Test6

From CSDMS
   
1D Hillslope MCMCMonte Carlo chain of 1D non-linear diffusion hillslope model to find most likely boundary conditionscarlo
monte
non-linear
conditions
non-linear diffusion rule
diffusion rule
back pressure ridge
model evolves
non-linear diffusion
markov chain monte
chain monte carlo
dragon back pressure
monte carlo inversion
roering
carrizo plain
boundary conditions idealised
varying boundary conditions
pressure ridge
hilley and arrowsmith
landscape evolution
hillslope model
1d hillslope mcmc
1D Particle-Based Hillslope Evolution Model1D probabilistic, particle-based model of hillslope evolution for studying hillslope equilibration and response to perturbations.probabilistic
particle-based
perturbations
hillslope
continuum description
module implements
implements a particle-based
hillslope evolution
particle-based model
equilibrium hillslope shape
produce equilibrium profiles
model
equilibrium hillslope
hillslope shape
evolution
description
introduced
shape and dynamics
hillslope model
landscape evolution
1d particle-based hillslope evolution model
1DBreachingTurbidityCurrent1D Breaching Turbidity current model for generating continuous turbidity currentsbreaching
turbidity
model
generating
turbidity current directed
turbidity current
steep subaqueous slope
breach-generated turbidity current
vertical turbidity current
retrogressive failure
sustained turbidity currents
steep subaqueous
quasi-horizontal turbidity current
current directed
current
breach-generated turbidity
monterey submarine canyon
subaqueous slope
1dbreachingturbiditycurrent
2DFLOWVELTidal & wind-driven coastal circulation routinetidal
wind-driven
routine
unsteady nonlinear tidal
wind-driven coastal circulation
unsteady nonlinear
nonlinear tidal
wind-driven coastal
coastal circulation
unsteady
circulation
flow dynamics
2dflowvel
ACADIAA finite element formulation of the non-conservative form of the vertically integrated advection/diffusion/reaction (ADR) equationadr
diffusion
reaction
equation
quoddy simulations
depth-averaged transport variables
conjunction with quoddy
tracks any number
depth-averaged transport
transport variables
quoddy
simulations
acadia
ADCIRCCoastal Circulation and Storm Surge Modelmodel
circulation
storm
surge
solving time dependent
free surface circulation
time dependent
free surface
system of computer
solving time
computer programs
typical adcirc applications
surface circulation
transport problems
larval transport studies
finite element method
typical adcirc
programs for solving
adcirc
flow dynamics
ADI-2DRead note in extended description. Advection Diffusion Implicit (ADI) method for solving 2D diffusion equationadi
read
description
code is inactive
module code
inactive
sediment transport
diffusion
adi-2d
ALFRESCOAlaskan Frame‐based Ecosystem Codecode
frame‐based
ecosystem
alaskan
rupp
simulate the response
response of subarctic
disturbance regime
fire regime
future fire regime
species composition
changing climate
regime
alfresco
alfresco was originally
vegetation
originally developed
developed to simulate
subarctic vegetation
treeline extention
Acronym1E-book: program for computing bedload transport in gravel rivers.e-book
program
rivers
sediment specific gravity
bed shear velocity
program computes gravel
computes gravel bedload
surface size distribution
effective bed shear
bed surface size
size distribution
specific gravity
shear velocity
based on skin
program computes
computes gravel
gravel bedload
sediment specific
bedload transport
fluvial morphodynamics
acronym1
Acronym1DE-book: program for computing bedload transport in gravel rivers over time.e-book
program
time
grain size distribution
surface grain size
flow duration curve
bedload grain size
volume bedload transport
bedload transport rate
grain size
size distribution
sand removed
flow duration
duration curve
computes the volume
transport rate
rate per unit
unit width
fluvial morphodynamics
bedload transport
acronym1d
Acronym1RE-book: program for computing bedload transport in gravel rivers with a Manning-Strickler relation for flow resistance.e-book
program
resistance
computing
grain size distribution
surface grain size
bedload grain size
volume bedload transport
bedload transport rate
grain size
size distribution
computes the volume
sand removed
transport rate
rate per unit
unit width
surface grain
volume bedload
bedload transport
fluvial morphodynamics
acronym1r
AeoLiSAeoLiS is a process-based model for simulating aeolian sediment transport in situations where supply-limiting factors are important, like in coastal environments.aeolis
important
environments
process-based
simulating aeolian sediment
aeolian sediment transport
factors are important
coastal environments
process-based model
model for simulating
simulating aeolian
transport in situations
situations where supply-limiting
supply-limiting factors
bed slope effects
aeolian sediment
sediment transport
beach armoring
sediment sorting
AgDegBWE-book: Calculator for aggradation and degradation of a river reach using a backwater formulation.e-book
calculator
formulation
aggradation
program computes
differential sediment transport
due to differential
sediment transport
differential sediment
rivers due
sediment
bed variation
transport
computes
assumed
variation in rivers
fluvial morphodynamics
agdegbw
AgDegNormGravMixPWE-book: calculator for aggradation and degradation of sediment mixtures in gravel-bed streamse-book
calculator
streams
constant width carrying
computes the time
time evolution
program computes
long profile
gravel bedload transport
constant width
width carrying
grain size
prescribed elevation
gravel
grain size distribution
gravel sizes
downstream end
elevation
bed profile evolution
fluvial morphodynamics
agdegnormgravmixpw
AgDegNormGravMixSubPWE-book: calculator for evolution of upward-concave bed profiles in rivers carrying sediment mixtures in subsiding basins.e-book
calculator
basins
evolution
constant width carrying
gravel sizes
prescribed elevation
program computes
computes the time
time evolution
long profile
river of constant
constant width
width carrying
carrying a mixture
mixture of gravel
downstream end
sizes
elevation
bed profile evolution
subside
fluvial morphodynamics
agdegnormgravmixsubpw
AgDegNormalE-book: illustration of calculation of aggradation and degradation of a river reach using the normal flow approximation.e-book
illustration
approximation
calculation
workbook computes
differential sediment transport
sediment transport
differential sediment
sediment
due to differential
bed variation
transport
computes
assumed
variation in rivers
fluvial morphodynamics
agdegnormal
AgDegNormalFaultE-book: Illustration of calculation of aggradation and degradation of a river reach using the normal flow approximation; with an extension for calculation of the response to a sudden fault along the reach.illustration
e-book
calculation
reach
sudden vertical fault
program computes
differential sediment transport
undergo a sudden
sudden vertical
vertical fault
sediment transport
differential sediment
due to differential
bed variation
sediment
transport
amount
bed
computes
fluvial morphodynamics
fault
agdegnormalfault
AgDegNormalGravMixHydE-book: A module that calculates the evolution of a gravel bed river under an imposed cycled hydrograph.e-book
hydrograph
module
calculates
imposed cycled hydrograph
gravel bed river
cycled hydrograph
module that calculates
calculates the evolution
gravel bed
bed river
imposed cycled
evolution
gravel
bed
river
bed evolution
fluvial morphodynamics
agdegnormalgravmixhyd
AgDegNormalSubE-book: Program to calculate the evolution of upward-concave bed profiles in rivers carrying uniform sediment in subsiding basins.e-book
program
basins
calculate
subsiding basin
workbook computes
steady state
time evolution
assumed
computes the time
time
basin
workbook
computes
evolution
steady
state
subsiding
river toward steady
bed profile evolution
fluvial morphodynamics
subside
agdegnormalsub
AlluvStratRules-based model to generate a 2-dimensional cross section of alluvial stratigraphy based on fluvial processesrules-based
cross
processes
generates alluvial stratigraphy
generates alluvial
alluvial stratigraphy
channel migration
channel
migration
generates
stratigraphy
fluvial
alluvstrat
Alpine3D3D model of alpine surface processesmodel
processes
high resolution simulation
high resolution
resolution simulation
simulation of alpine
alpine surface processes
snow
alpine surface
meteoro-logical model outputs
vegetation
snow model solving
drifting snow model
automatic weather stations
snow processes
snow dynamics
alpine3d
AnugaANUGA is a hydrodynamic modelling tool that allows users to model realistic flow problems in complex 2D geometries.geometries
anuga
complex
hydrodynamic modelling tool
model realistic flow
realistic flow problems
hydrodynamic modelling
realistic flow
modelling tool
model realistic
python
include dam breaks
anuga components
problems in complex
water
continental
AnugaSedAdd-on package to ANUGA with modules for sediment transport and vegetation draganuga
add-on
drag
simulating depth-averaged flows
hydrodynamic model
model for simulating
simulating depth-averaged
vegetation
depth-averaged flows
operator
simpson and castelltort
davy and lague
vegetation drag operator
vegetation drag
flows
kean and smith
nepf
sediment transport
flood
anugased
ApsimXThe Agricultural Production Systems sIMulator (APSIM)apsim
agricultural
production
systems
agricultural production systems
production systems simulator
highly advanced simulator
agricultural production
production systems
agricultural systems
advanced simulator
internationally recognized
highly advanced
systems simulator
simulator of agricultural
apsimx
AquaTellUsFluvial-dominated delta sedimentation modelfluvial-dominated
model
models fluvial-dominated delta
aquatellus models fluvial-dominated
fluvial-dominated delta sedimentation
fluvial-dominated delta
models fluvial-dominated
aquatellus models
erosion
delta sedimentation
nested model approach
flux
aquatellus
erosion flux
flux depends
longitudinal profiles
sediment
coastal evolution
Area-Slope Equation CalculatorPixel scale Area-Slope equation calculatorpixel
calculator
slope plot
area vs. slope
traditionally the area-slope
area-slope equation
alpha
catchment area
traditionally
equation
plot
area-slope
calculate the area-slope
area-slope constant
catchment
constant and coefficient
downslope neighbor
geomorphologic
area-slope equation calculator
Auto marshCellula automata model for salt marsh evolution with variable soil resistance under wind waves attackcellula
attack
reproduce the effect
salt marsh erosion
soil resistance
model reproduce
soil
salt marsh
randomly distributed resistance
model
wind waves
resistance
erosion
eroded
model consists
critical soil height
distributed resistance
cellula automata
extreme events
ecogemorphology
auto marsh
AvulsionStream avulsion modelstream
model
model stream avulsion
model stream
random walk
stream avulsion
avulsion as random
walk
coastal evolution
avulsion
BEDLOADBedload transport modelbedload
model
bedload transport rates
rates and weights
weights per unit
unit area
transport rates
bedload transport
calculates the bedload
calculates
size-density
transport
fluvial morphodynamics
BOMBergen Ocean Modelmodel
ocean
bergen
three-dimensional hydrodynamic multi-purpose
hydrodynamic multi-purpose model
shelf seas
coupled to biological
re-suspension and contaminant
three-dimensional hydrodynamic
hydrodynamic multi-purpose
coastal and shelf
multi-purpose model
contaminant models
model for coastal
seas
biological
re-suspension
seasonal scale processes
hydrodynamics
bom
BRaKEComputes evolution of a bedrock river longitudinal profile in the presence of large, hillslope-derived blocks.computes
large
hillslope-derived
blocks
profile evolution model
channel profile evolution
bedrock channel profile
evolution model
channel profile
profile evolution
bedrock channel
bedrock
brake
model
bedrock erosion
erosion
bedrock channel erosion
bedrock incision
river profile
channel-hillslope coupling
BackwaterCalculatorE-book: program for backwater calculations in open channel flowe-book
program
flow
open channel flow
program for backwater
channel flow
backwater calculations
calculations in open
open channel
subcritical flow
fluvial morphodynamics
backwatercalculator
BackwaterWrightParkerE-book: calculator for backwater curves in sand-bed streams, including the effects of both skin friction and form drag due to skin frictione-book
skin
friction
calculator
program calculates backwater
calculates backwater curves
spatially constant bed
constant bed slope
program calculates
calculates backwater
backwater curves
sand-bed stream
spatially constant
constant bed
bed slope
wright and parker
flow stratification correction
hydraulic resistance formulation
formulation of wright
elevation profile
fluvial morphodynamics
backwaterwrightparker
BadlandsBasin and landscape dynamicsbasin
dynamics
parallel tin-based landscape
tin-based landscape evolution
landscape evolution model
simulate topography development
landscape dynamics
time scales
tin-based landscape
landscape evolution
parallel tin-based
topography development
space and time
built to simulate
basin and landscape
simulate topography
evolution model
hillslope model
sediment flux
badlands
Barrier Inlet Environment (BRIE) ModelCoastal barrier island transgression modelcoastal
model
simulates storm overwash
barrier transgression resulting
coastal barrier model
estimates coastal barrier
coastal barrier transgression
coastal barrier
sea-level rise
model that simulates
simulates storm
storm overwash
overwash and tidal
tidal inlets
inlets and estimates
transgression resulting
resulting from sea-level
shoreline dynamics
sea level rise
tidal inlet
barrier island
coastal evolution
coastal morphodynamics
barrier inlet environment (brie) model
BatTriA graphical Matlab interface to the C language 2-D quality finite element grid generator Triangle.triangle
matlab
language
quality
file to triangle
triangle and visualizes
mesh editing
bathymetry incorporation
incorporation and interpolation
refinement properties
prepares the input
generation and refinement
input file
visualizes and saves
saves the created
grid generation
created grid
battri
Bedrock Erosion ModelRead note in extended description. Knickpoint propagation in the 2D sediment-flux-driven bedrock erosion modelread
description
code is inactive
module code
inactive
bedrock incision
bedrock erosion model
Bedrock Fault ScarpThis is a two-dimensional numerical model that computes the topographic evolution of the facet slope in the footwall of an active normal fault.fault
two-dimensional
numerical
model
active normal fault
normal fault
code computes
computes the formation
active normal
hillslope profile
hillslope
points move due
prescribed erosion rate
vertical and horizontal
code
computes
formation
profile
fault, erosion, hillslope, facet, spur, scarp
bedrock fault scarp
BedrockAlluvialTransitionE-book: calculator for aggradation and degradation with a migrating bedrock-alluvial transition at the upstream end.e-book
calculator
end
computes fluvial aggradation
program computes fluvial
bedrock-alluvial transition
fluvial aggradation
bedrock basement channel
sba
program computes
computes fluvial
bedrock basement
basement channel
bedrock-alluvial
transition
point sba
alluvial reach
change
bed variation
fluvial morphodynamics
bedrockalluvialtransition
BifurcationFlow-partitioning and avulsion in a river delta bifurcationflow-partitioning
bifurcation
river delta bifurcation
river delta
model
delta bifurcation
avulsion
ongoing avulsion dynamics
model generates
bed elevation profiles
model outputs include
ongoing avulsion
avulsion dynamics
interaction
model generates ongoing
include
BingSubmarine debris flowssubmarine
flows
submarine debris flow
run a submarine
debris flow
submarine debris
run
flow
sediment transport
bing
BioBiogenic mixing of marine sedimentsbiogenic
sediments
biogenic mixing
marine sediments
mixing of marine
sediment transport
bio
BlockLabBlockLab computes landscape evolution in the presence of large blocks of rock on hillslopes and in channels.blocklab
channels
computes
landscape
treats landscape evolution
blocklab treats landscape
treats landscape
landscape evolution
surface rock
blocklab treats
large blocks
rock
evolution in landscapes
landscapes where surface
large
blocks
sediment transport theory
CAESAR LisfloodCaesar Lisflood is a morphodynamic / Landscape evolution model that simulates erosion and deposition in river catchments and reaches over time scales from hours to 1000's of years.landscape
lisflood
caesar
morphodynamic
caesar geomorphic model
landscape evolution model
caesar geomorphic
caesar lisflood
landscape evolution
combines the lisflood-fp
erosion and deposition
bates
model
flow model
simulate erosion
evolution model
time scales
CAM-CARMAA GCM for Titan that incorporates aerosolsgcm
titan
aerosols
titan by friedson
adaptation of cam
converted to titan
developing a recent
recent adaptation
cam
jpl
friedson
microphysics from carma
carma
global climate
cam-carma
CBOFS2The Second Generation Chesapeake Bay Operational Forecast System (CBOFS2): A ROMS‐Based Modeling Systemsystem
generation
chesapeake
bay
regional ocean modeling
ocean modeling system
national ocean service
regional ocean
ocean modeling
operational forecast system
modeling system
ocean service presently
forecast system
baroclinic forecast system
national ocean
ocean service
water levels
special case
cbofs2
CEMCoastline evolution modelcoastline
model
spatial scales ranging
addresses predominately sandy
time-scales ranging
ranging from years
scales ranging
addresses predominately
years to millenia
spatial scales
