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Terrestrial (section Modeling erosion, sediment and solute transport, and deposition on land)
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3 KB (229 words) - 16:22, 6 December 2022
Coastal (section Modeling erosion, sediment and solute transport in nearshore environments like deltas, estuaries, bays and lagoons)
About Join About Join About Join About Join Models The Coastal community makes available a diverse set of 89 numerical models and tools, for you to

2 KB (128 words) - 14:58, 19 October 2022
Model download portal
channel-and-platform. Coastal Giulio Mariotti River Network Bed-Material Sediment Bed-material sediment transport and storage dynamics on river networks. Hydrology

2 KB (6,836 words) - 17:21, 3 December 2021
2022 CSDMS meeting-024 (section Numerical modeling of subglacial sediment entrainment)
of concentrated sediment incorporated into ice near the base of the glacier. Despite the prevalence of these ice-sediment facies, sediment transported in

3 KB (252 words) - 14:13, 15 April 2022
2019 CSDMS meeting-082 (section Introducing a sediment module to the National Water Model (WRF-Hydro))
2 Dimensional SEDiment (CASC2D-SED) model and adapted it to the WRF-Hydro platform. The model mainly contains two components: (1) sediment erosion and transport

3 KB (262 words) - 21:16, 7 March 2019
2019 CSDMS meeting-091 (section The influence of bio-physical processes on sediment motion over tidal flat)
was obviously higher in the sediment layer below the surface seabed at aquaculture site. Further, we find that the sediments on the flat inhabited by clams

4 KB (425 words) - 01:48, 18 March 2019
2019 CSDMS meeting-083 (section Introducing a wave-supported gravity flow module to Community Sediment Transport Model System)
processes into the Community Sediment Model System (CSTMS) on the platform of the Coupled Ocean-Atmosphere-Wave-and-Sediment Transport Modeling system (COAWST)

4 KB (301 words) - 16:30, 7 March 2019
2019 CSDMS meeting-008
rivers to variable upstream sediment supply remains poorly understood, and operational flood models do not account for sediment in flood prediction. We introduce

5 KB (344 words) - 19:51, 1 April 2019
2019 CSDMS meeting-004 (section An investigation of the impact of Marine Hydrokinetic devices on sediment transport)
around a bed mounted MHK structure to analyze the impacts of seabed slope, sediment grain size, and wave condition on the long-term stability of the device

3 KB (321 words) - 12:18, 25 March 2019
2019 CSDMS meeting-092 (section Estimating the Impact of Oil on Flocculation Processes with a New Parameterized Sediment Model)
processes into the Community Sediment Transport Modeling System (CSTMS) within the Coupled Ocean-Atmosphere-Wave-and-Sediment Transport (COAWST) modeling

4 KB (382 words) - 14:45, 22 March 2019
Labs portal
get your lab on the CSDMS JupyterHub Sediment Supply to the Global Ocean Stand alone module Investigate river sediment supply to the ocean by exploring the

602 bytes (1,163 words) - 14:08, 26 August 2020
2019 CSDMS meeting-005 (section Sediment dynamics along the fluvial-tidal transition: a case study from the Ganges delta)
multiple flood ranges (low, medium and extreme) and sediment cases (-50%, average +50% suspended sediment concentration of 4 cohesive grain classes). Preliminary

4 KB (346 words) - 10:54, 28 May 2019
2019 CSDMS meeting-003 (section Response of Fluvial Suspended Sediment Fluxes and River Discharge to Future Climate Change on a Global Scale)
of Alabama Tuscaloosa Alabama, United States. sagy.cohen@ua.edu Fluvial sediment dynamics play an important role in the functioning and connectivity of

3 KB (297 words) - 17:47, 31 March 2019
2022 CSDMS meeting-025 (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 (312 words) - 15:03, 15 April 2022
2022 CSDMS meeting-004 (section Comparing sedimentological facies with modeled sediment transport pathways in fault scarp environments)
colluvial wedge development, connecting this knowledge to the physics of sediment transport can open new frontiers in our understanding. Here, I present

2 KB (216 words) - 16:47, 14 April 2022
2022 CSDMS meeting-041 (section Sediment Transport in Permafrost Landscapes)
Edit registration Pay registration (if you haven't already) Log in (or create account for non-CSDMS members) Forgot username? Search or email:CSDMSweb@colorado

