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Adriaan J. Teuling, Remko Uijlenhoet, Bart van den Hurk, and Sonia I. Seneviratne

land are significantly reduced (e.g., Douville 2003 ; Koster et al. 2004 ; Seneviratne et al. 2006a ). It is also known that there is a tight relation between soil moisture and screen-level temperature and humidity ( Mahfouf 1991 ). In addition, there is a two-way coupling between the memory of the land surface and the strength of the coupling between the land surface and the atmosphere ( Koster and Suarez 1996 , 2001 ). The correct simulation of land surface–atmosphere interactions requires

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