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Daniel J. McEvoy, Justin L. Huntington, John T. Abatzoglou, and Laura M. Edwards

. 2011b ). The time scale with the highest correlations will depend on the type and characteristics of the water body (i.e., lake or stream) and the surrounding watershed (i.e., managed/unmanaged, drainage area, etc.). To evaluate the correlations between SPI and SPEI and hydrologic states and fluxes, several streams, lakes, and reservoirs throughout the study area were chosen for analysis. Hydrologic data of water stage and streamflow were obtained from the U.S. Geologic Survey (USGS), and site

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Kingtse C. Mo, Lindsey N. Long, and Jae-Kyung E. Schemm

, 19 569 – 19 585 . Liang , X. , D. P. Lettenmaier , E. F. Wood , and S. J. Burges , 1994 : A simple hydrologically based model of land surface water and energy fluxes for GCMs . J. Geophys. Res. , 99 , 14 415 – 14 428 . Liang , X. , D. P. Lettenmaier , and E. F. Wood , 1996 : One-dimensional statistical dynamic representation of subgrid spatial variability of precipitation in the two-layer Variable Infiltration Capacity model . J. Geophys. Res. , 101 , 21 403

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