1 KB (44 words) - 15:51, 16 February 2022
2022 CSDMS meeting-026 (section Sediment Response to Deforestation in the Amazon River Basin)
significant increases in suspended sediment flux in adjacent streams and that the effect of deforestation on suspended sediment flux will decrease significantly

3 KB (334 words) - 16:32, 18 February 2022
2019 CSDMS meeting-056 (section Seasonal variation in wave-driven sediment resuspension in the northern Andaman Sea: Results from a numerical model)
surface morphology and sediment texture in the east – to – west direction, and recent field observations indicate that sediment accumulation rates increase

3 KB (270 words) - 06:32, 1 April 2019
2022 CSDMS meeting-087 (section Implementation of a Hydrodynamic - Sediment Transport Model for the Beaufort Sea Shelf)
hydrodynamic and sediment transport conditions on the continental shelf, motivating this study. To analyze this, we are using a coupled hydrodynamic-sediment transport

3 KB (269 words) - 09:29, 1 April 2022
2019 CSDMS meeting-076 (section Constraining hydroclimate control on permafrost slope stability with sediment records, modern landscapes and coupled models)
timing and magnitude of slope instabilities in past glaciations. Using sediment records from these deposits, we show how hillslope denudation varies as

3 KB (240 words) - 10:29, 15 April 2019
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
2022 CSDMS meeting-035 (section Modeling the effects of detachment and entrainment of sediment in fault-crossing channels in strike-slip faults)
can be represented by the transport-limited theory, which assumes that sediment is always available but may or not be transportable depending on the flow

3 KB (310 words) - 12:32, 14 April 2022
2022 CSDMS meeting-106 (section Role of fluid-drag force and particle interactions on shape-induced segregation in sediment transport)
soil creep, landslides and debris flows, and river bed-load and suspended sediment transport. In the case of river bed-load transport, grains may move by

3 KB (355 words) - 14:26, 14 April 2022
2024 CSDMS meeting-057 (section How does abrasion impact the fluvial morphodynamics of a volcanic sediment pulse, Suiattle River, WA?)
the downstream impact of sediment supply from Glacier Peak, a stratovolcano that regularly supplies the channel with large sediment pulses. This phenomenon

5 KB (491 words) - 15:44, 27 March 2024
2023 CSDMS meeting-098 (section Simulated river channel response to a coarse sediment pulse with and without bed material abrasion)
and coarse sediment fluxes. We suggest that in some landscapes, abrasion may also be an important control on the morphodynamics of sediment pulses. Here

3 KB (330 words) - 16:29, 25 May 2023
2019 CSDMS meeting-029
three-dimensional distributions of sediment deposits characteristic of fluvial, wave, and tidal dominated deltas. The generated sediment deposits are used to create

4 KB (345 words) - 06:12, 28 May 2019
2023 CSDMS meeting-081 (section Variability in Bed Shear Stresses and Sediment Fluxes on the Alaskan Beaufort Sea Shelf: A Numerical Modeling Study)
hydrodynamic and sediment transport conditions on the continental shelf. To analyze this, we are using a coupled hydrodynamic - sediment transport numerical

3 KB (280 words) - 08:58, 17 March 2023
2024 CSDMS meeting-048 (section The Great Flood of 1927: Comparative Analysis of Historical and Current Sediment Trends)
in substantial change in the sediment load of the Mississippi River. In this study, we compiled historical water and sediment data from ~ 1851 through 1929

4 KB (260 words) - 10:17, 25 March 2024
2023 CSDMS meeting-111 (section Testing the Influence of Sediment Cover on Channel Steepness and Erosion Rates in Layered Rocks with the SPACE Model)
and lower than predicted in hard rocks. Sediment cover also exerts a strong control on erosion rates. Sediment cover preferentially accumulates over soft

4 KB (383 words) - 08:02, 1 April 2023
2022 CSDMS meeting-031
further changes when computations include reduction in sediment settling velocity due to offshore sediment fining, based on field observations. These profile

4 KB (360 words) - 10:38, 5 May 2022
2023 CSDMS meeting-109
geometries in response to changing water and sediment inputs, base level and the transport of this sediment through the fluvial system. In this study, we

