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- About Newsletters Join Member award Survey About Newsletters Join Member award Survey About Newsletters Join Member award Survey About Newsletters3 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 to2 KB (128 words) - 14:58, 19 October 2022
- channel-and-platform. Coastal Giulio Mariotti River Network Bed-Material Sediment Bed-material sediment transport and storage dynamics on river networks. Hydrology2 KB (6,836 words) - 17:21, 3 December 2021
- of concentrated sediment incorporated into ice near the base of the glacier. Despite the prevalence of these ice-sediment facies, sediment transported in3 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 transport3 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 clams4 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
- rivers to variable upstream sediment supply remains poorly understood, and operational flood models do not account for sediment in flood prediction. We introduce5 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 device3 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) modeling4 KB (382 words) - 14:45, 22 March 2019
- 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 the602 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). Preliminary4 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 of3 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 modified3 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 present2 KB (216 words) - 16:47, 14 April 2022
- Edit registration Pay registration (if you haven't already) Log in (or create account for non-CSDMS members) Forgot username? Search or email:CSDMSweb@colorado1 KB (44 words) - 15:51, 16 February 2022
- significant increases in suspended sediment flux in adjacent streams and that the effect of deforestation on suspended sediment flux will decrease significantly3 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 increase3 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 transport3 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 as3 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 coefficients4 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, allowing4 KB (415 words) - 11:52, 14 April 2022
- HydroTrend was used to estimate incoming sediment load from the Skeena River. Model estimates of suspended sediment load are higher than past estimates due5 KB (378 words) - 11:24, 5 April 2019
- model runs. We find that sediment cover strongly modulates landscape response to uplift, and model runs with “finer” sediment (lower particle settling4 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 geochemistry4 KB (417 words) - 07:29, 6 April 2022
- level rise: From decades to millennia 2021/12/02 Syvitski, Jaia Earth's Sediment Cycle during the Anthropocene 2021/11/30 Campforts, Benjamin Shuffling2 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 impact3 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 and5 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 relevant4 KB (389 words) - 16:56, 14 April 2022
- 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 seagrass4 KB (357 words) - 11:55, 8 February 2019
- fluvial sediment flux to the delta directly linked to changes in delta morphology? (2) What are the magnitudes and trends of riverine sediment fluxes that4 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 production2 KB (195 words) - 10:40, 13 May 2022
- differences in vertical incision rate and influences sediment characteristics such as clast lithology, coarse sediment generation rate, and grain size. In rivers4 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 modified3 KB (310 words) - 14:46, 26 January 2023
- between runs. Further, 3 scenarios of fluvial sediment discharge corresponding to low, medium, and high sediment discharges, are incorporated into each fluvial4 KB (371 words) - 08:57, 10 May 2022
- greatest exhumation. Sediment transport modeling across the orogen suggests that areas of highest exhumation will be inundated with sediment over three orders4 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 flowline4 KB (377 words) - 16:45, 27 February 2023
- and death of vegetation, surface water infiltration, linear diffusion of sediment), or drivers of these processes (e.g. rainfall, solar radiation). Users4 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 stratigraphy5 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 flow3 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 by3 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 phenomenon5 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. Here3 KB (330 words) - 16:29, 25 May 2023
- three-dimensional distributions of sediment deposits characteristic of fluvial, wave, and tidal dominated deltas. The generated sediment deposits are used to create4 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 numerical3 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 19294 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 soft4 KB (383 words) - 08:02, 1 April 2023
- further changes when computations include reduction in sediment settling velocity due to offshore sediment fining, based on field observations. These profile4 KB (360 words) - 10:38, 5 May 2022
- geometries in response to changing water and sediment inputs, base level and the transport of this sediment through the fluvial system. In this study, we3 KB (312 words) - 14:38, 30 March 2023