Times associated with source-to-sink propagation of environmental signals during landscape transience
Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …
The sha** of erosional landscapes by internal dynamics
Erosional landscapes transport sediment downstream, host natural hazards and are
geologically active. While perturbations in external forcing, particularly climate and tectonics …
geologically active. While perturbations in external forcing, particularly climate and tectonics …
[ספר][B] Rivers in the Landscape
E Wohl - 2020 - books.google.com
Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …
level do not lie within a drainage basin. Even points distant from the nearest channel are …
A new efficient method to solve the stream power law model taking into account sediment deposition
The stream power law model has been widely used to represent erosion by rivers but does
not take into account the role played by sediment in modulating erosion and deposition …
not take into account the role played by sediment in modulating erosion and deposition …
Geomorphometric delineation of floodplains and terraces from objectively defined topographic thresholds
Floodplain and terrace features can provide information about current and past fluvial
processes, including channel response to varying discharge and sediment flux, sediment …
processes, including channel response to varying discharge and sediment flux, sediment …
The dynamics of channel slope, width, and sediment in actively eroding bedrock river systems
The evolution of rivers in eroding landscapes plays a key role in determining landscape
relief and modulating climate‐tectonic interactions. A common approach to quantifying river …
relief and modulating climate‐tectonic interactions. A common approach to quantifying river …
Fluvial bevelling of topography controlled by lateral channel mobility and uplift rate
Valley morphologies of rivers crossing zones of active uplift range from narrow canyons to
broad alluvial surfaces. They provide illuminating examples of the fundamental, but poorly …
broad alluvial surfaces. They provide illuminating examples of the fundamental, but poorly …
How is time distributed in a river meander belt?
River meandering controls the age of floodplains through its characteristic paces of growth
and eventual cutoff of channel bends, forming oxbows. Hence, floodplain‐age distributions …
and eventual cutoff of channel bends, forming oxbows. Hence, floodplain‐age distributions …
[HTML][HTML] Alluvial channel response to environmental perturbations: fill-terrace formation and sediment-signal disruption
The sensitivity of fluvial systems to tectonic and climatic boundary conditions allows us to
use the geomorphic and stratigraphic records as quantitative archives of past climatic and …
use the geomorphic and stratigraphic records as quantitative archives of past climatic and …
Controls on the lateral channel‐migration rate of braided channel systems in coarse non‐cohesive sediment
Lateral movements of alluvial river channels control the extent and reworking rates of
alluvial fans, floodplains, deltas, and alluvial sections of bedrock rivers. These lateral …
alluvial fans, floodplains, deltas, and alluvial sections of bedrock rivers. These lateral …