3 KB (312 words) - 14:38, 30 March 2023
2024 CSDMS meeting-070 (section Icy Landscapes: modeling sediment transport in permafrost regions)
cold river water starts running, slowing the sediment bed from thawing. This would imply a decoupling of sediment transport from water discharge, at least

3 KB (414 words) - 11:24, 1 April 2024
2019 CSDMS meeting-052
fluvial and marine sediment transport via differential equations. The modular code includes components to deal with sea level changes, sediment compaction, local

3 KB (159 words) - 17:32, 27 May 2019
2023 CSDMS meeting-043 (section A coupled benthic-pelagic biogeochemical model for estimating sediment-water exchange of particulates and solutes: sensitivity tests and application to the northern Gulf of Mexico)
Boulder Boulder Colorado, United States. Julia.Moriarty@colorado.edu The sediment bed and the water column are tightly coupled in shallow water systems including

5 KB (412 words) - 13:36, 8 March 2023
2023 CSDMS meeting-096 (section Representing fluxes within upper Galveston Bay using ROMS (Regional Ocean Modeling System): Initial efforts toward a coupled hydrological / oceanic / sediment transport model)
flooding mobilized thick layers of sediment, including contaminated sediment from the Buffalo Bayou shipping channel. Sediment core data taken after the storm

5 KB (467 words) - 08:30, 28 March 2023
2022 CSDMS meeting-027 (section Spatial Trends and Drivers of Bedload and Suspended Sediment Fluxes in Global Rivers)
can very well predict the distribution of water discharge and suspended sediment and well predict bedload. Bedload predictions’ sensitivity to river slope

4 KB (280 words) - 13:01, 31 January 2022
PyMT
algorithm for storage-cell inundation modeling. Adams, Jordan Plume Hypopycnal sediment plume Hutton, Eric RAFEM A.k.a. RAFEM River Avulsion and Floodplain Evolution

2 KB (193 words) - 10:01, 16 February 2023
2022 CSDMS meeting-100
Stream discharge is often used to drive sediment transport models across channel networks. Because sediment transport is nonlinear, discharge arising

3 KB (312 words) - 16:10, 13 April 2022
2023 CSDMS meeting-102 (section The Impact of Streambed Mobilization on Fine Sediment and Organic Carbon Hysteresis in Mountain Rivers)
concentrations, which can result in distinct hysteresis patterns of suspended sediment (SS), particulate organic carbon (POC), and dissolved organic carbon (DOC)

6 KB (456 words) - 13:15, 2 April 2023
2024 CSDMS meeting-052 (section Complex Patterns of Sediment Erosion and Deposition under Sea-Level Variations Change: Insights from a Coupled Stratigraphic Experiment and Moving Boundary Modelling Approach for Fluvio-Deltaic Evolution.)
an experimental run with oscillating sea level conditions and constant sediment supply. We found that the dynamics of the fluvial surface play an important

5 KB (378 words) - 09:05, 1 April 2024
2024 CSDMS meeting-093 (section Emergent dynamics of soil production and sediment transport revealed using Agent-Based Models of biological agents)
opportunity is in the simulation of biologically driven soil production and sediment transport. Biological systems exhibit some of the most compelling examples

5 KB (450 words) - 17:08, 1 April 2024
2022 CSDMS meeting-072
Atmosphere Wave Sediment Transport modeling system (COAWST), which includes ocean (ROMS), atmosphere (WRF), surface-wave (SWAN, WAVEWATCHIII), sediment (CSTMS)

6 KB (440 words) - 16:34, 18 April 2022
Cross Shore Sediment Flux-Publications
References Cross Shore Sediment Flux Add references Citations View all Publications per year View all

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River Network Bed-Material Sediment-Publications
References River Network Bed-Material Sediment Add references Citations View all Publications per year View all

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2019 CSDMS meeting-101
spatially, distributed erosion models are validated to discharge and sediment yield at catchment outlets. Spatial information on erosion and deposition rates

3 KB (254 words) - 14:04, 28 May 2019
Presenters-0580
network-scale sediment (dis)connectivity and its response to anthropic pressures provides a foundation understanding of river processes and sediment dynamics

