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Agustín Robles-Morua, Enrique R. Vivoni, and Alex S. Mayer

rainfall fields are based on a temporal disaggregation of gauge-only U.S.–Mexico daily analyses ( Higgins et al. 2000 ), adjusted to account for orography using the Parameter-elevation Regressions on Independent Slopes Model (PRISM; Daly et al. 1994 ). In Mexico, precipitation is temporally downscaled by deriving disaggregated weights from the 8-km Climate Prediction Center morphing technique (CMORPH) hourly data ( Joyce et al. 2004 ). The weather forcing fields of NLDAS were derived from analysis

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