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William Ryan Currier, Theodore Thorson, and Jessica D. Lundquist

significant uncertainty in spatially distributed precipitation estimates ( Gutmann et al. 2012 ; Livneh et al. 2014 ; Henn et al. 2016 ) due to a sparse network of gauges ( Lundquist et al. 2003 ) and observational uncertainty at the gauge itself ( Goodison et al. 1998 ; Rasmussen et al. 2012 ). WRF or PRISM are frequently used to force hydrologic models, which guide decisions regarding avalanche control, reservoir storage, and flood forecasting. Therefore, uncertainties in the estimation of

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Qian Cao, Thomas H. Painter, William Ryan Currier, Jessica D. Lundquist, and Dennis P. Lettenmaier

. 2017 ). COOP, ASOS, and SNOTEL stations have daily minima and maxima observations for temperature in addition to precipitation. SNOTEL temperature data were biased warm at cold temperatures, and the biases were corrected based on Currier et al. (2017) . In addition, we used hourly temperature data from 26 sites, which had HOBO U23 Pro v2 temperature/relative humidity sensors installed during the OLYMPEX period (see Fig. 2 ). Wind speed data, required as the VIC forcing, were obtained from the

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Robert Conrick and Clifford F. Mass

Mission . Bull. Amer. Meteor. Soc. , 95 , 701 – 722 , https://doi.org/10.1175/BAMS-D-13-00164.1 . 10.1175/BAMS-D-13-00164.1 Houze , R. A. , Jr. , and Coauthors , 2017 : The Olympic Mountains Experiment (OLYMPEX) . Bull. Amer. Meteor. Soc. , 98 , 2167 – 2188 , https://doi.org/10.1175/BAMS-D-16-0182.1 . 10.1175/BAMS-D-16-0182.1 Iacono , M. J. , J. S. Delamere , E. J. Mlawer , M. W. Shephard , S. A. Clough , and W. D. Collins , 2008 : Radiative forcing by long–lived greenhouse gases

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