coastline evolution model
coastline evolution
ranging from kilometers
hundreds of kilometers
kilometers to hundreds
wave-dominated coastlines
ranging
coastal evolution
cem
CHILDLandscape Evolution Modelmodel
evolution
landscape
child computes
sediment transport
computes the time
time evolution
topographic surface
fluvial and hillslope
hillslope erosion
erosion and sediment
child
transport
computes
time
topographic
surface
landscape evolution
erosion
soil erosion
landform development
drainage basin
CICELos Alamos sea ice modelalamos
los
model
polar sea ice
computationally efficient model
simulating the growth
computationally efficient
movement of polar
sea ice model
sea ice
polar sea
ice model suitable
efficient model
cice model
melting
including process studies
cice
global climate models
CLUMondoThe CLUMondo model is a spatially explicit and dynamics land system change modelmodel
clumondo
spatially
explicit
land systems approach
land systems
land
systems
systems approach
land cover
land systems depends
land cover composition
land cover classifications
management activities employed
reflect land
clumondo is based
socio-ecological systems
approach
land system change model
CMFTCoupled salt Marsh - tidal Flat Transect modelmarsh
flat
transect
coupled
coupled long-term evolution
coupled long-term
salt marshes
tidal flats
includes tidal currents
dimensional model
long-term evolution
evolution of salt
framework includes tidal
model framework includes
model
tidal currents
marshes and tidal
includes tidal
flats
ecogemorphic
salt marsh - tidal flat evolution
cmft
CMIPData component provides monthly mean temperature for Permafrost Region 1902-2100permafrost
region
data
1902-2100
model intercomparison project
climate model intercomparison
intercomparison project
data component processed
cru-ncep climate model
called cmip
model intercomparison
component processed
original climate models
data component
cru-ncep climate
data presented include
climate model
project
cmip
CRESTThe Coupled Routing and Excess STorage (CREST) model is a distributed hydrologic model developed to simulate the spatial and temporal variation of atmospheric, land surface, and subsurface water fluxes and storages by cell-to-cell simulation.crest
simulation
coupled
routing
servir project team
nasa servir project
university of oklahoma
project team
nasa servir
servir project
hybrid modeling strategy
distributed hydrological model
excess storage
distributed hydrological
crest model
hybrid modeling
modeling strategy
hydrological model
continental
CVFEM Rift2Dmulti-physics numerical model that simulates rock deformation, fluid flow, solute transport and heat transfer in response to ice sheet loading of multiple cyclesmulti-physics
deformation
fluid
flow
pore pressure evolution
multiple glacial cycles
hybrid numerical model
ice sheet loading
regular finite element
finite element methods
control volume finite
volume finite element
brine migration
stress variation
pore pressure
pressure evolution
solute transport
glacial cycles
finite element
cvfem rift2d
CVPMMultidimensional heat-transfer modeling system for permafrost with advanced unfrozen water physicsmultidimensional
physics
control volume permafrost
control volume
volume permafrost model
modular heat-transfer modeling
volume permafrost
educational tool
designed for scientific
modular heat-transfer
cvpm
modeling system designed
permafrost terrain
nonlinear heat-transfer equations
engineering studies
heat-transfer modeling system
control
permafrost
heat-transfer
earth
mars
CaesarCellular landscape evolution modelcellular
model
including flow routing
multi grainsize sediment
grainsize sediment transport
cellular landscape evolution
landscape evolution model
fluvial processes
including flow
flow routing
multi grainsize
sediment transport
cellular landscape
landscape evolution
emphasis on fluvial
grainsize sediment
caesar
CarboCATCarbonate cellular automatacyclicitycarbonate
automatacyclicity
carbonate lithofacies
cellular automata
automata to model
model horizontal
horizontal and vertical
vertical distributions
distributions of carbonate
carbocat
lithofacies
carbonate lithofacy
cellular automatacyclicity
Channel-OscillationRead note in extended description. Simulates Oscillations in arid alluvial channelsread
description
code is inactive
module code
inactive
channel oscillation
arid alluvial channel
channel-oscillation
ChannelProfilerThe ChannelProfiler extracts and plots channel networks from a landlab grid.grid
extract channel networks
channel networks
order to extract
extract channel
flow connectivity
flow
networks
identified
receiver
order
extract
channel
connectivity
profile
channelprofiler
ChesROMSChesapeake Bay ROMS Community Model (ChesROMS), special case of ROMSchesroms
model
roms
bay
chesapeake research consortium
noaa merhab program
ocean modeling system
research consortium
natural resources
maryland department
noaa merhab
department of natural
chesapeake bay region
regional ocean modeling
rutgers regional ocean
chesapeake bay program
chesapeake research
university of maryland
chesapeake bay
Chi analysis toolsTool for examining channel profiles in chi-elevation space using the integral method of channel analysistool
analysis
channel
examining
examining bedrock channels
examining bedrock
bedrock channels
adequately describes channel
chi-elevation space
describes channel incision
power incision model
stream power incision
statistical tests
spim
channel incision
space
incision model
describes channel
geomorphology
bedrock channel erosion
topographic analysis
chi analysis tools
ChiFinderCalculate Chi Indicesindices
chi
calculate
sensu perron
calculates chi indices
landlab landscape
royden
component calculates chi
chi indices
perron
component calculates
calculates chi
landlab
sensu
landscape
chi index
chifinder
CliffsNumerical model to compute tsunami propagation and runup on land in the shallow-water approximationnumerical
approximation
shallow-water approximation
cliffs features
cartesian or spherical
dimensional splitting
features
shallow-water
titov
synolakis
tsunami
inundation
runup on land
shallow-water model
cliffs
CoastMorpho2DLong term 2D morphodynamics of coastal areaslong
term
morphodynamics
areas
including tidal currents
long term
storm surge
edge erosion
wind waves
swell waves
marsh vegetation
marsh ponding
morphodynamics of coastal
coastal areas
including tidal
tidal currents
sand
mud
waves
coastmorpho2d
Coastal Dune ModelEvolution of Coastal Foredunesforedunes
coastal
evolution
vegetated coastal foredunes
model describing
coastal foredunes
describing the morphodynamic
morphodynamic evolution
evolution of vegetated
vegetated coastal
model
coastal dune model
CompactSediment compactionsediment
compaction
compact a sediment
sediment column
compact
column
CosmoLand2-D model tracking cosmogenic nuclides and mixing in landslide terrainmodel
terrain
simplified landscape undergoing
surface crn concentration
model tracks
tracks both surface
eroded off hillslopes
simplified landscape
landscape undergoing
concentration eroded
fluvial network
surface crn
crn concentration
diffusive-like
concentration
erosion
landslide erosion
landscape evolution
landslides
cosmogenic radionuclides
cosmoland
Coupled1DRead note in extended description. Coupled 1D bedrock-alluvial channel evolutioncoupled
code is inactive
module code
inactive
alluvial-channel evolution
coupled1d
CrevasseFlowThe module calculates crevasse splay morphology and water discharge outflow of a crevasse splay.crevasse
splay
module
calculates
preset flood event
crevasse splay
daily water discharge
water discharge outflow
water discharge
trunk channel downstream
water discharge series
trunk channel
preset flood
flood event
event and evolves
daily water
lower yellow river
coastal evolution
crevasseflow
Cross Shore Sediment FluxCross-Shore Sediment Flux Equationsequations
sediment
flux
cross-shore
cross-shore sediment flux
addresses predominately sandy
sediment flux model
spatial scales ranging
flux model addresses
model addresses predominately
sediment flux
cross-shore sediment
airy wave theory
linear airy wave
predominately sandy
wave-dominated coastlines
full linear airy
time-scales ranging
ranging from years
coastal sediment transport
coastal evolution
cross shore sediment flux
CryoGrid3CryoGrid 3 is a simple land-surface scheme dedicated to modeling of ground temperatures in permafrost environments.cryogrid
environments
represent energy transfer
surface energy balance
energy transfer processes
surface energy
represent energy
energy transfer
calculates the surface
order to represent
model includes processes
energy balance
model calculates
transfer processes
energy
balance in order
radiation balance
permafrost
cryogrid3
CyclopathA 2D/3D model of carbonate cyclicitymodel
cyclicity
scale platform geomtry
carbonate sediment production
generates high-frequency platform
large scale platform
high-frequency platform top
platform top auto
model of carbonate
platform geomtry
carbonate sediment
sediment production
production and transport
transport that generates
generates high-frequency
top auto
auto and allocycles
stratigraphy
cyclopath
DELTASimulates circulation and sedimentation in a 2D turbulent plane jet and resulting delta growthsimulates
turbulent
growth
circulation
turbulent plane jet
resulting delta growth
simulates circulation
turbulent plane
delta growth
circulation and sedimentation
plane jet
jet and resulting
resulting delta
sedimentation
plane
coastal evolution
delta
DHSVMDHSVM is a distributed hydrologic model that explicitly represents the effects of topography and vegetation on water fluxes through the landscape.dhsvm
landscape
distributed
hydrologic
ten years ago
university of washington
distributed hydrology model
years ago
distributed hydrology
hydrology model
ten years
university
washington
ago
continental
DLBRMDistributed Large Basin Runoff Modelmodel
large
basin
runoff
simulates hydrologic processes
entire watershed sequentially
watershed hydrology model
physically based
grid network
hydrology model
model that subdivides
network and simulates
simulates hydrologic
hydrologic processes
watershed sequentially
watershed hydrology
entire watershed
dlbrm
watershed
basins
fluvial morphodynamics
pollutants
DR3MDistributed Routing Rainfall-Runoff Model--version IImodel
routing
distributed
version
branched system
routing storm runoff
rainfall as input
system of pipes
branched
natural channels
routing storm
storm runoff
watershed model
natural
input
basins
dr3m
DROG3D3-DIMENSIONAL DROGUE TRACKING ALGORITHM FOR A FINITE ELEMENT GRID WITH LINEAR FINITE ELEMENTSfinite
drogue
tracking
algorithm
finite element mesh
tracks passive drogues
harmonic velocity field
tracks passive
velocity field
finite element
element mesh
passive drogues
harmonic velocity
tracks
field
mesh
drog3d
DakotathonA Python API for the Dakota iterative systems analysis toolkit.python
api
dakota
toolkit
sandia national laboratories
national laboratories
sandia national
developed at sandia
uncertainty quantification
software toolkit
including support
calibration techniques
support for sensitivity
basic model interface
laboratories
dakota experiment
sandia
national
uncertainty
sensitivity
optimization
calibration
dakotathon
Delft3D3D hydrodynamic and sediment transport modelhydrodynamic
model
cohesive sediment transport
curvilinear multi-domain mesh
wave-current interaction
hydrostatic flow
bed stratigraphy
water quality
particle tracking
online visualization
cohesive sediment
sediment transport
curvilinear multi-domain
spheric coord.
multi-domain mesh
mesh in cartesian
cartesian or spheric
hydrodynamics
coastal and marine
delft3d
DeltaBWE-book: Calculator for evolution of long profile of a river ending in a 1D migrating delta, using a backwater formulation.e-book
calculator
migrating
delta
subaerial fluvial fan-delta
subaerial fluvial
fluvial fan-delta
constant width
subaerial
fluvial
width
constant
constant bed resistance
fan-delta
channel
constant bed
fan-delta prograding
unit width
bed profile evolution
subaerial fluvial delta
deltabw
DeltaClassificationGeometry classification of delta islandsgeometry
islands
active geomorphic processes
extracting information
nature and spatial
spatial extent
extent of active
active geomorphic
geomorphic processes
processes across deltas
unsupervised machine learning
machine learning algorithm
machine learning
ensemble unsupervised machine
remotely sensed imagery
two-step ensemble unsupervised
spatially continuous zones
delta landforms
deltaclassification
DeltaNormE-book: Calculator for evolution of long profile of a river ending in a 1D migrating delta, using the normal flow approximation.e-book
calculator
migrating
delta
subaerial fluvial fan-delta
subaerial fluvial
fluvial fan-delta
constant width
subaerial
fluvial
width
constant
constant bed resistance
fan-delta
channel
constant bed
fan-delta prograding
unit width
bed profile evolution
subaerial fluvial delta
deltanorm
DeltaRCMRiver delta formation and evolution model with channel dynamicsriver
dynamics
rule-based exploratory models
parcel-based cellular flux
cellular flux routing
river deltas
sediment transport model
exploratory models
parcel-based cellular
cellular flux
flux routing
formation of river
broad category
category of rule-based
rule-based exploratory
transport model
sediment transport
delta evolution
cellula automata
coastal morphdynamics
deltarcm
DeltaRCM VegetationDelta-building model DeltaRCM expanded to include vegetationdelta-building
vegetation
delta-building model deltarcm
model deltarcm expanded
included vegetation effects
delta-building model
model deltarcm
deltarcm expanded
expanded to included
vegetation effects
included vegetation
increasing bank stability
effects
vegetation colonizes
logistic growth rate
resistance to flow
delta
delta evolution
deltarcm vegetation
DeltaSIMProcess-response model simulating the evolution and stratigraphy of fluvial dominated deltaic systemsprocess-response
systems
fluvial dominated deltaic
dominated deltaic systems
process-response model simulating
based on simple
erosion and deposition
simulating the evolution
evolution and stratigraphy
stratigraphy of fluvial
fluvial dominated
dominated deltaic
deltaic systems
simple approximations
approximations of erosion
process-response model
model simulating
delta evolution
stratigraphy
fluvial
deltasim
DemeterDemeter - A Land Use and Land Cover Change Disaggregation Modeldemeter
model
land
cover
source python package
open source python
earth system models
integrated assessment model
source python
python package
future land allocations
land allocations generated
change assessment model
assessment model
system models
open source
built to disaggregate
disaggregate projections
projections of future
lulcc
land use and land cover change
DepDistTotLoadCalcE-book: Illustration of calculation of depth-discharge relation, bed load transport, suspended load transport and total bed material load for a large, low-slope sand-bed river.illustration
e-book
load
transport
total load calculator
wright-parker formulation
load calculator
depth-discharge and total
total load
flow resistance
bedload transport
ashida-michiue formulation
suspended load
wright-parker
formulation for flow
formulation for bedload
formulation
calculator
sediment transport
river discharge
fluvial morphodynamics
depdisttotloadcalc
DepressionFinderAndRouterFind depressions on a topographic surface.find
surface
topographic surface
component identifies depressions
default true
component identifies
identifies depressions
find existing routing
component
existing routing fields
routing fields output
finds an outlet
find existing
identifies
topographic
outlet
flow path
drainage
depressionfinderandrouter
DepthDependentDiffuserSoil depth-dependent linear hillslope diffusersoil
diffuser
johnstone and hilley
dependent linear diffusion
linear diffusion rule
style of johnstone
slope dependent linear
component implements
implements a depth
dependent linear
linear diffusion
diffusion rule
hilley
johnstone
slope dependent
vertical velocity profile
prescribed exponential vertical
hillslope
depthdependentdiffuser
DepthDependentTaylorDiffuserThis component implements a depth-dependent Taylor series diffusion rule, combining concepts of Ganti et al. (2012) and Johnstone and Hilley (2014).taylor
ganti
rule
combining
taylor series expansion
johnstone and hilley
taylor series
component inspired johnstone
hillslope sediment flux
nonlinear hillslope flux
hillslope flux derived
series expansion
inspired johnstone
dependent component inspired
math
hillslope sediment
nonlinear hillslope
depth dependent component
andrews-bucknam formulation
soil creep
hillslope
diffusion
depthdependenttaylordiffuser
DetachmentLtdErosionSimulate detachment limited sediment transport.simulate
transport
simulates detachment limited
detachment limited sediment
limited sediment transport
stream power component
simulates detachment
detachment limited
limited sediment
sediment transport
stream power
flow receiver
flow receiver fields
upstream node order
landlab component
power component
component
erosion
detachmentltderosion
Detrital ThermochronCode for estimating long-term exhumation histories and spatial patterns of short-term erosion from the detrital thermochronometric data.code
data
detrital thermochronometric data
estimating long-term exhumation
long-term exhumation histories
code for estimating
thermochronometric data
estimating long-term
long-term exhumation
exhumation histories
histories and spatial
spatial patterns
patterns of short-term
short-term erosion
detrital thermochronometric
detrital thermochron
DiffusionDiffusion of marine sediments due to waves, bioturbationbioturbation
diffusion
waves
diffusion of marine
marine sediments
