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Roland J. Viger, Lauren E. Hay, Steven L. Markstrom, John W. Jones, and Gary R. Buell

Vaccaro 2002 ), to move outflow from each HRU through the drainage network to control the travel time downstream. Derivation of the Muskingum routing parameters is described in Viger et al. ( Viger et al. 2010 ). 4.2. Model inputs PRMS requires daily inputs of precipitation and maximum and minimum air temperature for each HRU. The USGS Downsizer ( Ward-Garrison et al. 2009 ) was used to select, download, verify, and format the station-based time series data for direct input to PRMS. The Downsizer

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David M. Bjerklie, Thomas J. Trombley, and Roland J. Viger

incorporate this variability into the future climate datasets. The weather stations were selected to provide geographic coverage of the model domain, to represent varying elevations and environmental settings within the domain, and to have records of sufficient quality. We recognize the difficulty and inherent issues related to distributing input weather data. In this study, we assume that the distribution pattern of the gauge records is representative, even considering issues of undercatch or overcatch

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Lauren E. Hay, Steven L. Markstrom, and Christian Ward-Garrison

Rep. 83-4238, 207 pp . Le Treut , H. , R. Somerville , U. Cubasch , Y. Ding , C. Mauritzen , A. Mokssit , T. Peterson , and M. Prather , 2007 : Historical overview of climate change science . Climate Change 2007: The Physical Science Basis, S. Solomon et al., Eds., Cambridge University Press, 93–127 . Lettenmaier , D. P. , 1976 : Detection of trends in water quality data from records with dependent observations . Water Resour. Res. , 12 , 1037 – 1046 . Leung , L. R

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