3 KB (318 words) - 09:52, 22 May 2022
Syvitski Student Modeler Award 2022
empirical sediment transport formulas to quantify spatiotemporal sediment (dis)connectivity in river networks. The D-CASCADE framework describes sediment connectivity

1 KB (183 words) - 10:53, 5 May 2022
2019 CSDMS meeting-104
naturally occurring arsenic. The arsenic likely derives from the pyrite-rich sediment of the Ganges basin, however, the cause and timing of mobilization of the

4 KB (302 words) - 15:23, 28 May 2019
2019 CSDMS meeting-050
change dramatically, where the time dimension is extremely important, where sediment fluxes are very large, where flotsam is trapped, and where numerical/physical

3 KB (329 words) - 17:59, 4 April 2019
2019 CSDMS meeting-094
conditions for adjoining hillslopes and respond to delivery of hillslope-derived sediment. But what happens when canyon walls deliver boulders that are too large

3 KB (314 words) - 13:37, 21 March 2019
2021 CSDMS meeting-028
times, we see those sediment deposits shift in size and location, we infer that there may also be physical abrasion from sediment impacts on the scalloped

3 KB (308 words) - 15:00, 20 June 2023
2018 CSDMS meeting-123
a depth-averaged hydrodynamic model to assess the impact of transported sediment deposition, erosion and trapping and binding in mound development. Numerical

3 KB (287 words) - 11:49, 2 April 2018
CSDMS 2010 meeting
Nicola Kettner, Albert Hicks, Murray Vandergoes, Marcus Modelling suspended sediment loads: Insight into the past and future of the Waipaoa catchment, North

11 KB (405 words) - 08:02, 20 August 2018
Presenters-0566
Mountain Basin Sediment Transfer Georgie Bennett University of Exeter, United Kingdom Bennett@exeter.ac.uk G.L. Bennett@exeter.ac.uk Abstract Sediment production

4 KB (550 words) - 09:49, 22 May 2022
Lab-0026 (section Linking Landlab Components and Creating Sediment Pulses in NetworkSedimentTransporter)
the NetworkSedimentTransporter with pulses of sediment to understand the impact of landscape disturbance on sediment yield: We evaluate sediment delivery

5 KB (535 words) - 13:27, 14 July 2022
2023 CSDMS meeting-033 (section The Impact of Tropical Cyclones on Streamflow and Sediment Dynamics in Large United States Rivers)
events are known to cause increased suspended sediment flux and discharge in nearby rivers, thus altering sediment dynamics in short time periods. This relationship

3 KB (246 words) - 13:24, 14 February 2023
Presenters-0451
(combination of cohesive and non-cohesive) sediment; and biodiffusive mixing of bed sediment. Additionally, changes to the sediment bed layering scheme were made that

4 KB (365 words) - 15:07, 20 June 2023
2019 CSDMS meeting-105
Tidal inlets are crucial land-forms that control the exchange of water and sediment between the open sea and the back-barrier basin. Despite the well accepted

3 KB (378 words) - 19:35, 31 March 2019
2023 CSDMS meeting-073
mangroves enhances estuary-scale sediment trapping due to altered sedimentation patterns. Only reductions in upstream sediment supply can limit estuarine muddification

4 KB (282 words) - 12:24, 12 May 2023
2024 CSDMS meeting-058 (section Using a new fundamental equation of sediment creep to model coastal breaching and landsliding)
Paris , France. Sediment creep is ubiquitous and precedes failure (e.g. landslides) in most landscapes. Accurate modeling of sediment creep is therefore

6 KB (630 words) - 09:03, 26 February 2024
2024 CSDMS meeting-101 (section Coupled Hydrodynamic-Sediment Transport Model in Galveston Bay during Hurricane Harvey)
bottom sediment input parameters are derived from the Texas Sediment Geodatabase (TxSed), which includes a comprehensive inventory of sediment properties

5 KB (395 words) - 20:35, 31 March 2024
2022 CSDMS meeting-022
flux through a fluvial system, and this is often under the assumption that sediment grain-size distribution on the bed remains static over time. However, recent

3 KB (307 words) - 09:08, 13 May 2022
AeoLiS-Publications
process-based model for aeolian sediment transport and spatiotemporal varying sediment availability: AN AEOLIAN SEDIMENT AVAILABILITY MODEL. Journal of