sediments
sediment transport
DrEICH algorithmAlgorithm for extracting channel networks from high resolution topographic dataalgorithm
data
chi river profile
river profile analysis
predict channel head
channel head locations
chi river
river profile
profile analysis
analysis to predict
river networks
predict channel
head locations
extraction of river
river
extracted channel heads
high resolution lidar
geomorphology
hydrological
bedrock channel erosion
dreich algorithm
Drainage DensityComponent for calculating drainage density in Landlab given a channel networklandlab
component
network
landlab drainage density
calculates landscape-averaged drainage
drainage density component
landscape-averaged drainage density
component calculates landscape-averaged
density component calculates
drainage density
landlab drainage
density component
calculates landscape-averaged
landscape-averaged drainage
component calculates
density
nearest channel
landscape morphology
morphometry
DredgeSlotBWE-book: calculator for aggradation and degradation of sediment mixtures in gravel-bed streams subject to cyclic hydrographs.e-book
calculator
hydrographs
normal flow
flow
dredge slot
normal flow equilibrium
program calculates
normal
depth
wright and parker
flow depth
bed evolution
bed
mobile-bed normal flow
dredge
sediment
flow depth prevailing
fluvial morphodynamics
dredgeslotbw
DynEarthSol3DDynEarthSol3D is a finite element solver that models the momentum balance and the heat transfer of elasto-visco-plastic material in the Lagrangian form.lagrangian
material
form
finite
dynamic earth solver
open-source finite element
finite element code
dynamic earth
transfer in lagrangian
lagrangian form
earth solver
open-source finite
unstructured meshes
finite element
element code
code that solves
solves the momentum
momentum balance
heat transfer
dynearthsol3d
ECSimpleSnowA simple snow modelmodel
previous analysis step
simple snow model
accumulate snow based
analysis step
model that employs
employs an empirical
empirical algorithm
algorithm to melt
melt or accumulate
based on surface
surface temperature
temperature and precipitation
previous analysis
simple snow
snow model
snow
ecsimplesnow
EF5Ensemble Framework For Flash Flood Forecastingforecasting
framework
flash
flood
remote sensing laboratory
university of oklahoma
hydrometeorology and remote
remote sensing
sensing laboratory
sacramento soil moisture
soil moisture accouning
moisture accouning model
oklahoma
water balance models
hydrometeorology
remote
sensing
laboratory
university
flash floods
ef5
ELCIRCEulerian-Lagrangian CIRCulationeulerian-lagrangian
circulation
unstructured-grid model designed
baroclinic circulation
unstructured-grid model
model designed
effective simulation
finite-difference eulerian-lagrangian algorithm
shallow water equations
scales
elcirc
baroclinic
finite-difference eulerian-lagrangian
water equations
written to realistically
river forcings
unstructured-grid
ocean circulation
ENTRAINSimulates critical shear stress of median grain sizessimulates
sizes
critical shear stress
yalin and karahan
karahan formulation
assuming no hiding
bed using yalin
calculates the critical
critical shear
shear stress
stress for entrainment
median size
size-density fraction
yalin
karahan
calculates
formulation
sediment entrainment
entrain
ENTRAINHSimulates critical shields theta for median grain sizessimulates
sizes
critical shields theta
critical shear stress
shields theta
calculates the critical
critical shields
jth fraction
hiding function
critical shear
median size
shear stress
calculates
critical
shields
theta
ith
sediment entrainment
entrainh
ESCAPEparallel global-scale landscape evolution modelparallel
model
simulate earth surface
earth surface dynamics
parallel landscape evolution
landscape evolution model
simulate earth
earth surface
built to simulate
geological times
parallel landscape
landscape evolution
surface dynamics
dynamics at global
global scale
evolution model
address problems related
geomorphology
marine sedimentation
erosion/deposition
parallel computing
python
escape
Ecopath with EcosimEcopath with Ecosim (EwE) is an ecological modeling software suite for personal computersewe
ecosim
ecopath
computers
modeling software suite
personal computers
suite for personal
ecological modeling software
protected areas
address ecological questions
impact and placement
ecological modeling
modeling software
software suite
evaluate
ecopath software package
marine protected areas
ecopath with ecosim
Elv-GSTNumerical 1D research code Elv applied to gravel-sand transitionsnumerical
elv
research
transitions
research code elv
code elv applied
gravel-sand transitions relates
abrupt gravel-sand transitions
code elv
elv applied
relates to blom
gravel-sand transitions
research code
alluvial rivers
advance
halt of abrupt
transitions relates
abrupt gravel-sand
retreat
mixed-size sediment
gravel-bed rivers
sand-bed rivers
elv-gst
Eolian Dune ModelRead note in extended description. Werner's model for eolian dune formation and evolutioncode is inactive
module code
inactive
eolian transport
eolian dune model
ErodeFluvial landscape evolution modelfluvial
model
fluvial landscape evolution
landscape evolution model
modeling tool cmt
csdms modeling tool
fluvial landscape
evolution model
landscape evolution
tool cmt
csdms modeling
modeling tool
written in python
erode
raster-based
ErosionDepositionLandlab component for fluvial erosion/deposition.deposition
landlab
erosion
davy and lague
journal of geophysical
geophysical research
component calculates fluvial
landlab erosiondeposition component
calculates fluvial erosion
erosiondeposition component calculates
derived by davy
component calculates
calculates fluvial
landlab erosiondeposition
single substrate
lague
journal
research
river erosion
sediment transport
landscape evolution
erosiondeposition
EstuarineMorphologyEstimatorEmpirical Assessment Tool for Bathymetry, Flow Velocity and Salinity in Estuaries Based on Tidal Amplitude and Remotely-Sensed Imagerybathymetry
flow
imagery
assessment
present a python
predicts the hydrodynamics
bed elevation
includes a comprehensive
comprehensive set
patterns of channels
channels and bars
bars in mere
python tool
along-channel width profile
python
empirical relations derived
flow velocity
along-channel width
width profile
estuary
morphology
salinity
rapid assessment
tool
estuarinemorphologyestimator
ExponentialWeathererExponential soil production function in the style of Ahnert (1976)ahnert
exponential
implements exponential weathering
component implements exponential
bedrock on hillslopes
soil production
component implements
weathering of bedrock
soil
soil production rate
production
implements exponential
exponential weathering
exponential soil production
style of ahnert
production rate
soil production function
hillslope
weathering
exponentialweatherer
FACETFloodplain and Channel Evaluation Tool (FACET)facet
tool
channel
evaluation
delaware river watersheds
digital elevation models
open source modules
derive reach-scale summaries
high-resolution digital elevation
chesapeake bay
bay and delaware
delaware river
python tool
floodplain geomorphic measurements
river watersheds
elevation models
current tool functionality
geomorphic measurements
open source
channel evaluation tool
floodplains
floodplain extent
channel width
FLDTASimulates flow characteristics based on gradually varied flow equationsimulates
equation
flow
characteristics
gradually varied flow
varied flow equation
open channel
velocity and depth
depth based
gradually varied
flow velocity
varied flow
flow equation
calculates the flow
calculates
channel
velocity
depth
reaches
fldta
FTCS1D-NonLinearRead note in extended description. Forward Time Centered Space (FTCS) method for 1D nonlinear diffusion equationftcs
code is inactive
module code
inactive
sediment transport
diffusion
ftcs1d-nonlinear
FTCS2DRead note in extended description. Forward Time Centered Space (FTCS) method for 2D diffusion equationftcs
code is inactive
module code
inactive
sediment transport
diffusion
ftcs2d
FTCS2D-TerraceDiffusionRead note in extended description. Forward Time Centered Space (FTCS) method for 2D Terrace diffusionftcs
code is inactive
module code
inactive
sediment transport
diffusion
ftcs2d-terracediffusion
FUNDYa 3-D diagnostic model for continental shelf circulation studiesdiagnostic
studies
barotropic boundary conditions
linear finite elements
linearized shallow water
shallow water equations
water equations forced
boundary conditions
finite elements
solves the linearized
linearized shallow
shallow water
water equations
equations forced
forced by tidal
barotropic boundary
density gradient
continental shelf circulation
hydrodynamics
fundy
FUNWAVEFully Nonlinear Boussinesq Wave Modelmodel
nonlinear
boussinesq
wave
time-stepping boussinesq model
time-stepping boussinesq
ocean surface wave
surface wave propagation
boussinesq model
funwave
model for ocean
ocean surface
surface wave
wave propagation
phase-resolving
time-stepping
nearshore
wave dynamics
FVCOMThe Unstructured Grid Finite Volume Coastal Ocean Modelmodel
unstructured
grid
finite
umassd-whoi joint efforts
ocean circulation model
circulation model developed
coastal ocean circulation
joint efforts
ocean turbulent model
umassd-whoi joint
primitive equation coastal
general ocean turbulent
circulation model
fvcom
ocean circulation
primitive equation
developed by umassd-whoi
equation coastal ocean
physical oceanography
FVshockFinite Volume two-dimensional shock-capturing model.volume
finite
model
two-dimensional shallow water
shallow water equations
numerical model solves
sediment transport
bed-load and suspended
suspended load
two-dimensional shallow
shallow water
modes of sediment
canestrelli
solves the two-dimensional
water equations
partial differential equations
differential equations cast
numerical model
hydro-morphodynamic
fluvial
fvshock
FallVelocityE-book: Particle fall velocity calculatore-book
particle
calculator
fall velocity
velocity for spheres
fluvial morphodynamics
fallvelocity
FastscapeEroderCompute fluvial erosion using stream power theory (“fastscape” algorithm)fastscape
algorithm
compute
theory
braun-willett fastscape approach
braun-willett fastscape
fastscape approach
stream power framework
power framework
approach to calculate
calculate the amount
amount of erosion
stream power scheme
stream power
explicit stream power
grid
framework
power scheme
erosion
fastscapeeroder
FillinPitsFlatsDEMRead note in extended description. Filling in pits and flats in a DEMread
description
note
extended
code is inactive
module code
inactive
hydrologivally corrected dem
fillinpitsflatsdem
FineSed3DA turbulence-resolving numerical model for fine sediment transport in bottom boundary layerlayer
fine sediment transport
turbulence-resolving numerical model
layer is developed
fine sediment
sediment transport
turbulence-resolving numerical
bottom boundary layer
simplified eulerian two-phase
eulerian two-phase flow
sediment
equilibrium eulerian approximation
numerical model
boundary layer
sediment settling velocity
simplified eulerian
turbulence-resolving
finesed3d
FireGeneratorThis component generates a random fire event or fire time series from the Weibull statistical distribution.weibull
distribution
fire
component
component generates random
generates random numbers
weibull distribution
weibull distribution assumes
component generates
generates random
random numbers
fire regime
fire recurrence units
distribution assumes
time
random
probability distribution
firegenerator
Flex1DRead note in extended description. Fourier filtering in 1D while solving the flexure equationread
description
code is inactive
module code
inactive
lithosphere deflection
flex1d
Flex2DRead note in extended description. Fourier filtering in 2D while solving the flexure equationread
description
code is inactive
module code
inactive
lithosphere deflection
flex2d
Flex2D-ADIRead note in extended description. Solving the flexure equation applying Advection Diffusion Implicit (ADI) methodadi
method
code is inactive
module code
inactive
lithosphere deflection
flex2d-adi
FlexureDeform the lithosphere with 1D or 2D flexure.flexure
deform
lithospheric flexure model
landlab component
lithospheric flexure
flexure model
component that implements
landlab
lithospheric
model
deflection
isostasy
FlowAccumulatorComponent to accumulate flow and calculate drainage area.component
area
calculates drainage area
drainage area
calculates drainage
accumulates flow
flow
flowaccumulator supports multiple
calculating flow direction
flowaccumulator
flowaccumulator component
drainage
flow path
FlowDirectorD8Single-path (steepest direction) flow direction with diagonals on rasters.single-path
steepest
flow
rasters
flow direction finding
steepest direction
finding on raster
raster grids
direction finding
flow direction
direction
method
finding
raster
grids
flow path
flow director
flowdirectord8
FlowDirectorDinfFlow direction on a raster grid by the D infinity method.method
flow
tarboton
directs flow
directs
flow directions
steepest subtriangle
subtriangle
flow path
flow director
flowdirectordinf
FlowDirectorMFDMultiple-path flow direction with or without out diagonals.multiple-path
diagonals
flow direction method
multiple flow direction
direction method
multiple flow
directs flow
assigned multiple flow
flow
flow direction
neighboring nodes
multiple
assigned multiple
directs
method
flow path
flow director
flowdirectormfd
FlowDirectorSteepestSingle-path (steepest direction) flow direction without diagonals.single-path
steepest
flow
diagonals
descent flow directions
single-path steepest descent
steepest descent flow
steepest single-path steepest
flow directions
components finds
descent flow
steepest single-path
single-path steepest
steepest descent
directions
finds the steepest
flow path
flow director
flowdirectorsteepest
Fourier-Bessel-integrationRead note in extended description. Numerical integration of Fourier-Bessel termscode is inactive
module code
inactive
morphologic
volcanic cone
fourier-bessel-integration
FractionalNoises1DRead note in extended description. 1D fractional-noise generation with Fourier-filtering methodcode is inactive
module code
inactive
stochastic
fractionalnoises1d
FractionalNoises2DRead note in extended description. 2D Gaussian fractional-noise generation with Fourier-filtering methodcode is inactive
module code
inactive
stochastic
fractionalnoises2d
FractureGridGeneratorCreate a 2D grid with randomly generated fractures.create
grid
fractures
cell wide
exist
fracture networks
wide
cell
weathering
erosion
flow dynamics
fracturegridgenerator
Frost ModelFrost model predicts the likelihood of occurrence of permafrost in the land surface based on the monthly temperature distributionfrost
distribution
model
predicts
air frost number
thawing degree days
dimensionless ratio based
frost number
model implement
implement the calculation
dimensionless ratio
freezing and thawing
thawing degree
degree days
air frost
ratio based
based on freezing
number
annual temperature distribution
annual temperature
cryosphere
permafrost
frost model
FwDETCalculate floodwater depth based on an inundation polygon (e.g. from remote sensing) and a DEMdem
calculate
polygon
sensing
flood extent layer
extent layer
quick estimation
estimation of water
water depths
flooded domain
flood extent
layer
flood
gis
water depth
fwdet
GEOMBESTGeomorphic Model of Barrier, Estuarine, and Shoreface Translationsestuarine
barrier
translations
model
morphological-behaviour model
model that simulates
simulates the evolution
evolution of coastal
coastal morphology
morphology and stratigraphy
stratigraphy resulting
sea level
level and sediment
sediment volume
geombest
shoreface
estuary
morphological-behaviour
barrier island
coastal morphdynamics
coastal sediment transport
morphologic
longshore sediment transport
GEOMBEST++Geomorphic model of barrier, estaurine, and shoreface translations plus dynamic marsh plus wavesestaurine
geomorphic
barrier
waves
geombest
morphological-behaviour model
model that simulates
coastal morphology
morphology and stratigraphy
stratigraphy resulting
sea level
level and sediment
sediment volume
simulates the evolution
evolution of coastal
introducing wave erosion
evolution
shoreface
marsh
barrier island
wave erosion
overwash
sea level rise
geombest++
GEOMBEST++SeagrassGeomorphic Model of Barrier, Estuarine, and Shoreface Translations + Marsh + Seagrassestuarine
marsh
seagrass
barrier
geombest
morphological-behaviour model
model that simulates
simulates the evolution
evolution of coastal
coastal morphology
morphology and stratigraphy
stratigraphy resulting
sea level
level and sediment
sediment volume
incorporating seagrass dynamics
seagrass builds
incorporating seagrass
barrier island
coastal evolution
geombest++seagrass
GEOMBEST-Plus2D cross-shore geomorphological model of barrier island and marsh response to sea level rise.cross-shore
rise
geomorphic model
sea level
coastal morphology
shoreface translations
geombest-plus differs
barrier and estuary
morphological-behaviour model
dean and maumeyer
large-scale behaviour models
barrier
shoreface
sediment volume
estuarine
geombest-plus
geomorphic
overwash
sea level rise
barrier island
marsh
GEOtopDistributed hydrological model, water and energy budgetsdistributed
model
water
budgets
water balance integrates
energy balance equation
accommodates very complex
complex topography
richards’ equation
surface energy balance
balance integrates
geotop accommodates
balance equation
geotop
surface snow temperature
digital elevation models
return surface temperature
models
land surfaces models
basins
GFlexMultiple solution methods for isostasy and lithospheric flexuremultiple
flexure
