@article {80491,
	title = {Effect of bedrock permeability on stream base flow mean transit time scaling relationships:  2.  Process study of storage and release},
	journal = {Water Resources Research},
	volume = {52},
	year = {2016},
	note = {This article is linked to an article by Hale and McDonnell in the same issue of Water Resources Research. These articles concern the hydrology of subterranean water flow in the Drift Creek catchments in the Alsea River Basin contrasted with catchments in the H.J. Andrews Experimental Forest.  The first article showed that water flow mean transit times were controlled by bedrock permeability. {\textquotedblleft}This paper presents a process-based investigation of storage and release in the more permeable catchments to explain the longer [mean transit times] and (catchment) area-dependent scaling.{\textquotedblright}  The authors postulate a discrete sub-alluvial storage zone to explain observed results.},
	pages = {p.1375-1397},
	keywords = {Alsea River Basin, Alsea Watershed Study, Drift Creek, Flynn Creek, H. J. Andrews Experimental Forest, geology, hydrology, mathematical modeling, Needle Branch, sediments, Tyee Formation,},
	doi = {doi:10.1002/2015WR017660},
	author = {Hale, V. Cody and McDonnell, Jeffrey J. and Stewart, Michael K. and Solomon, D. Kip and Doolitte, Jim and Ice, George G. and Pack, Robert T.}
}
