Property:Describe output parameters model

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Showing 20 pages using this property.

S

Sakura +

CSV file of final bathymetry and deposit thickness for each grain size contained in the flow +

H

Hydromad +

Calibration algorithms, fit statistics. +

S

SINUOUS +

Centerline and floodplain evolution through time, as well as hydraulic parameters as detailed in the model documentation +

A

AR2-sinuosity +

Channel centerlines and associated model parameters +

R

River Erosion Model +

Channel geometry; sediment export +

D

D'Alpaos model +

Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features +

T

TreeThrow +

Characteristics of tree growth (stand biomass, stem count, leaf area, diamter) and characteristics of sediment transport (sediment flux in m4/m/yr, # of tree falls) +

C

CarboCAT +

Chronostrat plots, maps, cross-sections, lithofacies thickness distributions +

G

GFlex +

Cofactor matrix (*.mtx sparse matrix file; ASCII) Flexural response map (ASCII) +

C

Compact +

Compacted sediment porosity +

M

Mocsy +

Compute all carbonate system variables +

S

SETTLE +

Constant terminal settling velocity at STP +

E

ENTRAINH +

Critical shear stress for entrainment of a noncohesive grain from a mixed size-density bed +

ENTRAIN +

Critical shear stress for entrainment of a noncohesive grain from a homogenous bed +

S

SUSP +

Cross-sectional average suspended load transport rates +

F

FLDTA +

Cross-sectional mean flow velocities, flow depths, bed shear stresses as a function of along-channel distance. +

1

1DBreachingTurbidityCurrent +

Current thickness, velocity, and D50 for active layer and in suspension. +

B

BOM +

Currents, salinity, temperature, ... all model variables. +

C

CAESAR Lisflood +

DEM, Flow patterns, Inundation, Grainsize and others +

D

DLBRM +

DLBRM output includes, for every cell in the watershed grid, surface runoff to surface storage, infiltration to USZ, ET, ETP, percolation from USZ to LSZ, interflow from LSZ to surface storage, deep percolation from LSZ to groundwater storage, groundwater flow from groundwater storage to surface storage, surface moisture storage, USZ, and LSZ moisture storages, groundwater storage, and lateral flows from storages to adjacent cells for the surface (channel outflow), USZ, LSZ, and groundwater (Changsheng He and Thomas E. Croley II, 2007). +