geoscientific model development
model development
geoscientific model
submitted to geoscientific
wickert gflex flexure
gflex flexure model
flexure model
wickert
landlab wrapper
wickert gflex
model
development
geoscientific
landlab
install
lithospheric flexure
gflex
GIPLGIPL(Geophysical Institute Permafrost Laboratory) is an implicit finite difference one-dimensional heat flow numerical model.gipl
geophysical
laboratory
institute
geophysical institute permafrost
institute permafrost laboratory
geophysical institute
one-dimensional heat flow
difference one-dimensional heat
permafrost laboratory
heat flow numerical
institute permafrost
gipl model
implicit finite difference
finite difference one-dimensional
flow numerical model
one-dimensional heat
heat flow
permafrost
GISKnickFinderThis python code can be used to find knickpoints and extract information about streams, it utilizes built-in functions of ArcGIS.streams
arcgis
find knickpoints based
find knickpoints
knickpoints based
create longitudinal profiles
landscape
stream including
stream path
knickpoint locations
elevation
created
find
based
curvature
longitudinal profiles
stream
gisknickfinder
GISS AOMGISS Atmosphere-Ocean Modelgiss
model
atmosphere-ocean model
simulates the earth
gridded domain
earth
computer program
program that simulates
earth orbital parameters
earth climate
prognostic variables
earth atmospheric constituents
earth surface distribution
model requires
earth topography
prognostic variables include
giss aom
GISS GCM ModelEGISS GCM ModelEgiss
gcm
modele
earth system models
coupled atmosphere-ocean models
including interactive atmospheric
interactive atmospheric chemsitry
land surface components
system models
earth system
atmosphere-ocean models
giss series
configurations of earth
including interactive
atmospheric chemsitry
carbon cycle
standard atmosphere
sea ice
giss gcm modele
GLUDMGlobal future agricultural land use dynamics modelglobal
model
unique regression equation
calculates a unique
unique regression
relative area
global population
global population predictions
predicted global population
regression equation
land
specific land
model calculates
population predictions
population
relative
land use
agriculture
future
gludm
GNESet of biogeochemical sub-models that predicts river exportset
export
human impact characteristics
predicts annual river
annual river exports
set of biogeochemical
impact characteristics
basin models
biogeochemical sub-models
sub-models that predicts
predicts annual
annual river
river exports
function of basin-aggregated
basin-aggregated natural
natural and human
human impact
biogeochemistry
water quality
gne
GOLEMLandscape evolution modellandscape
model
landscape evolution model
landscape evolution
evolution model
golem
GRLPEvolves gravel-bed river long profilesevolves
profiles
transport-limited gravel-bed rivers
semi-implicit numerical
transport-limited gravel-bed
analytical and numerical
compute long-profile evolution
gravel-bed rivers
computes transient
long-profile evolution
numerical
experience flow resistance
valley-resolving exner equation
meyer-peter and müller
bed-material sediment discharge
evolution of transport-limited
compute long-profile
alluvial-channel evolution
long profile
grlp
GSDCalculatorE-book: Calculator for statistical characteristics of grain size distributions.e-book
calculator
distributions
distribution statistics calculator
size distribution statistics
grain size distribution
statistics calculator
size distribution
distribution statistics
grain size
size
distribution
statistics
grain
fluvial morphodynamics
gsdcalculator
GSFLOWGround-water and Surface-water FLOW modelsurface-water
flow
ground-water
model
geological survey modular
geological survey precipitation-runoff
precipitation-runoff modeling system
survey precipitation-runoff modeling
survey modular groundwater
geological survey
modular groundwater flow
modeling system
coupled model based
survey modular
groundwater flow model
survey precipitation-runoff
precipitation-runoff modeling
modular groundwater
model based
hydrological model
basin
gsflow
GSFLOW-GRASSQuickly generates input files for and runs GSFLOW, and visualizes the outputgsflow
quickly
output
generates
usgs integrated groundwater
quickly generates input
generates input files
surface-water model
runs gsflow
usgs integrated
quickly generates
integrated groundwater
outputs of gsflow
generates input
input files
visualize the outputs
usgs
hydrological model
watershed
groundwater
gsflow-grass
GST-extendedmodelExtended GST model: combination of an analytical GST migration model combined with closure relations based on the assumption of quasi-equilibrium conditionsgst
extended
combination
conditions
analytical gst migration
gst migration model
extended gst model
migration model combined
analytical gst
gst migration
closure relations
surface texture
quasi-equilibrium conditions
extended gst
combined with closure
slope and surface
assumption of quasi-equilibrium
gst model
gravel-sand transitions
mixed-size sediment
gravel-bed rivers
sand-bed rivers
gst-extendedmodel
Gc2dGlacier / ice sheet evolution modelglacier
ice
model
models the growth
ice sheets
growth and evolution
evolution of valley
valley glaciers
glaciers and ice
models
sheets
growth
evolution
valley
glaciers
cryosphere
gc2d
GeoClawDepth-averaged fluid dynamics for modeling geophysical flows and wave propagationdepth-averaged
propagation
originally developed
modeling tsunami generation
storm surge modeling
tsunami generation
dam break problems
developed for modeling
modeling tsunami
surge modeling
modeling
originally
inundation
generation
overland flooding
dam break
shallow-water model
tsunami
storm wave
geoclaw
Glimmer-CISMDynamic thermo-mechanical ice sheet modeldynamic
model
ice sheet model
global climate models
three-dimensional thermomechanical ice
thermomechanical ice sheet
sheet model
climate models
open source
three-dimensional thermomechanical
gpl
thermomechanical ice
ice sheet
range of global
global climate
nerc genie project
nerc genie
glimmer-cism
GosplGlobal Scalable Paleo Landscape Evolutionevolution
scalable
paleo
landscape
simulate global-scale forward
global-scale forward models
stratigraphic history forced
deforming plate tectonics
coarse and fine
landscape evolution
paleotopographies and paleoclimate
paleoclimate reconstructions
complete sediment routing
sediment routing perspective
simulate global-scale
global-scale forward
forward models
models of landscape
stratigraphic history
gospl
GrainHillCellular automaton model of hillslope evolutioncellular
evolution
grain hill model
grain hill
hill model
computational framework
rock
hill
model
study slope forms
disturbance
grain
stochastic disturbance
grain aggregates
cells representing
events
stochastic disturbance events
grainhill
GravelSandTransitionE-book: Calculator for evolution of long profile of river with a migrating gravel-sand transition and subject to subsidence or base level rise.e-book
calculator
rise
evolution
gravel-bed reach
sand-bed reach
reach
gravel-bed
sand-bed
calculates the long
long profile
gravel
sand
transport
assumed
model
bed material
model calculates
bed
bed evolution
subside
fluvial morphodynamics
gravelsandtransition
GreenAmptInfiltrationModelThe Green-Ampt method of infiltration estimation.estimation
infiltration estimation
green-ampt method
method of infiltration
greenamptinfiltrationmodel
GroundwaterDupuitPercolatorThe GroundwaterDupuitPercolator solves the Boussinesq equation for flow in an unconfined aquifer over an impermeable aquifer base and calculates groundwater return flow to the surface.boussinesq
flow
aquifer
surface
shallow groundwater flow
modeling shallow groundwater
modeling shallow
groundwater flow
hydraulic conductivity
vertical component
shallow groundwater
flow is negligible
landlab components
groundwater table approaches
groundwater
total groundwater
hydraulic
conductivity
hydrology
seepage
groundwaterdupuitpercolator
GullyErosionProfiler1DThis model is designed to simulate longitudinal profiles with headward advancing headcuts.headcuts
simulate longitudinal profiles
headward advancing headcuts
longitudinal profiles
profiles with headward
headward advancing
simulate longitudinal
model simulates gully
advancing headcuts
model simulates
model
model is designed
gully
elevation profile
matlab
arid alluvial channel
gullyerosionprofiler1d
HBVHBV model is a rainfall-runoff modelhbv
model
rainfall-runoff
hydrologiska byråns vattenbalansavdelning
includes conceptual numerical
byråns vattenbalansavdelning
hydrologiska byråns
conceptual numerical descriptions
hbv hydrological model
catchment scale
includes conceptual
conceptual numerical
rainfall-runoff model
hbv model
hydrological processes
hbv hydrological
hydrological model
professor amir aghakouchak
discharge
HIMHallberg Isopycnal Modelmodel
isopycnal
hallberg
boussinesq primitive equations
primitive equation model
general orthogonal horizontal
orthogonal horizontal coordinates
isopycnal vertical coordinates
solving the boussinesq
boussinesq primitive
simulating the ocean
equation model
ocean by numerically
numerically solving
general orthogonal
orthogonal horizontal
primitive equation
isopycnal vertical
him
HackCalculatorCalculate Hack parameters.hack
calculate
parameters
component calculates hack
drainage basins
hacks law
component calculates
calculates hack
drainage
law parameters
drainage area
drainage divide
law
basins
parameter fit
component
hack ’s law
parameter calculation
hackcalculator
HexWatershedA watershed delineation model based on hexagonal mesh grid
Hilltop and hillslope morphology extractionTools for extracting hilltops and analysing hillslope morphologytools
morphology
sample hilltop curvature
high resolution topography
variable length scales
performing hillslope traces
computing curvature
slope and aspect
hilltop curvature
series of tools
tools for extracting
extracting a network
aspect over variable
scales from high
high resolution
resolution topography
topography and performing
topographic analysis
hilltop and hillslope morphology extraction
Hilltop flow routingAlgorithm for directly measuring hillslope length from high resolution topographic dataalgorithm
data
generating hillslope length
generating hillslope
hillslope length
flow path
hilltop pixel
length and relief
hillslope scale
landscape scale
relief data
produces a flow
hillslope
nonlinear sediment flux
sediment flux laws
scale
tool produces
geomorphology
hillslope model
sediment flux
hilltop flow routing
HogbackEvolution of a hogbackevolution
hogback
model evolves
rate
rock
HydroTrendClimate driven hydrological transport modelclimate
model
hydrological water balance
simulates water discharge
climate-driven hydrological water
river outlet
climate-driven hydrological
balance and transport
transport model
model that simulates
discharge and sediment
sediment load
hydrological water
water balance
simulates water
water discharge
hydrotrend
basins
hydrological model
sediment transport
river
hydrological
transport
HydromadHydrological Model Assessment and Developmentdevelopment
model
assessment
hydrological
hydrological model assessment
compare hydrological models
assessment and development
model assessment
hydrological model
analyse and compare
compare hydrological
set of functions
functions which work
manipulate
hydromad
package
event separation
Hyper2D Turbidity Current modelturbidity
current
model
sediment failure
hyperpycnal transport
transport after sediment
transport
sediment
failure
hyperpycnal
sediment transport
hyper
IDAAn implementation of the Implicit Drainage Area method (regular and hybrid versions) for calculating drainage area from flow directions using parallel iterative solvers.drainage
area
implicit
method
implicit equations
formulates the task
task of determing
ida formulates
drainage area
distributed memory systems
ida
processor
determing the drainage
ida permits large
flow
system of implicit
memory systems
flow directions
drainage basin
watershed
hydrological
parallel computing
ILAMBThe International Land Model Benchmarking (ILAMB) toolkitilamb
toolkit
benchmarking
international
integration project designed
land surface processes
key land surface
international land model
land model benchmarking
land model performance
surface processes
land model
improve the design
integration project
project designed
campaigns to reduce
reduce uncertainties
international community
international land
benchmark
uncertainty
cmip5
cmip6
ISSMIce Sheet System Model (ISSM)issm
model
sheet
system
jet propulsion laboratory
california at irvine
jet propulsion
propulsion laboratory
laboratory and university
university of california
grace science team
national science foundation
sea-level change team
greenland and antarctica
nasa sea-level change
science team
change team
irvine
technology and development
ice sheet
glacier
sea-level rise
glacial isostatic adjustment
gia
Ice-sheet-Glacier-reconstructionRead note in extended description. Sandpile method for ice-sheet and glacier reconstructioncode is inactive
module code
inactive
cryosphere
ice-sheet-glacier-reconstruction
IceFlow2D semi-implicit shallow ice approximation glacier modelsemi-implicit
model
simulates ice dynamics
simplified basal sliding
glacial systems
iceflow simulates ice
dynamics by solving
solving equations
equations for internal
internal deformation
deformation and simplified
basal sliding
alongside basal sliding
simplified basal
iceflow simulates
simulates ice
ice dynamics
glacial
iceflow
IceagesRead note in extended description. Stochastic-resonance subroutine of Pleistocene ice agescode is inactive
module code
inactive
cryosphere
iceages
IcepackIcepack is a Python package for simulating the flow of glaciers and ice sheets, as well as for solving glaciological data assimilation problems.python
icepack
sheets
problems
data assimilation problems
solving glaciological data
glaciological data assimilation
python package
ice sheets
assimilation problems
package for simulating
simulating the flow
flow of glaciers
glaciers and ice
solving glaciological
glaciological data
data assimilation
ice flow
ice sheet
glacier flow
InflowSteady-state hyperpycnal flow modelsteady-state
model
steady-state hyperpycnal flow
hyperpycnal flow model
steady-state hyperpycnal
flow model
hyperpycnal flow
hyperpycnal inflows
river
inflow
KWAVEA model representing infiltration, interception, and runoff using the kinematic wave approximationinterception
infiltration
approximation
kinematic wave equation
equation to represent
green-ampt equation
represent infiltration
wave equation
represent runoff
kinematic wave
equation
represent
landscape
model
green-ampt
kinematic
wave
kwave
KnickZone-PickerMatlab-based scripts to extract topometrics for catchments and identify river knickpoints.matlab-based
knickpoints
jgr earth surface
jgr earth
earth surface
matlab-based scripts extract
research
cite
calibration and validation
steepness index
code
knickzone selection algorithm
analyze transient landscapes
matlab-based scripts
automated knickzone selection
catchment scale based
log area
knickzone-picker
Kudryavtsev ModelPermafrost Active Layer Thickness Model based on Kudryavtsev's parametrizationactive
layer
thickness
model
active layer thickness
models the temporal
active layer
layer thickness
temporal and spatial
spatial distribution
permafrost soils
soil thermal properties
underlying approximation accounts
temperature
snow cover
models
permafrost
cryosphere
kudryavtsev model
LEMmingLEMming landscape evolution model: a 2-D, regular-grid, rules-based, hybrid finite-difference / cellular automaton model that is designed to explore the effect of multiple rock types on landscape evolution.regular-grid
rules-based
landscape
evolution
lemming tracks regolith
lemming tracks
rockfall
including bedrock erosion
rockfall debris
steep slopes
sediment fluxes
including bedrock
tracks regolith
slope angle
regolith
slope
cell
debris
based
landscape evolution
rock type
lemming
LEMming22D model that simulates the retreat of hard-capped cliffsmodel
cliffs
finite-difference landscape evolution
landscape evolution model
finite-difference landscape
landscape evolution
hard-capped cliffs
evolution model
nonlinear-diffusion erosion equations
regular grid
finite-difference
simulates the retreat
retreat of hard-capped
model that simulates
implements common
nonlinear-diffusion erosion
landscape
lemming2
LISFLOODLISFLOOD - a distributed hydrological rainfall-runoff modellisflood
model
joint research centre
semi-physical hydrological rainfall-runoff
research centre
hydrological rainfall-runoff model
joint research
commission in late
european commission
european flood awareness
spatially distributed
semi-physical hydrological
flood awareness system
emergency management system
hydrological rainfall-runoff
rainfall-runoff model
copernicus emergency management
hydrological model
rainfall-runoff
LITHFLEX1Lithospheric flexure solutionlithospheric
solution
lithospheric flexure solution
lithospheric flexure
infinite plate
flexure solution
solution for infinite
greens function
convolved with greens
load
plate
continuous plate
lithflex1
LITHFLEX2Lithospheric flexure solution for a broken platelithospheric
plate
lithospheric flexure solution
lithospheric flexure
flexure solution
broken plate
equal width loading
width loading elements
broken edge
broken
load is assumed
flexure
solution
edge of plate
lithflex2
LOADESTSoftware for estimating constituent loads in streams and riverssoftware
rivers
fortran program
maximum likelihood estimation
estimating constituent loads
additional data variables
likelihood estimation
estimation
maximum likelihood
streams and rivers
regression model
loadest
program for estimating
data variables
estimating constituent
adjusted maximum likelihood
