Property:Describe processes
From CSDMS
This is a property of type Text.
S
H
DEM resampling;
Depression filling;
Flow direction;
Flow accumulation; +
G
Discretizes a watershed into sub-catchments (for surface water) and a MODFLOW grid (for groundwater), and then uses these fundamental units to build input files for and execute GSFLOW and visualize it. +
L
Disturbance-driven soil creep (or other processes that can be represented by 2D diffusion). +
D
Erosion, transport and deposition of sediments (terrestrial -> deep-marine). Carbonate production. Complex tectonics (growth faults, salt deformation). +
W
Evolution of wind wave spectra under influence of wind, breaking, nonlinear interactions, bottom interaction (including shoalng and refraction), currents, water level changes and ice concentrsations. No diffraction. +
B
Explores ecogeomorphic couplings between adjacent and non-adjacent components of the entire coastal barrier system, from the ocean shoreface to the mainland forest. Processes include: Dune growth and storm erosion; storm overwash; shoreline change (ocean and back-barrier); dynamic shoreface response to sea-level rise, overwash, and dune growth; horizontal and vertical marsh dynamics; bay depth changes with wind waves; marsh migration into coastal forests; sediment exchange between barrier-marsh-bay-forest ecosystems; and carbon processes associated with ecogeomorphic changes. +
A
Extract c and alpha from:
Slope=cArea^alpha
For more details:
Cohen, S., G. Willgoose, and G. Hancock (2008), A methodology for calculating the spatial distribution of the area-slope equation and the hypsometric integral within a catchment, J. Geophys. Res., 113, F03027, doi:10.1029/2007JF000820. +
T
B
A
Fluvial erosion and depositions, lateral deposition across the floodplain, plume deposition in marine domain. +
C
Fluvial erosion, deposition and sedimentation, hillslope (diffusion) processes, flexure, orography +
E
Fluvial sediment entrainment and deposition +
S
Fluvial sediment erosion and deposition, fluvial bedrock erosion, the bedrock cover effect. +
P
Flux routing and sediment transport for the formation of river deltas. Resolves channel bifurcations, avulsion and migration. Can simulate subsidence (default basin-like shape, modify the Python code to customize). Can store stratigraphy (as sand fraction and thickness). +
C
For forward time integration, the simplest possible scheme, first-order forward Euler, is employed. +
B
Free surface flow of water. Conservation of heat, salinity, mass, turbulent kinetic energy, dissipation. +
S
Free surface, generalized s coordinate model. Classical representation of oceanic processes (tides, wind circulation, density driven circulation ...). Coupling with sediment transport and biogeochemistry +
G
Free-surface flow including wave action
Clastic erosion, transport, deposition
Compaction (load-based, vertical porous flow, full 3D porous flow)
Rudimentary carbonate growth +
GENESIS was designed to describe long-term trends of the beach plan shape in the course of its approach to an equilibrium form. The shoreline change model best calculates shoreline movement in transition from one equilibrium state to another. This change is usually caused by a notable pertubation, for example, jetty construction at a harbor or inlet, or placement of beach nourishment material. +
