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2022 CSDMS meeting-083 (section Modeling Tsunami Inundation and Sediment Transport to Characterize Earthquake Source Parameters from Tsunami Deposits)
hydrodynamic boundary conditions for the sediment transport simulations. The Delft3D-FLOW model uses van Rijn (2007) sediment transport formulations and coefficients

4 KB (426 words) - 19:47, 4 April 2022
2022 CSDMS meeting-033 (section Modeling Future Sediment Transport Variations at a Watershed-Scale Using Landlab: A Preliminary Example from the Chestatee River in Northern Georgia, USA.)
centuries will influence sediment delivery to reservoirs, locks, harbors, and coasts. The models will be calibrated by historical sediment flux data, allowing

4 KB (415 words) - 11:52, 14 April 2022
2019 CSDMS meeting-078
HydroTrend was used to estimate incoming sediment load from the Skeena River. Model estimates of suspended sediment load are higher than past estimates due

5 KB (378 words) - 11:24, 5 April 2019
2022 CSDMS meeting-016
model runs. We find that sediment cover strongly modulates landscape response to uplift, and model runs with “finer” sediment (lower particle settling

4 KB (436 words) - 16:02, 15 April 2022
2022 CSDMS meeting-058 (section Generating geochemical maps from river sediment samples: an inverse modelling approach)
composition of sediment contained within rivers or floodplains, which integrate large upstream areas [1]. Our method works by modelling sediment geochemistry

4 KB (417 words) - 07:29, 6 April 2022
Webinars
level rise: From decades to millennia 2021/12/02 Syvitski, Jaia Earth's Sediment Cycle during the Anthropocene 2021/11/30 Campforts, Benjamin Shuffling

2 KB (70 words) - 08:41, 24 January 2023
2022 CSDMS meeting-064 (section Insights from new model for river incision accounting for stochastic water and sediment discharge)
and width freely evolve to optimize sediment transport and bedrock incision in response to stochastic water and sediment discharge. We investigate the impact

3 KB (327 words) - 10:40, 25 February 2022
2023 CSDMS meeting-106 (section Identifying sediment transport pathways on a heavily managed and chronically eroding, mixed sediment beach)
of the movement of sediment within the nearshore zone on beaches such as Pevensey will improve our understanding of how mixed sediment beaches function and

5 KB (465 words) - 04:43, 30 March 2023
2022 CSDMS meeting-082 (section Riverbank stability and cross-stream sediment diffusion governed by turbulence)
stabilization of channels by the attainment of the equilibrium between sediment diffusion and gravity forces. However, the role of other potentially relevant

4 KB (389 words) - 16:56, 14 April 2022
2019 CSDMS meeting-071
shoreline erosion control often listed as a key service, but can also alter the sediment dynamics and waves within back-barrier bays. Here we incorporate seagrass

4 KB (357 words) - 11:55, 8 February 2019
2019 CSDMS meeting-002
fluvial sediment flux to the delta directly linked to changes in delta morphology? (2) What are the magnitudes and trends of riverine sediment fluxes that

4 KB (348 words) - 17:45, 31 March 2019
2022 CSDMS meeting-094 (section Mass Wasting Router: A watershed-scale sediment production and transport model)
filter sediment production signals into a time series of bedload transport. Here, we describe the Mass Wasting Router, a new watershed-scale sediment production

2 KB (195 words) - 10:40, 13 May 2022
2022 CSDMS meeting-002
differences in vertical incision rate and influences sediment characteristics such as clast lithology, coarse sediment generation rate, and grain size. In rivers

4 KB (438 words) - 11:30, 25 January 2022
2023 CSDMS meeting-007 (section Modeling the development of wide bedrock valleys as a function of collapsed bedrock block size, bed sediment, and discharge variability)
closer in size to bedload sediment and narrower in landscapes where collapsed material is much larger than bedload sediment. I also use the newly modified

3 KB (310 words) - 14:46, 26 January 2023
2022 CSDMS meeting-077
between runs. Further, 3 scenarios of fluvial sediment discharge corresponding to low, medium, and high sediment discharges, are incorporated into each fluvial

4 KB (371 words) - 08:57, 10 May 2022
2019 CSDMS meeting-067
greatest exhumation. Sediment transport modeling across the orogen suggests that areas of highest exhumation will be inundated with sediment over three orders

4 KB (355 words) - 12:55, 28 May 2019
2022 CSDMS meeting-080 (section The influence of geologically instantaneous, event-scale processes on basin-scale sediment dispersal patterns)
geologically instantaneous, event-scale processes may exert long-term control on sediment dispersal patterns and thus preserved stratigraphy at the basin scale,

4 KB (395 words) - 11:48, 22 March 2022
2023 CSDMS meeting-049 (section Topographic and surface mass balance controls on Greenland glacier dynamics in a coupled ice-sediment model)
sedimentation dynamics including sediment diffusion (removing sediment from moraines) and glaciofluvial sedimentation (adding sediment to moraines) in a flowline

4 KB (377 words) - 16:45, 27 February 2023
Landlab
and death of vegetation, surface water infiltration, linear diffusion of sediment), or drivers of these processes (e.g. rainfall, solar radiation). Users

4 KB (330 words) - 12:22, 9 November 2023
2022 CSDMS meeting-030 (section Inverting passive margin stratigraphy for marine sediment transport dynamics over geologic time)
SFM, which is based on an approximation of local, linear slope-dependent sediment transport, fails to produce diagnostic features of passive margin stratigraphy

5 KB (402 words) - 16:00, 1 February 2022

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