data
biogeochemistry
water quality
LOGDISTLogrithmic velocity distribution solutionlogrithmic
solution
called from trcalc
logrithmic velocity distribution
velocity distribution called
calculates the logrithmic
trcalc
logrithmic velocity
velocity distribution
distribution called
calculates
vertical velocity profile
fluvial
logdist
LONGPRODynamic evolution of longitudinal profilesdynamic
profiles
stream longitudinal profile
longitudinal profile
program to calculate
calculate the dynamical
dynamical evolution
stream longitudinal
profile
program
calculate
dynamical
evolution
stream
longitudinal
fluvial morphodynamics
longpro
LTRANSThe Larval TRANSport Lagrangian model (LTRANS) is an off-line particle-tracking model that runs with the stored predictions of a 3D hydrodynamic model, specifically the Regional Ocean Modeling System (ROMS).ltrans
roms
system
larval
ocean modeling system
regional ocean modeling
modeling system
regional ocean
ocean modeling
larval transport lagrangian
transport lagrangian model
specifically the regional
transport lagrangian
off-line particle-tracking model
lagrangian model
off-line particle-tracking
stored predictions
larval transport model
LaMEMLaMEM - Lithosphere and Mantle Evolution Modellamem
lithosphere
model
mantle
thermomechanical geodynamical processes
model various thermomechanical
thermomechanical geodynamical
geodynamical processes
mantle-lithosphere interaction
interaction for rocks
numerical code
rheologies
finite difference discretization
code
parallel
numerical
staggered finite difference
difference discretization
mantle evolution model
LakeMapperBarnesTemporarily fills depressions and reroutes flow across themtemporarily
landlab by dejh
landlab
lake
barnes
landlab implementation
lakes
lake routing algorithms
adapted for landlab
flow
component
surface
map
run
flow routing
routing
flow path
depressions
lakemapperbarnes
LandlabPython software framework for writing, assembling, and running 2D numerical modelsassembling
python
writing
running
python software package
python software
software package
package for creating
landlab
numerical models
models
powerful gridding engine
engine for creating
gridding engine
toolkit
creating
components
LandslidesLandlab component that simulates landslide probability of failure as well as mean relative wetness and probability of saturation.probability
landlab
saturation
component
infinite slope stability
slope stability model
stability model driven
monte carlo simulation
relative wetness
number of iterations
monte carlo
soils inputs
infinite slope
slope stability
stability model
model driven
driven by topographic
topographic and soils
recharge provided
landslides
hazards
LateralEroderLaterally erode neighbor node through fluvial erosion.laterally
erosion
calculates lateral erosion
landlab component
lateral erosion
component that finds
finds a neighbor
neighbor node
node to laterally
laterally erode
erode and calculates
calculates lateral
landlab
lateraleroder
LateralVerticalIncisionGeometric model to explore autogenic increase of vertical incision rate in entrenching alluvial rivers.geometric
rivers
promote vertical incision
increasingly tall valley
river lateral erosion
tall valley walls
valley walls constrain
vertical incision
explore how increasingly
increasingly tall
tall valley
constrain the river
erosion and promote
promote vertical
river lateral
lateral erosion
valley walls
meander center line
river
lateralverticalincision
LavaFlow2DRead note in extended description. 2D radially symmetric lava flow modelcode is inactive
module code
inactive
geodynamics
lavaflow2d
LinearDiffuserLandlab component that models soil creep as a linear diffusion processlandlab
process
models soil creep
explicit finite-volume solution
diffusion equation
landlab component
component that models
models soil
soil creep
explicit finite-volume
finite-volume solution
lineardiffuser
diffusion
equation
component
models
hillslope
hillslope model
LithologyCreate a Lithology object with different propertieslithology
create
properties
landlab components
dimensional representation
landlab
material operated
components
erodibility
geology
LossyFlowAccumulatorComponent to calculate drainage area and accumulate flow, while permitting dynamic loss or gain of flow downstream.component
downstream
flow
calculate
finding flow directions
closely related
finding flow
flow directions
user-specified method
calculating the drainage
drainage area
component additionally requires
component is closely
component additionally
area and discharge
flowaccumulator
discharge
gained downstream
flow dynamics
drainage
flow path
lossyflowaccumulator
LuSSA set of MATLAB functions to model how luminescence evolves in different geomorphic scenarios.matlab
scenarios
resulting signals shown
exposures to heat
signals shown
heat and sunlight
resulting signals
luminescence rate equations
exposures
shown
rate equations
underlying luminescence rate
brown
luminescence
osl
luss
LumSoilMixerThis is a model to simulate the non-dimensionalized luminescence in a mixing soil.soil
model
simulate
non-dimensionalized
non-dimensional equation
fokker-plank equation
mixing soil
equation for luminescence
equation
non-dimensional
luminescence
mixing
derived
fokker-plank
lumsoilmixer
MARM5DLandscape-scale soil evolution modellandscape-scale
model
explicit particle size
particle size distribution
simulates soil evolution
spatial dimensions
temporal dimension
explicit particle
particle size
size distribution
distribution and temporal
simulates soil
prefix
soil evolution
dimensions
dimension
simulates
pedogenesis
landform development
soil
marm5d
MARSSIMLandform evolution modellandform
model
landform evolution model
evolution model operating
larger scale
landform evolution
drainage basin
basin or larger
evolution model
model operating
scale
recent model development
targeted planetary applications
landscape evolution
marssim
MCPMA stand alone model for the morphological evolution of an idealized transect across a marsh channel-and-platform.marsh
stand
model
morphological
idealized transect
millennial time scales
model simulates morphological
simulates morphological evolution
mcpm
MFDroutingRead note in extended description. Multiple Flow Direction (MFD) flow routing methodmfd
read
description
code is inactive
module code
inactive
basins
mfdrouting
MFDrouting-SuccessiveRead note in extended description. Successive flow routing with Multiple Flow Direction (MFD) methodmfd
read
description
code is inactive
module code
inactive
basins
mfdrouting-successive
MICOMMiami Isopycnic Coordinate Ocean Modelmodel
isopycnic
coordinate
ocean
primitive equation numerical
equation numerical model
evolution of momentum
heat and salt
primitive equation
equation numerical
numerical model
model that describes
describes the evolution
mass
micom
momentum
heat
primitive
MIDASCoupled flow- heterogeneous sediment routing modelcoupled
flow
heterogeneous
model
single channel flow
heterogeneous size-density mixtures
channel flow model
movable bed
single channel
size-density mixtures
channel flow
heterogeneous size-density
flow model
quasi-unsteady
model for heterogeneous
nonuniform
movable
bed
single
fluvial morphodynamics
midas
MITgcmThe MITgcm (MIT General Circulation Model) is a numerical model designed for study of the atmosphere, ocean, and climate.ocean
mit
model
general
mit general circulation
general circulation model
numerical model designed
mit general
general circulation
circulation model
numerical model
model designed
designed for study
circulation
state estimation problems
non-hydrostatic formulation enables
mitgcm
MODFLOWMODFLOW is a three-dimensional finite-difference ground-water modelmodflow
model
three-dimensional finite-difference ground-water
three-dimensional finite-difference
flow
finite-difference ground-water model
finite-difference ground-water
ground-water flow
ground-water
boundary
head
geological survey
three-dimensional
finite-difference
published
basins
MOM6MOM6 is the latest generation of the Modular Ocean Model which is a numerical model code for simulating the ocean general circulation.ocean
model
modular
circulation
modular ocean model
ocean general circulation
numerical model code
modular ocean
ocean model
numerical model
model code
ocean general
general circulation
code for simulating
simulating the ocean
latest generation
ocean circulation
mom6
MRSAAMacro-roughness model framework for treating erosion, bed cover, and sediment transport in bedrock river channels.macro-roughness
erosion
bed
cover
earth surface dynamics
earth surface
surface dynamics
macro-roughness model
alluvial river morphodynamics
code functionality
model of bedrock
stark
functionality and purpose
inoue
viparelli
references
alluvial river
izumi
sediment transport
mrsaa
Manningseq-bouldersforpaleohydrologyMatlab® code for paleo-hydrological flood flow reconstruction in a fluvial channelmatlab
code
channel
first-order magnitude estimations
topographic input data
average flow velocity
channel bed slope
paleo-hydrological flood flow
flood flow reconstruction
maximum flow height
maximum average flow
peak discharge
code for paleo-hydrological
first-order magnitude
input data
bed slope
paleo-hydrological flood
magnitude estimations
paleo-hydrology
terrestrial hydrology
boulders
flash floods
sediment transport
channel morphology
manningseq-bouldersforpaleohydrology
MarshMorpho2D2D long-term marsh evolution model based on tidal dispersionlong-term
dispersion
10-10000 time scale
time scale
simulate marsh evolution
marsh evolution
evolution at 10-10000
10-10000 time
marshmorpho2d
MarshPondModel2D marsh evolution model focused on pond dynamicsmarsh
dynamics
marsh evolution model
marsh evolution
pond dynamics
evolution model focused
marshpondmodel
Meander Centerline Migration ModelSimulation of the long-term migration of meandering rivers flowing above heterogeneous floodplainssimulation
floodplains
long-term
migration
heterogeneous floodplain surfaces
point bars
floodplain surfaces
model simulates
simulates the long-term
long-term evolution
evolution of meandering
formation of oxbow
oxbow lakes
lakes and point
meandering rivers
heterogeneous floodplain
rivers above heterogeneous
surfaces
bars
river migration
meander
meander migration
river profile
meander center line
fluvial morphodynamics
meander centerline migration model
MeanderpyA simple kinematic model of meanderingmeandering
sufficient conditions
simulation approach
conditions for river
river meandering
simple numerical model
migration rate
python module
nominal migration rate
migration
numerical model
computing migration rate
sufficient
approach
rate
fluvial morphodynamics
meanderpy
Mixed bedrock-alluvial morphodynamicAlluvial morphodynamics of bedrock reachesalluvial
reaches
developed to simulate
simulate the sediment
sediment transport
alluvial morphodynamics
alluvial reaches
alluvial cover fraction
bedrock reaches
transport and alluvial
model
model is developed
morphodynamics of bedrock
alluvial cover
bedrock
mixed bedrock-alluvial morphodynamic
MocsyRoutines to model the ocean carbonate systemroutines
system
ocean carbonate system
carbonate system
ocean carbonate
ocean carbon models
carbonate system variables
ocean
carbonate
routines to model
mocsy
ocean carbon
fortran
dissolved inorganic carbon
input dissolved inorganic
carbon models
ModelParameterDictionaryTool written in Python for reading model input parameters from a simple formatted text file.python
tool
file
param
model parameter dictionary
simple formatted input
access model parameters
dict.read
number
tool for numerical
numerical modelers
modelers to easily
simple formatted
key
model parameters
access model
parameters
fruit
input parameters
read in
modelparameterdictionary
MripMrip is a self-organization type model for the formation and dynamics of megaripples in the nearshore.mrip
nearshore
self-organization
type
mrip consists
sea floor
representing the sea
matrix representing
users choice
floor
time
matrix
rules or equations
consists
representing
sea
transport rules
flow
bedform evolution
NEXRAD-extractExtract data from NEXRAD Doppler Radar NetCDFsnexrad
doppler
radar
extract
national weather service
doppler weather radar
weather radar network
doppler weather
weather service
radar network operated
national weather
python tool
weather radar
tool for extracting
plotting data
radar network
network operated
weather
hydrological
nexrad-extract
NUBBLEA turbulent boundary layer model for the linearized shallow water equationsequations
time-stepping point model
linear finite elements
surface forcing
time-stepping point
point model
linear finite
finite elements
elements to determine
determine the vertical
vertical structure
horizontal components
components of velocity
velocity and density
mellor and yamada
closure scheme
nubble
NWM Data ComponentA CSDMS data component used to download the National Water Model datasets.csdms
national
water
model
national water model
time series datasets
national water
basic model interface
nwm package
water model
time series
model grid
set of functions
river reach
csdms modeling framework
model interface
nwm
series datasets
basic model
nwm data component
NearCoMNearshore Community Modelmodel
community
nearshore
nearcom predicts waves
nearcom predicts
nearshore ocean
water depth
bathymetric change
sediment transport
sediment transport module
predicts waves
currents
handling data input
transport and bathymetric
nearcom
ocean
depth
sediment
flow dynamics
Nitrate Network ModelNitrate and organic carbon dynamics on a wetland-river networknitrate
network
network-based modeling framework
water resources research
network-based modeling
modeling framework
organic carbon
water resources
resources research
wetland-river network
assess nitrate removal
framework of czuba
inform watershed management
contextualizing wetlands
czuba
foufoula-georgiou as applied
river network
wetland
denitrification
nitrate network model
applied to nitrate
Non Local Means FilteringPerforms non-local means filtering of a DEM following Buades et al. (2005)dem
buades
dem by finding
smoothes noise
neighbouring cells
central cell
smoothes
cells and assigning
topographic analysis
non local means filtering
NormalFaultNormalFault implements relative rock motion due to a normal fault.normalfault
fault
trace input parameter
input parameter
arbitrary trace
trace input
trace
parameter
points
rows and columns
arbitrary
input
scarp
uplift
OGGMOGGM is a modular open source model for glacier dynamicsoggm
dynamics
including contributory branches
ice dynamics module
explicit ice dynamics
including contributory
contributory branches
dynamics module
model accounts
includes an explicit
explicit ice
ice dynamics
glacier geometry
accounts for glacier
including
branches
module
glacier flow
glacier
glacier dynamics
OTEQOne-Dimensional Transport with Equilibrium Chemistry (OTEQ): A Reactive Transport Model for Streams and Riversoteq
chemistry
equilibrium
transport
reactive transport model
solute transport model
transport model
model
chemical equilibrium
reactive transport
chemical
solutes
one-dimensional transport
solute transport
reactions
oteq equilibrium approach
biogeochemistry
water quality
OTISOne-Dimensional Transport with Inflow and Storage (OTIS): A Solute Transport Model for Streams and Riversotis
storage
rivers
transport
streams and rivers
mathematical simulation model
solute transport model
rivers otis
simulation model
mathematical simulation
characterize the fate
streams
one-dimensional transport
transient storage
solute transport
transport model
model
biogeochemistry
water quality
OTTEREvolution of a river profile with dynamic widthevolution
width
technique in transient
transient evolution
optimization technique
evolution of rivers
otter
channel
technique
transient
channel width
river profile
shear stress
slightly
shear
OceanWavesCalculate wave-generated bottom orbital velocities from surface wave parameterscalculate
parameters
calculate wave-generated bottom
bottom orbital velocities
surface wave parameters
wave-generated bottom orbital
measured surface wave
calculate wave-generated
bottom orbital
orbital velocities
wave parameters
surface wave
surface wave spectra
wave-generated bottom
measured surface
orbital
velocities from measured
wave model
wind wave estimation
oceanwaves
OlaFlowWave generation and active absorption interaction with porous structures frameworkwave
framework
numerical model conceived
numerical model
model conceived
work in ihfoam
ihfoam
olafoam
continuous from ihfoam
olaflow
jul
feb
mar
nov
numerical
model
conceived
openfoam
wave current interaction
breakwaters
OpenFOAMOpen Field Operation and Manipulation is a toolbox for the development of customized numerical solvers.field
operation
manipulation
open
open field operation
customized numerical solvers
continuum mechanics problems
including computational fluid
computational fluid dynamics
open field
operation and manipulation
field operation
numerical solvers
post-processing utilities
mechanics problems
including computational
fluid dynamics
development of customized
customized numerical
toolbox
continuum mechanics
openfoam
OptimalCycleIDA numerical method to analyse a vertical succession of strata and identify the most cyclical arrangement of constituent faciesfacies
numerical
method
analyse
probability matrix approach
optimised transition probability
transition probability matrix
matrix approach
numerical method
method to analyse
analyse a vertical
vertical succession
succession of strata
strata and identify
cyclical arrangement
arrangement of constituent
constituent facies
optimised transition
transition probability
cyclicity
strata
markov
optimalcycleid
OrderIDA method to test for order in a vertical succession of stratastrata
method
