact of degradation of five regions within tropical north ...
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    How Well Do Large-Scale Models Reproduce Regional Hydrological Extremes in Europe? 

    Source: Journal of Hydrometeorology:;2011:;Volume( 012 ):;issue: 006:;page 1181
    Author(s): Prudhomme, Christel; Parry, Simon; Hannaford, Jamie; Clark, Douglas B.; Hagemann, Stefan; Voss, Frank
    Publisher: American Meteorological Society
    Abstract: his paper presents a new methodology for assessing the ability of gridded hydrological models to reproduce large-scale hydrological high and low flow events (as a proxy for hydrological extremes) as described by catalogues ...
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    Comparing Large-Scale Hydrological Model Simulations to Observed Runoff Percentiles in Europe 

    Source: Journal of Hydrometeorology:;2011:;Volume( 013 ):;issue: 002:;page 604
    Author(s): Gudmundsson, Lukas; Tallaksen, Lena M.; Stahl, Kerstin; Clark, Douglas B.; Dumont, Egon; Hagemann, Stefan; Bertrand, Nathalie; Gerten, Dieter; Heinke, Jens; Hanasaki, Naota; Voss, Frank; Koirala, Sujan
    Publisher: American Meteorological Society
    Abstract: arge-scale hydrological models describing the terrestrial water balance at continental and global scales are increasingly being used in earth system modeling and climate impact assessments. However, because of incomplete ...
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    Multimodel Estimate of the Global Terrestrial Water Balance: Setup and First Results 

    Source: Journal of Hydrometeorology:;2011:;Volume( 012 ):;issue: 005:;page 869
    Author(s): Haddeland, Ingjerd; Clark, Douglas B.; Franssen, Wietse; Ludwig, Fulco; Voß, Frank; Arnell, Nigel W.; Bertrand, Nathalie; Best, Martin; Folwell, Sonja; Gerten, Dieter; Gomes, Sandra; Gosling, Simon N.; Hagemann, Stefan; Hanasaki, Naota; Harding, Richard; Heinke, Jens; Kabat, Pavel; Koirala, Sujan; Oki, Taikan; Polcher, Jan; Stacke, Tobias; Viterbo, Pedro; Weedon, Graham P.; Yeh, Pat
    Publisher: American Meteorological Society
    Abstract: ix land surface models and five global hydrological models participate in a model intercomparison project [Water Model Intercomparison Project (WaterMIP)], which for the first time compares simulation results of these ...
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