@article {76296,
	title = {Hydrologic landscape classification evaluates streamflow vulnerability to climate change in Oregon, USA},
	journal = {Hydrology and Earth System Sciences},
	volume = {18},
	year = {2014},
	note = {In this paper, the authors examined three river basins in areas of Oregon with different rainfall/snowfall regimes.  They used a hydrologic landscape model to evaluate the effects of climate change on the basins.  The model used five factors:  climate, seasonality, aquifer permeability, terrain, and soil permeability. {\textquotedblleft}We evaluate changes when the 1971{\textendash}2000 HL climate indices are recalculated using 2041{\textendash}2070 simulation results from the ECHAM (European Centre HAMburg) and PCM (Parallel Climate Model) climate models with the A2, A1b, and B1 emission scenarios. . . At the basin scale, simulated changes for the Siletz Basin, in Oregon{\textquoteright}s Coast Range, include a small switch from very wet to wet climate, with no change in seasonality. However, there is a modest increase in fall and winter water due to increased precipitation.{\textquotedblright} (from the Abstract) Note:  this does not mean that fish and wildlife dependent upon the stream would be unaffected.},
	month = {2014},
	pages = {p.3367-3392},
	keywords = {climate change, hydrology, Middle Fork John Day River Basin, precipitation, Sandy River Basin, Siletz River Basin, statistical modeling},
	doi = {10.5194/hess-18-3367-2014},
	author = {Leibowitz, S. G, and Comeleo, R. L. and Wigington Jr., P. L. and Weaver, C. P. and Morefield, P. E. and E A Sproles E and Ebersole, J.L.}
}