test
order
thickness and facies
facies data
vertical succession
presence of order
succession of strata
strata and tests
orderid
thickness
facies
data
vertical
succession
tests
sequence stratigraphy
OverlandFlowComponent simulating overland flow using a 2-D numerical approximation of the shallow-water equations following the de Almeida et al., 2012 algorithm for storage-cell inundation modeling.almeida
component
numerical
algorithm
simplified inertial approximation
landlab overlandflow component
shallow water equations
landlab overlandflow
simplified inertial
inertial approximation
water equations
shallow water
overlandflow component
landlab
equations
component is based
overlandflow
based
OverlandFlowBatesThis component simulates overland flow using the 2-D numerical model of shallow-water flow over topography using the Bates et al. (2010) algorithm for storage-cell inundation modeling.bates
numerical
flow
overland flow
simulate overland flow
overland
flood
shallow water
overlandflowbates
PHREEQCPHREEQC version 3 is a computer program written in the C and C++ programming languages that is designed to perform a wide variety of aqueous geochemical calculationsphreeqc
version
programming
calculations
lawrence livermore national
livermore national laboratory
specific ion interaction
ion interaction theory
national laboratory model
ion-association aqueous models
interaction theory
lawrence livermore
livermore national
national laboratory
specific ion
ion interaction
aqueous models
laboratory model
phreeqc implements
geochemical reaction model
inverse modeling
saturation indices
contaminant migration
PIHMPIHM is a multiprocess, multi-scale hydrologic model.pihm
multiprocess
multi-scale
model
finite volume method
major hydrological processes
semi-discrete finite volume
multi-scale hydrologic model
multi-scale hydrologic
volume method
major hydrological
hydrological processes
processes are fully
fully coupled
semi-discrete finite
finite volume
hydrologic model
gis interface
basins
continental
PIHMgisTightly coupled GIS interface for the Penn State Integrated Hydrologic Modelmodel
gis
penn
state
physically-based fully-distributed hydrologic
simulate hydrologic state
hydrologic state variables
topography and hydrogeology
fully-distributed hydrologic models
physically-based fully-distributed
heterogeneity in climate
state variables
variables in space
space and time
information regarding heterogeneity
hydrologic model requires
fully-distributed hydrologic
simulate hydrologic
hydrologic state
basins
pihmgis
PISMParallel Ice Sheet Model, PISMpism
model
ice
sheet
hybrid shallow ice
shallow shelf model
shelf model
hybrid shallow
shallow shelf
computing research community
increasing problem size
scalable software libraries
high-performance computing research
pism is designed
shallow
flow
simulate ice flow
shallow ice
ice flow
ice sheet
ice sheet model
PRMSPrecipitation-Runoff Modeling Systemsystem
modeling
precipitation-runoff
general basin hydrology
modular-design modeling system
sediment yields
combinations of precipitation
surface-water runoff
basin hydrology
modular-design modeling
modeling system
developed to evaluate
evaluate the impacts
general basin
climate
prms
precipitation
runoff
hydrological model
basin
PSTSWMParallel Spectral Transform Shallow Water Modelmodel
spectral
transform
shallow
spectral transform method
message-passing benchmark code
parallel algorithm testbed
nonlinear shallow water
shallow water equations
transform method
message-passing benchmark
benchmark code
algorithm testbed
testbed that solves
solves the nonlinear
rotating sphere
spectral transform
shallow water
shallow water test
pstswm
ParFlowParallel, high-performance, integrated watershed modelparallel
high-performance
integrated
model
parallel watershed flow
watershed flow model
parallel watershed
flow model
watershed flow
fully-integrated overland flow
simulate complex topography
ncar code wrf
includes fully-integrated overland
land-surface processes including
parflow
coupled land-surface processes
object-oriented
overland flow
biogeochemistry and snow
basins
Permafrost Benchmark SystemThe PBS is a web-based tool for conducting benchmarking studies of permafrost models.pbs
models
permafrost benchmark system
csdms web modeling
web modeling tool
ilamb benchmarking system
command-line ilamb benchmarking
permafrost benchmark
modeling tool
benchmark system
benchmark datasets
csdms web
web modeling
benchmarking system
adds tools
wraps the command-line
model outputs
cmip5
wmt
permafrost
data
benchmark
PerronNLDiffuseNonlinear diffusion, following Perron (2011).perron
nonlinear
diffusion
taylor perron
nonlinear hillslope diffusion
hillslope diffusion equation
perron ’s implicit
module uses taylor
method to solve
single timestep
solve the nonlinear
nonlinear hillslope
hillslope diffusion
diffusion equation
regular grid
taylor
implicit
hillslope
soil
soil creep
perronnldiffuse
Pllcart3d3D numerical simulation of confined miscible flowsnumerical
flows
miscible hele-shaw flows
flows using dns
dns of incompressible
nonlinear three dimensional
transport equations
dimensional simulations
simulations of miscible
miscible hele-shaw
hele-shaw flows
incompressible navier-stokes
navier-stokes and transport
dns
nonlinear
equations
dimensional
micible hele-shaw flow
pllcart3d
PlumeHypopycnal sediment plumehypopycnal
plume
hypopycnal sediment plume
run a hypopycnal
sediment plume
hypopycnal sediment
run
sediment transport
Point-Tidal-flatPoint Model for Tidal Flat Evolution modelmodel
tidal
flat
evolution
stochastic point model
tidal flat equilibrium
tidal flat evolution
flat equilibrium
tidal flat
stochastic point
point model
evolution to study
study the influence
currents and wind
wind waves
flat evolution
tidal currents
point-tidal-flat
PotentialEvapotranspirationCalculates potential evapotranspirationcalculates
evapotranspiration
potential evapotranspiration component
evapotranspiration component calculates
component calculates spatially
distributed potential evapotranspiration
potential evapotranspiration based
priestley taylor
spatially distributed potential
evapotranspiration component
potential evapotranspiration
calculates spatially distributed
component calculates
constant or priestley
input radiation factor
evapotranspiration based
spatial distribution
potentialevapotranspiration
PotentialityFlowRouterMultidirectional flow routing using a novel method.multidirectional
method
class implements voller
experimental matrix solutions
implements voller
paola ’s experimental
class implements
experimental matrix
matrix solutions
hobley
voller
paola
flow
chezy or manning
routing
manning equations
class
flow path
flow routing
potentialityflowrouter
PrecipitationDistributionGenerate random sequence of precipitation eventsgenerate
events
water resources research
rectangular poisson pulse
poisson pulse model
water resources
resources research
generates precipitation events
rectangular poisson
poisson pulse
landlab component
component that generates
generates precipitation
precipitation events
pulse model
eagleson
water
precipitation
precipitationdistribution
Princeton Ocean Model (POM)POM: Sigma coordinate coastal & basin circulation modelpom
sigma
coastal
basin
princeton ocean model
powerful ocean modeling
ocean modeling code
shelf and slope
princeton ocean
wide-range of problems
circulation and mixing
processes in rivers
semi-enclosed seas
modeling code
simulate a wide-range
mixing processes
seas and open
open and global
ocean model
physical oceanography
princeton ocean model (pom)
PsHICPixel-scale Hypsometric Integral Calculatorcalculator
hypsometric
integral
pixel-scale
calculate the hypsometric
hypsometric integral
calculate
catchment
pixel
contributing area
considered a local
local outlet
geomorphologic
pshic
PyDeltaRCMReduced complexity river delta formation and evolution model with channel dynamicsreduced
dynamics
csdms model repository
man liang
python version
csdms model
model repository
liang
python
man
csdms
wmt component
deltarcm
model
sediment transport model
sediment transport
version
delta evolution
cellular automata
coastal morphodynamics
pydeltarcm
PyRiverBedA Python framework to generate synthetic riverbed topography of constant-width meandering riverspython
rivers
placeholder
meandering rivers
riverbed
pyriverbed
QTCMQuasi-equilibrium Tropical Circulation Modelmodel
tropical
circulation
quasi-equilibrium
intermediate complexity suitable
intermediate complexity
complexity suitable
modeling of tropical
tropical climate
models
general circulation models
complex general circulation
qtcms
variability
climate models
climate
qtcms are models
intermediate
complexity
qtcm
QUAL2KA Modeling Framework for Simulating River and Stream Water Qualityquality
modeling
framework
simulating
brown and barnwell
river and stream
intended to represent
represent a modernized
modernized version
brown
barnwell
model
water quality model
diurnal
diurnal time scale
quality model
stream water quality
stream water
simulated
biogeochemistry
water quality
qual2k
QUODDYA state-of-the-art finite-element computer simulation program for coastal ocean circulation modelingfinite-element
modeling
incorporates advanced turbulence
advanced turbulence closure
free surface
incorporates advanced
turbulence closure
tidal time
model is three-dimensional
three-dimensional and fully
fully nonlinear
advanced turbulence
operates in tidal
structured linear elements
surface
incorporates
closure
coastal circulation
quoddy
RAFEMRiver Avulsion and Floodplain Evolution Modulemodule
avulsion
floodplain
evolution
morphodynamic river avulsion
river avulsion model
coupled with cem
morphodynamic river
avulsion model
river avulsion
cem
morphodynamic
model
designed
rafem
REF-DIFPhase-resolving parabolic refraction-diffraction model for ocean surface wave propagation.phase-resolving
propagation
phase-resolving parabolic refraction-diffraction
surface wave propagation
parabolic refraction-diffraction model
ocean surface wave
tony dalrymple starting
phase-resolving parabolic
parabolic refraction-diffraction
ocean surface
tony dalrymple
ref
dif
jim kirby
wave propagation
kirby
wave dynamics
ref-dif
RHESSysRegional Hydro-Ecologic Simulation Systemsystem
simulation
regional
hydro-ecological modelling framework
modelling framework designed
simulate carbon
nutrient fluxes
framework designed
designed to simulate
hydro-ecological modelling
modelling framework
rhessys is capable
rhessys
water
physically-based process models
gis-based
hydro-ecological
carbon
biogeochemistry
water quality
c-cycle
nutrient cycle
ROMSRegional Ocean Modeling Systemsystem
ocean
modeling
regional
primitive equations ocean
orthogonal curvilinear
equations ocean model
primitive equations
equations ocean
representer tangent linear
tangent linear
roms
free-surface
terrain-following
ocean model
linear
orthogonal
curvilinear
primitive
flow dynamics
wave dynamics
physical oceanography
RadiationCompute 1D and 2D total incident shortwave radiation.compute
total
radiation
total incident shortwave
landlab component
total incident
incident shortwave radiation
shortwave radiation
incident shortwave
shortwave radiation compared
landlab
shortwave
solar radiation
RecircFeedE-book: calculator for approach to equilibrium in recirculating and feed flumese-book
calculator
flumes
mobile-bed normal equilibrium
studying the approach
approach to mobile-bed
mobile-bed normal
normal equilibrium
equilibrium in recirculating
recirculating and sediment-feed
implements a calculation
uniform sediment
sediment-feed flumes
sediment
sediment feed
water and sediment
implements
recirc
bed equilibrium
fluvial morphodynamics
recircfeed
Rescal-snowA model of dunes and snow-wavessnow-waves
snow
wind blows
study snow features
forms surface features
features
rescal-snow
snow features
enable snow scientists
surface features
self-organizes
snow science
blows
data
ripples and dunes
loose grains rescal-snow
snow dynamics
sand
aeolian sediment transport
dune
aeolian dune
ReservoirReservoir: Tools for Analysis, Design, and Operation of Water Supply Storagesdesign
reservoir
tools
analysis
determine no-fail rippl
evaluate inflow characteristics
no-fail rippl storage
measure single reservoir
sequent peak analysis
optimize release decisions
stochastic dynamic programming
single reservoir performance
no-fail rippl
rippl storage
measure single
performance using resilience
vulnerability metrics
determine no-fail
peak analysis
water storage yield
RivMAPMatlab toolbox for mapping and measuring river planform changesmatlab
changing river planforms
analyze changing river
aerial views
analyze changing
river planforms
changing river
centerline
areas
river
planforms
aerial
views
compute
channel
cutoff
planform change
meander migration
river migration
width
spacetime mapping
rivmap
River Erosion ModelAn intermediate complexity model for simulating stream channel evolution (years to decades) at the watershed scale.evolution
years
decades
scale
channel bed aggradation
rem mechanistically simulates
mechanistically simulates channel
simulates channel bed
bed aggradation
rem mechanistically
river networks
simulate channel change
mechanistically simulates
monte carlo simulations
channel bed
channel widening
running monte carlo
rem
simulates channel
river erosion model
River Network Bed-Material SedimentBed-material sediment transport and storage dynamics on river networks.bed-material
networks
water resources research
resources research
water resources
czuba
doi
gravel bed dynamics
sediment
earth surface
research
earth surface processes
bed-material sediment transport
geophysical research
sediment transport
foufoula-georgiou
bed dynamics
river network
river network bed-material sediment
River Temperature ModelRiver Temperature Model based on heat balance approachtemperature
model
river
approach
applied in arctic
water temperature model
river water temperature
arctic rivers
water temperature
arctic
temperature model
river water
heat
net solar radiation
net longwave radiation
radiation
designed
include surface net
permafrost
river discharge
river temperature model
RiverMUSESimulates freshwater mussel populations' response to changes in suspended sedimentsimulates
sediment
mussel population density
suspended sediment
modulates suspended sediment
population density
model simulates
mussel population
simulates the interaction
modulates suspended
chlorophyll-a
minnesota rivers
mussel population declines
suspended
model
mussel
mussels
matlab
chlorophyll
anthropogenic impact
rivermuse
RiverWFRisingBaseLevelNormalE-book: Calculator for disequilibrium aggradation of a sand-bed river in response to rising base level.e-book
calculator
level
steady-state aggradation
program steadystateag
program computes
program
downstream end
constant chezy resistance
grain size
computes
steady-state
aggradation
computes the steady-state
chezy resistance coefficient
size
base level
constant chezy
bed variation
fluvial morphodynamics
riverwfrisingbaselevelnormal
RouseVanoniEquilibriumE-book: Program for calculating the Rouse-Vanoni profile of suspended sediment.e-book
program
sediment
sediment profile calculator
equilibrium suspended sediment
suspended sediment profile
rouse-vanoni equilibrium suspended
profile calculator
equilibrium suspended
suspended sediment
sediment profile
rouse-vanoni equilibrium
calculator
equilibrium
suspended
profile
rouse-vanoni
fluvial morphodynamics
rousevanoniequilibrium
SBMSorted Bedform Modelmodel
bedform
sorted
sorted bedform model
sorted bedforms present
continental shelf environments
bedform model
sorted bedform
addresses the formation
shelf environments
bedforms present
sbm
formation mechanism
continental shelf
mechanism for sorted
addresses
sorted bed forms formation
SEASouthamption--East Angliasouthamption
east
anglia
pvm message passing
message passing library
primitive equation ocean
equation ocean general
ocean general circulation
general circulation model
circulation model based
give good performance
massively parallel machines
cox formulation
pvm message
passing library
primitive equation
equation ocean
ocean general
ocean circulation
sea
SELFESemi-implicit Eulerian–Lagrangian Finite Elementeulerian
lagrangian
element
finite
unstructured-grid model designed
baroclinic circulation
unstructured-grid model
model designed
effective simulation
shallow water equations
selfe
scales
semi-implicit finite-element eulerian-lagrangian
finite-element eulerian-lagrangian algorithm
baroclinic
water equations
written to realistically
ocean and river
river forcings
SETTLEPartical settling velocity solutionpartical
solution
dietrich equation
constant terminal settling
terminal settling velocity
size-density fraction median
fraction median size
size from dietrich
calculates the constant
constant terminal
terminal settling
settling velocity
size-density fraction
fraction median
median size
dietrich
calculates
setting velocity
turbulent fluid
fluvial
settle
SIBERIASIBERIA simulates the evolution of landscapes under the action of runoff and erosion over long times scales.siberia
scales
simulates
evolution
long times scales
siberia simulates
times scales
simulates the evolution
evolution of landscapes
action of runoff
runoff and erosion
erosion over long
long times
landscapes
action
landscape evolution
SICOPOLISIce sheet modelice
model
polythermal ice sheets
large ice sheets
greenland ice sheet
simulation code
thermodynamic model
ice sheets
code for polythermal
model that simulates
simulates the evolution
evolution of large
ice caps
polythermal ice
large ice
ice sheet
sicopolis
SIGNUMSIGNUM (Simple Integrated Geomorphological Numerical Model) is a MAtlab TIN-based landscape evolution modelsignum
model
simple
integrated
tin-based landscape evolution
landscape evolution model