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Lab-0005 (section Sediment Supply to the Global Ocean)
io/help-desk. Download associated file: SedimentSupplyModeling02_2013.ppt Learn more about HydroTrend and its approach to sediment supply modeling from this presentation

5 KB (628 words) - 14:12, 14 April 2022
2024 CSDMS meeting-092
of model validation against runoff and sediment data from a field site and a sensitivity analysis on how sediment flux and landform development respond

3 KB (368 words) - 19:57, 31 March 2024
2024 CSDMS meeting-068
watershed of over 3.2 million square kilometers. The continental flux of water, sediment, and nutrients passes through the state of Louisiana in the last stretch

4 KB (346 words) - 02:28, 17 March 2024
WBMsed-Publications
Geography, and Humans Battle for Dominance over the Delivery of Fluvial Sediment to the Coastal Ocean. The Journal of Geology, 115, 1–19. 10.1086/509246

44 bytes (45 words) - 14:04, 20 December 2019
Presenters-0529
findings hint at the importance of abrasion and sediment heterogeneity in the morphodynamics of sediment pulse transport in river networks. A new modeling

4 KB (464 words) - 15:07, 20 June 2023
2023 CSDMS meeting-067 (section Quantifying Oxygen Exposure Time Due to Sediment Resuspension)
Edit registration Pay registration (if you haven't already) Log in (or create account for non-CSDMS members) Forgot username? Search or email:CSDMSweb@colorado

1 KB (44 words) - 09:34, 14 March 2023
Lab-0006 (section Future Sediment Flux of the Ganges River)
tremendous amounts of sediment (sand, silt and clay) from its steep Himalayan hinterland. We ask: how does this amount of sediment change with a changing

6 KB (732 words) - 14:19, 14 April 2022
Model:Delft3D
salinity, temperature and sediment, free surface flow, wave-current interaction, wind forcing, precipitation and evaporation, sediment sorting, fluid mud, morphological

5 KB (3 words) - 20:15, 16 September 2020
2022 CSDMS meeting-047
different processes could be compared, as has recently been done using a sediment flux budget approach. To explore this question, we analyze Landsat-derived

5 KB (358 words) - 23:25, 17 April 2022
2022 CSDMS meeting-054
lacustrine and marine basins bear archives of corresponding changes in sediment accumulation. Yet given the scale that the global climate exerts on geomorphological

3 KB (365 words) - 08:47, 11 May 2022
HydroTrend-Publications
climate-driven hydrological transport model that simulates discharge and sediment load leaving a river system. Computers & Geosciences, 34, 1170–1183

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2024 CSDMS meeting-114 (section Modeling the effects of bed-sediment entrainment on the dynamics and runout of outburst floods and emergent debris flows with the granular-fluid model D-Claw.)
floods and debris flows often incorporate large volumes of erodible bed sediment along their runout path. Although this phenomenon is widely recognized

3 KB (300 words) - 09:50, 3 April 2024
Lab-0024
to learn how these apply to numerical modeling, landscape evolution, and sediment flux. Although no Python skills are required to run the notebook, those

4 KB (458 words) - 13:24, 14 July 2022
2024 CSDMS meeting-053
salinization hazards associated with sea-level rise, storm surges, dwindling sediment supplies, and land subsidence. One of the greatest hurdles to hazard prediction

4 KB (310 words) - 10:53, 25 March 2024
2023 CSDMS meeting-034
boat-wake generated waves on lakebed sediment? Are large wakeboarding waves (up to 0.5 m in height) driving significant sediment resuspension or transport? Using

3 KB (263 words) - 12:56, 23 March 2023
SedCas-Publications
P.; McArdell, B. W.; Burlando, P.; 2014. A probabilistic sediment cascade model of sediment transfer in the Illgraben. Water Resources Research, 50, 1225–1244

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2023 CSDMS meeting-038
which brings about the delivery of terrestrial sediment, and waves, which redistribute the input sediment across the coastline. Given that there are many

3 KB (274 words) - 16:21, 25 May 2023
2024 CSDMS meeting-081
preserved environmental signals to erosional and transport processes within the sediment generation portion of landscapes is vital in constraining uncertainties

3 KB (298 words) - 09:57, 27 March 2024

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