Complex channel responses to changes in stream flow and sediment supply on the lower Duchesne River, Utah

Development of sediment slug upstream from the Czorsztyn Reservoir (southern Poland) and its interaction with river morphology

“…However, observations of flood-induced changes from different gravel-bed rivers with an erodible bank (e.g., Hooke, 2003;Gaeuman et al, 2005;Dean and Schmidt, 2013) supports the potential occurrence of the hypothesized fluctuating tendency between phases 2 and 3 upstream from the CR in the future. The temporal variation in the effectiveness of bar-bank interaction may also depend on the future rate of floodplain sedimentation, which may increase the erosional resistance of the bank (e.g., Xu, 2001a), and the relative channel depth (Xu, 1990(Xu, , 2001b, the tendency observed in a finegrained, high-suspended load meandering and wandering braided river in China.…”

“…8B-11). The lack of changes in the channel depth (p = 0.190) may be explained by width changes to flood and in-channel sedimentation, typical for a gravel-bed river channel (Gaeuman et al, 2005). This suggested that the evolution of the gravel-bed channel with erodible banks in the backwater area may not be correctly predicted by models made based on the observation of fine-grained bed rivers, with high suspended load (Xu, 1990(Xu, , 2001a.…”

Hydrologic modeling of flood conveyance and impacts of historic overbank sedimentation on West Fork Black's Fork, Uinta Mountains, northeastern Utah, USA

“…Counts and Pederson (2003) assessed the geomorphic record of a large paleflood on the Green River; Pederson (2004) evaluated the record of drainage evolution in the Green River basin; and Larsen et al (2004) evaluated reworking of debris fan deposits in the Green River canyon downstream of Flaming Gorge Dam. Gaeuman et al (2003Gaeuman et al ( , 2005 studied the effects of historic changes in discharge and sediment transportation along a reach of the lower Duchesne River near its confluence with the Green River in the Uinta Basin. Additionally, several unpublished theses have been completed (Smelser, 1998;Stamp, 2000;Paepke, 2001;Gaeuman, 2003;Larsen, 2003).…”

Numerical modelling of climate change impacts on Saint‐Lawrence River tributaries

“…Moreover, river response depends on base level as well as hydrology (Blum and Törnqvist, 2000) and in some situations both of these are expected to change. Responses to base-level change can be complex and depend on the type and duration of change and type of river (Schumm, 1977;Begin et al, 1981;Simon and Hupp, 1986;Bonneau and Snow, 1992;Hassan and Klein, 2002;Gaeuman et al, 2005).…”