geomorphological numerical model
integrated geomorphological numerical
simple integrated geomorphological
simulating sediment transport
multi-process numerical model
numerical model written
integrated numerical framework
numerical model
time scales
sediment transport
transport and erosion
erosion by river
river flow
SLAMM 6.7The Sea Level Affecting Marshes Model (SLAMM)slamm
model
sea
level
affecting marshes model
sea level rise
sea level affecting
level affecting marshes
dominant processes involved
long-term sea level
level rise
sea level
marshes model
level affecting
affecting marshes
simulates the dominant
accelerated sea level
dominant processes
processes involved
slamm 6.7
SLEPIAN AlphaComputation of spherical harmonics, Slepian functions, and transformsslepian
computation
harmonics
functions
doi
routines pertaining
paper published
routines
toolbox
slepian alpha
SLEPIAN BravoLinear inverse problems using spherical harmonics and spherical Slepian functionsslepian
linear
functions
spherical
doi
routines pertaining
paper published
routines
toolbox
slepian bravo
SLEPIAN CharlieSpectral estimation problems using spherical harmonics and spherical Slepian functionsslepian
spectral
functions
spherical
doi
routines pertaining
paper published
routines
toolbox
slepian charlie
SLEPIAN DeltaAnalysis of time-variable gravity from the GRACE satellite mission using spherical harmonics and spherical Slepian functionsgrace
slepian
analysis
functions
doi
routines pertaining
paper published
routines
toolbox
slepian delta
SLEPIAN EchoComputation of vectorial spherical harmonics, vectorial Slepian functions, and transformsslepian
computation
harmonics
functions
doi
routines pertaining
paper published
routines
toolbox
slepian echo
SNACAn updated Lagrangian explicit finite difference code for modeling a finitely deforming elasto-visco-plastic solid in 3D.lagrangian
deforming
solid
heat energy balance
energy balance equations
solid with complicated
complicated rheology
solve momentum
momentum and heat
heat energy
energy balance
balance equations
snac
snac can solve
rheology
snac makes
SNOWPACKSNOWPACK is a multi-purpose snow and land-surface model, which focuses on a detailed description of the mass and energy exchange between the snow, the atmosphere and optionally with the vegetation cover and the soil. It also includes a detailed treatment of mass and energy fluxes within these media.snowpack
snow
detailed
mass
properties including weak
weak layer characterization
including weak layer
snow properties including
snowpack has originally
support avalanche warning
originally been developed
developed to support
detailed description
properties including
including weak
water transport
layer characterization
weak layer
avalanche warning
SPACELandlab component for 2-D calculation of fluvial sediment transport and bedrock erosionlandlab
calculation
erosion
stream power
conservation and entrainment
simultaneously conserving mass
power with alluvium
alluvium conservation
landlab space
enables modeling
water column
bedrock-alluvial rivers
rivers by simultaneously
simultaneously conserving
conserving mass
geoscientific model development
alluvial bed
stream
river erosion
sediment transport
bedrock erosion
landscape evolution
space
SPARROWThe SPARROW Surface Water-Quality Modelmodel
sparrow
surface
spatially referenced regressions
relating water-quality measurements
water-quality measurements made
watershed modeling technique
spatially referenced
referenced regressions
monitoring stations
modeling technique
technique for relating
relating water-quality
water-quality measurements
measurements made
nonlinear regression equation
regression equation describing
watershed attributes
biogeochemistry
water quality
SPHYSICSSmoothed Particle Hydrodynamics codeparticle
hydrodynamics
smoothed
code
smoothed particle hydrodynamics
violent free-surface hydrodynamics
smoothed particle
particle hydrodynamics
potentially violent free-surface
free-surface hydrodynamics
sph
written in fortran
simulation of potentially
potentially violent
violent free-surface
code written
sphysics
STORMWindfield simulator for a cyclonewindfield
cyclone
storm computes windfield
storm computes
computes windfield
storm
wave dynamics
STSWMNCAR Spectral Transform Shallow Water Modelncar
model
spectral
transform
shallow water equations
shallow water
spherical geometry
water equations
numerical solution
evaluating numerical methods
general circulation models
equations in spherical
shallow
water
atmospheric general circulation
model is related
geometry
equations
circulation models
stswm
STVENANT1D gradually varied flow routinegradually
routine
gradually varied flow
predicts
unsteady
nonlinear
gradually varied
varied flow
flow
reaches
stvenant
STWAVESteady-State Spectral Wave Modelmodel
spectral
wave
steady-state
steady state spectral
state spectral wave
nearshore wind-wave growth
steady state
state spectral
stwave simulates depth-induced
half-plane model
parametric wave growth
model for nearshore
nearshore wind-wave
steepness-induced wave breaking
growing wave field
wind-wave growth
depth-induced wave refraction
spectral wave
wave dynamics
stwave
SUSPSuspended load transport subroutinesuspended
subroutine
calculates non-equilibrium suspended
non-equilibrium suspended load
suspended load transport
load transport rates
calculates non-equilibrium
non-equilibrium suspended
suspended load
load transport
transport rates
size-density fractions
calculates
bed
fluvial morphodynamics
susp
SVELAShear velocity solution associated with grain roughnessshear
roughness
calculates shear velocity
calculates shear
grain roughness
shear velocity
calculates
sediment transport
fluvial
svela
SWANSWAN is a third-generation wave modelswan
model
short-crested wind-generated waves
third-generation wave model
computes random
short-crested wind-generated
inland waters
model that computes
coastal regions
regions and inland
third-generation wave
wave model
wind-generated waves
waves in coastal
random
short-crested
wave dynamics
SWATSWAT is a river basin scale model developed to quantify the impact of land management practices in large, complex watersheds.swat
large
complex
watersheds
water assessment tool
agricultural research service
usda agricultural research
assessment tool
research service
jeff arnold
scale model developed
water assessment
usda agricultural
agricultural research
river basin
scale model
ars
tool
service
biogeochemistry
water quality
SWEHRA coupled model for infiltration, fluid flow, and sediment transport.infiltration
fluid
flow
transport
hairsine-rose soil erosion
shallow water equations
green-ampt infiltration model
soil erosion model
couples the shallow
shallow water
green-ampt infiltration
hairsine-rose soil
soil erosion
water equations
model couples
infiltration model
erosion model
high sediment concentrations
model
swehr
SWMMStorm Water Management Modelmodel
water
management
storm
epa storm water
storm water management
water management model
epa storm
management model
rainfall-runoff simulation model
primarily urban areas
dynamic rainfall-runoff simulation
storm water
water management
event or long-term
dynamic rainfall-runoff
single event
primarily urban
simulation model
reaches
swmm
Sakura3 Equation hyperpycnal flow modelequation
model
hyperpycnal flow model
hyperpycnal flow
flow model
hyperpycnal
sediment transport
sakura
SedBergAn iceberg drift and melt model, developed to simulate sedimentation in high-latitude glaciated fjords.model
developed
fjords
utilizing monte carlo
monte carlo based
icebergs utilizing monte
carlo based techniques
underlying parametric probability
parametric probability distributions
monte carlo
utilizing monte
carlo based
population of icebergs
icebergs utilizing
behavior of iceberg
model simulates
based techniques
number of underlying
sediment transport
sedberg
SedDepEroderCompute fluvial erosion using using “tools and cover” theorytheory
compute
tools
cover
volumetric sediment flux
volumetric sediment transport
stream power-like term
bed erosion rate
implements sediment flux
sediment flux dependent
module implements sediment
sediment transport capacity
flux dependent channel
dependent channel incision
volumetric sediment
sediment flux
power-like term
optional threshold
erosion rate
stream power
erosion
tools and cover
seddeperoder
SedFoam-2.0A multi-dimensional Eulerian two-phase model for sediment transport (version 2.0)version
eulerian
transport
three-dimensional two-phase flow
three-dimensional two-phase
two-phase flow solver
sediment transport
sediment
two-phase flow
flow
solver
models
turbulence models
sediment transport applications
stress
inter-granular stress
turbulent sediment transport
two-phase model
openfoam
multi-dimensional
sedfoam-2.0
SedfluxBasin filling stratigraphic modelbasin
model
sedflux basin-filling model
sedflux basin-filling
newest version
sedflux
basin-filling model
sediment transport
geodynamics
stratigraphy
Sedtrans05Sediment transport model for continental shelf and estuariessediment
estuaries
shelf and estuaries
continental shelf
sediment transport
transport
sediment transport model
single point model
function water depth
transport model
sedtrans05
SiStERAn easy-to-use MATLAB code to simulate long-term lithosphere and mantle deformation.matlab
deformation
simple stokes solver
simple stokes
exotic rheologies
non-linear rheologies
complex bcs
solver with exotic
simulates lithosphere
continuum mechanics
sharp contrasts
material properties
stokes solver
stokes flow
strain localization
lithosphere and mantle
mantle deformation
lithosphere deflection
sister
SinkFillerFill sinks in a landscape to the brim, following the Barnes et al. (2014) algorithms.barnes
fill
brim
algorithms
shallow gradient surfaces
algorithms to replace
continued draining
shallow gradient
gradient surfaces
replace pits
topography with flats
flats
draining
topography
initial topography
replace
optionally
depressions
flow routing
sinkfiller
SoilInfiltrationGreenAmptLandlab component that calculates soil infiltration based on the Green-Ampt solution.landlab
solution
surface water depths
updates surface water
time step
water depths
component calculates
calculates an infiltration
infiltration rate
model location
location and updates
updates surface
surface water
step
depths
form of julien
green-ampt method
soilinfiltrationgreenampt
SoilMoistureCompute the decay of soil moisture saturation at storm-interstorm time periodcompute
period
live leaf area
leaf area index
simulates root-zone average
root-zone average soil
average soil moisture
soil moisture
live leaf
area index
vegetation cover
simulates root-zone
root-zone average
leaf area
soil
landlab component
average soil
evapotranspiration
soilmoisture
SpatialPrecipitationDistributionGenerate random sequence of spatially-resolved precipitation eventsgenerate
events
env res lett
env res
res lett
lightly modified version
spatially resolved storms
component
year
generate a sequence
sequence of spatially
spatially resolved
total
limit
geosci
env
lett
precipitation
stochastic precipitation
spatialprecipitationdistribution
SpeciesEvolverEvolve life in a landscape.evolve
landscape
biotic and abiotic
dynamics at earth
earth
earth ’s surface
complex dynamics
abiotic processes
ecology
evolution
speciesevolver
Spirals1DRead note in extended description. 1D model of spiral troughs on Marscode is inactive
module code
inactive
spiral trough
mars
spirals1d
SteadyStateAgE-book: calculator for approach to equilibrium in recirculating and feed flumese-book
calculator
flumes
sea level rise
outlined in chapter
constant rate
program implements
implements the calculation
calculation for steady-state
steady-state aggradation
sand-bed river
river in response
response to sea
sea level
level rise
chapter
rate
bed variation
fluvial morphodynamics
steadystateag
SteepnessFinderCalculate steepness and concavity indices from gridded topographycalculate
topography
sensu wobus
calculates steepness indices
component calculates steepness
steepness indices
wobus
component calculates
calculates steepness
concavity
terrain analysis
steepness
steepnessfinder
StreamPowerRead note in extended description. Modeling the development of topographic steady state in the stream-power modelread
description
code is inactive
module code
inactive
bedrock channel erosion
topographic steady state
streampower
StreamPowerSmoothThresholdEroderCompute fluvial erosion using stream power theory with a numerically smoothed thresholdcompute
threshold
derived from fastscapeeroder
defines the streampowersmooththresholderoder
defines
stream
power
threshold.py
fastscapeeroder
smooth threshold formulation
stream power
erosion
streampowersmooththresholderoder
SubsideFlexure modelflexure
model
flexure model
basin uplift or subside
subside
SubsidingFanE-book: calculator for evolution of profiles of fans in subsiding basinse-book
calculator
basins
evolution
undergoing piston-style subsidence
sediment deposition
calculation of sediment
fan-shaped basin
piston-style subsidence
undergoing piston-style
basin
subsidence
sediment
deposition
calculation
undergoing
geodynamics
subside
fluvial morphodynamics
subsidingfan
SurfaceRoughnessQuantifies surface roughness with high-resolution topographic data by analyzing the local variability of surface normal vectors.quantifies
vectors
surface
roughness
surface roughness
map out areas
areas of hillslopes
emergence of bedrock
bedrock drives
drives an increase
increase in surface
float format
dem in float
input dem
tool requires
output the rasters
tool
float
rock exposure
lidar
surfaceroughness
SuspSedDensityStratE-book: Module for calculating the effect of density stratification on the vertical profiles of velocity and suspended sediment.e-book
module
sediment
calculating
density stratification effects
open channels
density stratification
calculation of density
stratification effects
suspended sediment
suspended sediment concentration
channels
density
stratification
open
sediment in open
suspended
sediment concentration profiles
fluvial morphodynamics
suspseddensitystrat
Symphonie3D primitive equation ocean modelprimitive
model
coastal ocean model
three-dimensional primitive equations
primitive equations coastal
equations coastal ocean
ocean model
symphonie
three-dimensional primitive
primitive equations
equations coastal
coastal ocean
physical oceanography
TAotAo is a software designed to model the interplay between lithosphere flexure and surface transport (erosion/sedimentation), particularly during the formation of orogens and foreland sedimentary basins (see details).erosion
sedimentation
tao
transport
model permits calculating
numerical model permits
independent variable
numerical model
permits calculating
lithospheric flexure
combination with faulting
model permits
cross-section
loading
deposition
linux platforms
gmt scripts
standard pcs match
produced using gmt
geodynamics
TISCTISC integrates quantitative models of lithospheric flexure, fault deformation, and surface mass transport (erosion/transport/sedimentation) along drainage networks.erosion
sedimentation
tisc
transport
geological time scales
large-scale sediment transport
time scales
computer program
program that simulates
simulates the evolution
geological time
sediment transport
surface transport
river sediment transport
large-scale sediment
tectonic
network
fluvial morphodynamics
geodynamics
bedrock erosion
groundwater
isostasy
orographic precipitattion
evaporation
lake
TOPMODELPhysically based, distributed watershed model that simulates hydrologic fluxes of water through a watershedphysically
based
distributed
watershed
infiltration-excess overland flow
saturation overland flow
distributed watershed model
overland flow
simulates hydrologic fluxes
subsurface flow
physically based
channel routing
distributed watershed
infiltration-excess overland
saturation overland
produce saturation overland
hydrologic fluxes
flow
model simulates explicit
basin
hydrological
topmodel
TOPOGTOPOG is a terrain analysis-based hydrologic modelling packagetopog
package
land surface
atmosphere via evaporation
groundwater and back
water moves
topog describes
conservative solute movement
moves through landscapes
landscapes
soil
three-dimensional landscapes
surface
evaporation
describes
moves
landscape
catchment
TURBGausian distribution calculator of instantaneous shear stresses on the fluvial bedgausian
bed
instantaneous shear stresses
calculates the gaussian
coefficient of variation
gaussian or log-gaussian
log-gaussian distribution
distribution of instantaneous
instantaneous shear
shear stresses
calculates
variation
gaussian
log-gaussian
distribution
instantaneous
bedload transport
fluvial
turb
TURBINSAn immersed boundary, Navier–Stokes code for the simulation of gravity and turbidity currents interacting with complex topographies.navier
stokes
boundary
topographies
modular code written
highly parallel modular
parallel modular code
turbidity currents interacting
modular code
code written
capable of modeling
modeling gravity
turbidity currents
complex topographies
pressure poisson equation
highly parallel
parallel modular
currents interacting
turbins
turbidity current
numerical simulation
complex topography
polydisperse suspension
sedimentation
parallel computing
TauDEMA suite of Digital Elevation Model (DEM) tools for the extraction and analysis of hydrologic information from topography as represented by a DEM. TauDEM 5 is a new version implemented to take advantage of parallel processingdem
model
digital
elevation
graphical user interface
argonne national laboratory
toolbox graphical user
calculates flow paths
command line executable
calculates contributing area
delineation threshold based
standalone command line
terrain analysis details
arcgis toolbox graphical
