Property:CSDMS meeting abstract title
From CSDMS
This is a property of type Text.
A
Using Neighborhood-Algorithm Inversion to Test and Calibrate Landscape Evolution Models +
2
Using a hydraulic model to identify the formative discharge for gravel-bedded rivers that fill with ice +
Using a new fundamental equation of sediment creep to model coastal breaching and landsliding +
A
Using a three-dimensional coupled sediment – hydrodynamic model to explore feedbacks between erodibility and sediment trapping in a partially mixed estuary, York River, VA. +
2
Using coupled geo-economic models to explore the interplay between coastal protection, natural processes, and economic values along developed shorelines +
Using flume and field measurements to estimate bedrock susceptibility to erosion +
Using individual-based models and animal movement to evaluate habitat-use intensity in fragmented landscapes: a case study using an ecosystem engineer in central Brazil +
Using relict Pleistocene geomorphology to inform future permafrost change +
A
Using the Flood Early Warning System with Ocean Modeling Data +
2
Variability in Bed Shear Stresses and Sediment Fluxes on the Alaskan Beaufort Sea Shelf: A Numerical Modeling Study +
Variability in Winds During River Flood and Quiescent Periods in Baltimore, MD: Implications for Modeling Estuarine Residence Time +
Variability in regolith characteristics as a proxy to model the seasonal evolution of the Draix CZO badland catchments. +
Variability of residence time and estuarine-ocean fluxes in a chain of Arctic estuaries +
Variations of Regional Erosion Rates Since LGM Mapped Through Time and Space +
Very Fine Scale of Permafrost Distribution and Controlling Factors +
Visualizing Ship Motion in Tsunami Currents +
Wave and fluvial discharge interaction along a multichannel delta coastline: A numerical modelling analysis +
A
Wax Lake Delta, Louisiana: Factors Controlling Hydrodynamics and Morphological Changes during Hurricane Rita (2005) +
2
What can I do with the USGS Model Catalog? +
M
What controls the disequilibrium state of gravel-bed
rivers? A test of the channel response number ξ +
