Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Justin K. Anderson"'
Publikováno v:
Hydrological Processes. 20:2443-2457
Studies of hyporheic exchange flows have identified physical features of channels that control exchange flow at the channel unit scale, namely slope breaks in the longitudinal profile of streams that generate subsurface head distributions. We recentl
Publikováno v:
Hydrological Processes. 19:2931-2949
There is a need to identify measurable characteristics of stream channel morphology that vary predictably throughout stream networks and that influence patterns of hyporheic exchange flow in mountain streams. In this paper we characterize stream long
Publikováno v:
Hydrological Processes. 19:2915-2929
This article has been retracted and replaced. See Retraction and Replacement Notice DOI: 10.1002/hyp.6350 Studies of hyporheic exchange flows have identified physical features of channels that control exchange flow at the channel unit scale, namely s
Publikováno v:
Advances in Water Resources. 26:925-937
The stream tracer technique has been widely used as a method of characterizing hyporheic exchange in stream-catchment studies, commonly incorporating the use of the numerical, transient storage model OTIS, which assumes an exponential residence time
Publikováno v:
Hydrological Processes; Oct2005, Vol. 19 Issue 15, p2931-2949, 0p
Publikováno v:
Hydrological Processes; Oct2005, Vol. 19 Issue 15, p2915-2929, 0p