line executable programs
multiple flow direction
channel network delineation
network delineation threshold
variable drainage density
hydrologivally corrected dem
watershed
taudem
TaylorNonLinearDiffuserModel non-linear soil creep after Ganti et al. (2012)ganti
taylor series expansion
taylor series
hillslope flux derived
nonlinear hillslope flux
series expansion
hillslope evolution
nonlinear hillslope
andrews-bucknam formulation
formulation of nonlinear
hillslope flux
flux derived
taylor
series
hillslope
diffusion
taylornonlineardiffuser
TerrainbentoA Python package for multi-model analysis in long-term drainage basin evolutionpython
evolution
python package
earth over geologic
geologic time
thousands to millions
millions of years
package for modeling
modeling the evolution
terrainbento
earth
established governing equation
time
thousands
years
TerrapinBuild and destroy strath and fill terracesbuild
terraces
destroy
strath
put into numerics
numerics
terrapin
terraces put
stands
terrace
fluvial
ThawLake1D1-D numerical model of permafrost and subsidence processes.numerical
processes
subsidence processes
numerical model
permafrost and subsidence
model of permafrost
model
subsurface thermal impact
warming climate
permafrost
subsidence
thermal
subsurface
thaw lake
talik
thawlake1d
The TELEMAC systema powerful integrated modeling tool for use in the field of free-surface flows.flows
powerful integrated modeling
integrated modeling tool
telemac system
free-surface flows
powerful integrated
integrated modeling
modeling tool
field of free-surface
high-capacity algorithms based
telemac
finite-element method
simulation modules
modules use high-capacity
high-capacity algorithms
hydrodynamics
coastal and marine
fluvial
groundwater
the telemac system
TopoFlowSpatially-distributed, D8-based hydrologic modelspatially-distributed
hydrologic
model
spatially-distributed hydrologic model
spatially-distributed hydrologic
interface
topoflow
powerful
user-friendly
hydrologic model
climatic forcings
hydrologic variables
basins
TopoFlow-Channels-Diffusive WaveDiffusive Wave process component for flow routing in a D8-based, spatial hydrologic modelwave
diffusive
spatial
model
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
hydrologic model
model called
stand-alone model
process component
component is part
spatially-distributed hydrologic
compute flow velocities
diffusive wave
river network
topoflow
basins
topoflow-channels-diffusive wave
TopoFlow-Channels-Dynamic WaveDynamic Wave process component for flow routing in a D8-based, spatial hydrologic modelwave
dynamic
spatial
model
spatially-distributed hydrologic model
hydrologic model called
model called topoflow
hydrologic model
model called
stand-alone model
process component
component is part
spatially-distributed hydrologic
wave method
dynamic wave method
called topoflow
method
diffusive wave method
basins
topoflow-channels-dynamic wave
TopoFlow-Channels-Kinematic WaveKinematic Wave process component for flow routing in a D8-based, spatial hydrologic model.wave
kinematic
spatial
model
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
hydrologic model
model called
stand-alone model
lighthill and whitham
process component
component is part
spatially-distributed hydrologic
method
topoflow
flow
basins
topoflow-channels-kinematic wave
TopoFlow-Data-HISThe CUAHSI Hydrologic Information Systemsystem
cuahsi
hydrologic
information
sharing hydrologic data
internet-based system
system for sharing
sharing hydrologic
hydrologic data
data
topoflow-data-his
TopoFlow-DiversionsDiversions component for a D8-based, spatial hydrologic model.diversions
spatial
model
spatially-distributed hydrologic model
hydrologic model called
model called topoflow
hydrologic model
model called
stand-alone model
component is part
spatially-distributed hydrologic
called topoflow
process component
topoflow
water
point
topoflow supports
basins
topoflow-diversions
TopoFlow-Evaporation-Energy BalanceEvaporation process component (Energy Balance method) for a D8-based, spatial hydrologic modelenergy
balance
evaporation
component
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-evaporation-energy balance
TopoFlow-Evaporation-Priestley TaylorEvaporation process component (Priestley-Taylor method) for a D8-based, spatial hydrologic modelevaporation
component
priestley-taylor
method
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-evaporation-priestley taylor
TopoFlow-Evaporation-Read FileEvaporation process component (read from file method) for a spatially-distributed hydrologic model.evaporation
component
read
method
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-evaporation-read file
TopoFlow-Infiltration-Green-AmptInfiltration process component (Green-Ampt method) for a D8-based, spatial hydrologic modelinfiltration
component
green-ampt
method
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-infiltration-green-ampt
TopoFlow-Infiltration-Richards 1DInfiltration process component (Richards 1D method) for a D8-based, spatial hydrologic modelrichards
method
infiltration
component
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-infiltration-richards 1d
TopoFlow-Infiltration-Smith-ParlangeInfiltration process component (Smith-Parlange method) for a D8-based, spatial hydrologic modelinfiltration
component
smith-parlange
method
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-infiltration-smith-parlange
TopoFlow-MeteorologyMeteorology process component for a D8-based, spatial hydrologic modelmeteorology
spatial
model
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
process
component
part
basins
topoflow-meteorology
TopoFlow-Saturated Zone-Darcy LayersSaturated Zone process component (Darcy's law, multiple soil layers) for a D8-based, spatial hydrologic modeldarcy
zone
saturated
component
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-saturated zone-darcy layers
TopoFlow-Snowmelt-Degree-DaySnowmelt process component (Degree-Day method) for a D8-based, spatial hydrologic modelsnowmelt
component
degree-day
method
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-snowmelt-degree-day
TopoFlow-Snowmelt-Energy BalanceSnowmelt process component (Energy Balance method) for a D8-based, spatial hydrologic modelenergy
balance
snowmelt
component
model called topoflow
spatially-distributed hydrologic model
hydrologic model called
called topoflow
process component
component is part
spatially-distributed hydrologic
hydrologic model
model called
stand-alone model
topoflow
model
process
part
basins
topoflow-snowmelt-energy balance
TopoToolboxA set of Matlab functions for topographic analysismatlab
analysis
digital elevation models
set of matlab
matlab functions
elevation models
analysis of relief
relief and flow
flow pathways
pathways in digital
digital elevation
support the analysis
efficient analytical gis
analytical gis utilities
functions that support
analytical gis
topographic analysis
geomorphology
geomorphometry
topotoolbox
TransportLengthHillslopeDiffuserTransport length hillslope diffusion.transport
diffusion
hillslope diffusion component
style of carretier
hillslope diffusion
diffusion component
davy and lague
carretier
hillslope
soil
transportlengthhillslopediffuser
TwoPhaseEulerSedFoamA four-way coupled two-phase Eulerian model for sediment transporteulerian
transport
sediment transport based
multi-dimensional numerical model
numerical model
sediment transport
two-phase flow formulation
transport based
model
model is developed
multi-dimensional numerical
two-phase flow
suspended load assumptions
numerical
developed
require conventional bedload
sediment
two-phase model
multi-dimensional
twophaseeulersedfoam
UEBThe Utah Energy Balance (UEB) Grid snowmelt modelueb
balance
grid
utah
david tarboton research
tarboton research group
utah energy balance
david tarboton
energy balance snowmelt
energy balance
snowmelt model developed
developed by david
tarboton research
balance snowmelt model
utah energy
research group
balance snowmelt
model
energy
snow dynamics
glacial melt
UMCESromsChesapeake Bay Application, special case of Regional Ocean Modeling System (ROMS)roms
application
system
bay
primitive equations ocean
orthogonal curvilinear
equations ocean model
primitive equations
equations ocean
representer tangent linear
tangent linear
free-surface
terrain-following
ocean model
linear
orthogonal
curvilinear
primitive
umcesroms
Underworld2Underworld2 is an open-source, particle-in-cell finite element code tuned for large-scale geodynamics simulations.open-source
finite
simulations
large-scale geodynamics simulations
element code tuned
finite element code
geodynamics simulations
code tuned
large-scale geodynamics
finite element
finite element mesh
element code
large-scale flow
fine-scale damage parameters
tuned for large-scale
fluid flow
large-scale
convecting medium
plate tectonics
lithospheric flexure
underworld2
VICVIC (Variable Infiltration Capacity) is a macroscale hydrologic model that solves full water and energy balances, originally developed by Xu Liang at the University of Washington.vic
variable
capacity
washington
grid cell
grid
semi-distributed hydrologic model
cell
grid cells
land surface
semi-distributed hydrologic
land
cells
surface
vic model
time
model
simulation
entire simulation
global
VegCALandlab component that simulates inter-species plant competition using a 2D cellular automata model.landlab
cellular
model
cellular automata tree
cellular automata
grass shrub simulator
automata tree grass
based on cellular
shrub simulator
automata tree
simulator
catgrass
automata
tree grass shrub
population ecology
species
competition
vegca
VegetationModel plant dynamics using multiple representative plant speciesmodel
species
plant
dynamics
net primary productivity
average soil moisture
simulates net primary
leaf area index
root-zone average soil
landlab component
primary productivity
biomass and leaf
soil moisture
component that simulates
simulates net
net primary
leaf area
area index
cell based
vegetation
plant dynamics
WACCM Dust-SulfurWhole atmosphere module of sulfate aerosols.aerosols
atmosphere module
module of sulfate
emphasis on stratospheric
sulfate aerosols
stratospheric aerosols
aerosols and dust
aerosols with emphasis
dust
atmosphere
module
sulfate
emphasis
stratospheric
waccm dust-sulfur
WACCM-CARMAatmospheric/aerosol microphysical modelatmospheric
aerosol
model
brian toon aerosol
ncar atmospheric high-altitude
waccm is ncar
carma is brian
toon aerosol microphysical
brian toon
atmospheric high-altitude model
microphysical sectional model
aerosol microphysical sectional
ncar atmospheric
toon aerosol
atmospheric high-altitude
microphysical sectional
high-altitude model
sectional model
microphysical
climate
waccm-carma
WACCM-EEGCM for deep paleoclimate studiesgcm
studies
ncar waccm model
ncar waccm
developing a gcm
gcm based
based on ncar
ancient earth
waccm model
studied the climate
earth
waccm
ncar
faint young sun
model to studied
titan-like photochemical hazes
paleoclimate
waccm-ee
WAVEREFWave refraction routinewave
routine
wave refraction program
refraction program
wave refraction
program
wave dynamics
waveref
WAVEWATCH III ^TMSpectral wind wave modelspectral
model
including shallow water
spectral wave model
shallow water physcis
generation random phase
random phase spectral
phase spectral wave
wave model
including shallow
water physcis
generation random
random phase
phase spectral
spectral wave
shallow water
physical oceanography
wavewatch iii ^tm
WBM-WTMWater Balance/Transport Modelbalance
transport
model
water
climate input forcings
water balance model
ground water recharge
gridded water balance
grid cell
surface and subsurface
subsurface runoff
balance model
model using climate
climate input
input forcings
forcings that calculate
water balance
ground water
water recharge
global
wbm-wtm
WBMsedGlobal sediment flux and water discharge model.global
model
wbm
wtm
psi models
bqart and psi
wbmplus
sediment flux
global model
hydrological model
wbmsed
WDUNEGUI implementation of the Werner (1995) cellular automata aeolian dune modelgui
werner
cellular
model
simple cellular automata
gui implementation
cellular automata dune
simple cellular
cellular automata
automata dune model
automata dune
proposed by werner
geology
aeolian dune
gis
geomorphologic
wdune
WILSIMLandscape evolution modellandscape
model
java applet
landform simulation model
web-based interactive landform
interactive landform simulation
cellular automata algorithm
tectonic uplift
change different parameters
user to change
evolve over time
simulation model
incorporating nonlinear rules
web-based interactive
cellular automata
interactive landform
landform simulation
landscape evolution
wilsim
WINDSEADeep water significant wave height and period simulator during a hurricane routinedeep
routine
deep water significant
water significant wave
significant wave height
subroutine computes
computes the deep
deep water
water significant
significant wave
wave height
height and period
hurricane
wave dynamics
windsea
WOFOSTWOFOST (WOrld FOod STudies) is a simulation model for the quantitative analysis of the growth and production of annual field crops.wofost
world
studies
crops
explains crop growth
underlying processes
mechanistic model
model that explains
influenced by environmental
environmental conditions
crop
processes are influenced
processes
yield gap atlas
global yield gap
european mars crop
explains crop
crop growth
crop production
biomass production
phenology
agromanagement
WPHydResAMBLE-book: Implementation of the Wright-Parker (2004) formulation for hydraulic resistance combined with the Ashida-Michiue (1972) bedload formulation.e-book
implementation
wright-parker
ashida-michiue
bedload calculator
bedload transport
flow resistance
stratification correction
wright-parker formulation
ashida-michiue formulation
formulation for flow
depth-discharge and bedload
calculator
formulation for bedload
bedload
formulation
depth-discharge
resistance
fluvial morphodynamics
wphydresambl
WRFWeather Research and Forecasting Modelmodel
research
forecasting
weather
mesoscale numerical weather
numerical weather prediction
next-generation mesoscale numerical
weather prediction system
prediction system designed
weather research
numerical weather
weather prediction
operational forecasting
atmospheric research
next-generation mesoscale
mesoscale numerical
designed to serve
serve both operational
forecasting and atmospheric
wrf
WRF-HydroThe WRF-Hydro® Modeling System, an open-source community model, is used for a range of projects, including flash flood prediction, regional hydroclimate impacts assessment, seasonal forecasting of water resources, and land-atmosphere coupling studies. It produces forecasts and analyses for all major terrestrial water-cycle components: Precipitation, Streamflow, Soil moisture, Snowpack, Flooding, Groundwater.modeling
system
precipitation
streamflow
forecasting model hydrological
model hydrological modeling
hydrological modeling system
major water cycle
water cycle components
multi-scale process models
model coupling framework
multi-physics land-atmosphere modeling
link multi-scale process
forecasting model
model hydrological
coupling framework designed
land-atmosphere modeling capability
open source
soil moisture
model
software
hydrometeorology
land-atmosphere interactions
terrestrial hydrology
hydrology
earth science
fortran
hydrologic model
wrf-hydro
WSGFAMWave and current supported sediment gravity flow modelwave
model
fine sediment riverine
sediment riverine sources
current supported sediment
supported sediment gravity
sediment gravity flows
simulates wave
high discharge
riverine sources
fine sediment
wave and current
current supported
gravity flows
seabed offshore
offshore of high
continental shelf research
sediment transport
wsgfam
Wetland3PA 3-point dynamic model for the morphological evolution of a backbarrier basin composed by marshes and mudflatsdynamic
mudflats
model
morphological
backbarrier tidal basin
mudflat depth
mudflat width
model simplifies
simplifies the geometry
backbarrier tidal
tidal basin
depth
mudflat
marsh depth
variables
width
wetland3p
XBeachMorphological changes, nearshore currents, wave propagation and sediment transport modelmorphological
nearshore
currents
wave
sediment transport
nearshore area
dunes and backbarrier
backbarrier during storms
wave propagation
long waves
transport and morphological
delft university
university of miami
two-dimensional model
corps of engineers
university of technology
army corps
beaches
public-domain model
coastal evolution
xbeach
YANGsFluvial sediment transport modelfluvial
model
bed grain size
total sediment transport
sediment transport rate
open channel assuming
median bed grain
calculates the total
grain size
total sediment
sediment transport
transport rate
open channel
channel assuming
assuming a median
median bed
bed grain
fluvial morphodynamics
yangs
ZoneControllerControls zones and populates them with taxa.controls
taxa
object manages
aspect of taxa
evaluate the spatial
spatial aspect
manages
zones’
object
evaluate
spatial
aspect
ecology
evolution
zonecontroller
ZoneTaxonA zone-based taxontaxon
zones
lower taxonomic level
zone
speciation
time
child taxon
stage
time step
lower taxonomic
taxonomic level
step
taxon member populations
object
method
ecology
evolution
zonetaxon
ZscapeA simple parallel code to demonstrate diffusiondiffusion
finite difference approximations
finite difference
great for modeling
modeling the erosion
erosion of landscapes
landscape evolution models
basin and range
difference approximations
hillslope sediment transport
paper by densmore
application of landscape
landscape evolution
anderson provides details
approximations are great
tectonic displacements
zscape