Executive summary of the completed WATCH project

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[29]  T. Huntington.  CO2‐induced suppression of transpiration cannot explain increasing runoff , 2008 .

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[31]  W. Lucht,et al.  Causes of change in 20th century global river discharge , 2008 .

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[34]  SPACE-TIME CHARACTERISTICS OF LARGE-SCALE DROUGHTS IN EUROPE DERIVED FROM STREAMFLOW OBSERVATIONS AND WATCH MULTI-MODEL SIMULATIONS , 2011 .

[35]  T. Holmes,et al.  Global land-surface evaporation estimated from satellite-based observations , 2010 .

[36]  Simon Parry,et al.  Examining the large‐scale spatial coherence of European drought using regional indicators of precipitation and streamflow deficit , 2011 .

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[38]  I. Haddeland,et al.  Climate Change Effects on Spatiotemporal Patterns of Hydroclimatological Summer Droughts in Norway , 2011 .

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[40]  Fahad Saeed,et al.  Impact of irrigation on the South Asian summer monsoon , 2009 .

[41]  Developing a feedbacks toolkit for regional water resource assessments , 2011 .

[42]  P. Stott,et al.  Anthropogenic greenhouse gas contribution to flood risk in England and Wales in autumn 2000 , 2011, Nature.

[43]  Christopher Moseley,et al.  Climate model bias correction and the role of timescales , 2010 .

[44]  Joseph Alcamo,et al.  Critical regions: A model-based estimation of world water resources sensitive to global changes , 2002, Aquatic Sciences.

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[46]  J. Haerter,et al.  Unexpected rise in extreme precipitation caused by a shift in rain type? , 2009, Nature Geoscience.

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[48]  L. Tallaksen,et al.  Propagation of drought through the hydrological cycle , 2011 .

[49]  S. Seneviratne,et al.  Recent decline in the global land evapotranspiration trend due to limited moisture supply , 2010, Nature.

[50]  J. Carrera,et al.  Irrigation enhances precipitation at the mountains downwind , 2010 .

[51]  Diego G. Miralles,et al.  Magnitude and variability of land evaporation and its components at the global scale , 2011 .