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water, sediment and agricultural chemical yields in large complex watersheds with varying soils, land use and management coditions over long periods of time

code Go to external source code site Model citations QR-code Link to this page Other models by author OpenFOAM

MODFLOW, which is called MODFLOW-2000 in order to distinguish it from earlier versions. MODFLOW-2000 simulates steady and nonsteady flow in an irregularly

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

code Go to external source code site Model citations QR-code Link to this page Other models by author Delft3D

and drying of grid points. Propagation of a wave spectrum can be solved using regular (rectilinear or curvilinear) and unstructured (triangular) grids

present tuning in SWAN (the default settings, see command TRIAD) seems to work reasonably in many cases but it has been obtained from observations in a narrow

code Go to external source code site Model citations QR-code Link to this page Other models by author Ecopath with Ecosim

code Go to external source code site Model citations QR-code Link to this page Other models by author XBeach

code Go to external source code site Model citations QR-code Link to this page Other models by author HBV

Through web repository Source web address https://www.myroms.org/index.php?page=login Source csdms web address Program license type Other Program license

Option: In this option a large number of runs of the model can be made using uniform random samples of the parameters chosen for inclusion in the analysis

Describe available calibration data sets Testing described in various papers (see web page) Upload calibration data sets if available: Describe available

tool for use in the field of free-surface flows. Extended model description The TELEMAC system is a powerful integrated modeling tool for use in the field

aqueous model, and the SIT (Specific ion Interaction Theory) aqueous model. Using any of these aqueous models, PHREEQC has capabilities for (1) speciation

more than two decades of community collaboration in building a sea ice model suitable for multiple uses including process studies, operational forecasting

preseented using generalized terrain-following coordinates. The General Ocean Turbulent Model (GOTM) developed by Burchard’s research group in Germany (Burchard

period) are stored in files specific to that grid cell Routing of stream flow is performed separately from the land surface simulation, using a separate model

Salinity at All Nodes in the Model Grid (fort.44) 3D Velocity at All Nodes in the Model Grid (fort.45) 3D Turbulence at All Nodes in the Model Grid (fort

constraints Long-term water balance can be simulated (using a daily time step), as can individual flood events (using hourly time intervals, or even smaller). The

2-D programs and funwave1d.data for 1-D programs. With the use of intrinsic function NAMELIST in the program, variable name and its corresponding data can

code Go to external source code site Model citations QR-code Link to this page Other models by author SICOPOLIS

gov/ceam/hydrological-simulation-program-fortran-hspf Edit Model information Template:HSPF autokeywords

code Go to external source code site Model citations QR-code Link to this page Other models by author PRMS

employing fluid isomorphisms, one hydrodynamical kernel can be used to simulate flow in both the atmosphere and ocean.

Describe pre-processing software Note that many input files are created using GIS and advanced skills are required. Post-processing software needed? No

the drainage system reduction in constituent concentration through treatment in storage units or by natural processes in pipes and channels Output format

code Go to external source code site Model citations QR-code Link to this page Other models by author PISM

code Go to external source code site Model citations QR-code Link to this page Other models by author MICOM

grid-based routing in DHSVM is the ability to route w ater between arbitrarily shaped surface elements. This allows greater flexibility in defining surface

computations are programmed in Fortran 90. Excel is used as the graphical user interface. All interface operations are programmed in the Microsoft Office macro

information OTIS can also be built from source on macOS using gfortran. Here are the steps. Edit the makefiles in the otis, otis-p, share, and starpac directories

code Go to external source code site Model citations QR-code Link to this page Other models by author STWAVE

originally developed by Eric Larour, Mathieu Morlighem, and Helene Seroussi in 2005. The development team and number of users has grown significantly since

maintains implementations of WOFOST in Fortran, python and java. However, there are currently 14 known implementations of WOFOST in a variety of programming languages

the surface. Typically, a minimum of four soil layers are used in a 2-meter soil column used in WRF-Hydro but this is not a strict requirement. Additional

Flow depths calculated using version of mannings implemented across a cellular grid using a scanning algorithm. Sediment tranport using either Einstein or

Aerosol Evolution and Role on Climate Forcing Using the GISS ModelE2.1 Contribution to CMIP6. Journal of Advances in Modeling Earth Systems, 12, . 10.1029/2019MS001978

nutrient concentrations in the landscape at the catchment scale. Its spatial division is related to catchments and sub-catchments, land use or land cover, soil

can be used for all cases, by using allocatable arrays and cases defined via a single configuration file pointing to input data in files typically in the

"Code IRF or not" property. WMT component Not yet"Not yet" is not in the list (Yes, In progress, No but possible, No not possible) of allowed values for

gridded land use and land cover change (LULCC) products derived directly from an IAM—in this case, the Global Change Assessment Model (GCAM)—in a variety

correct (pit removed) DEMs using the flooding approach •Calculates flow paths (directions) and slopes •Calculates contributing area using single and multiple

inappropriate to use for calculating sea level rise effects but serve as data in areas where more precise data are not available ( in this case the elevation

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

code Go to external source code site Model citations QR-code Link to this page Other models by author ELCIRC SELFE

approach. Land systems are socio-ecological systems that reflect land use in a spatial unit in terms of land cover composition, spatial configuration, and the

differential equations (PDE), we first discretize in space via the finite volume method. This results in a system of ordinary differential equations (ODE)

version: 1.1 Doi: 10.5281/zenodo.1297012 Model citations QR-code Link to this page Other models by author OlaFlow

the architecture is typically 1-25 cm in the vertical, and 10-100 m in the horizontal when operating in 2D-mode. In 3D-mode, the ....

constituent loads in streams and rivers Extended model description LOAD ESTimator (LOADEST) is a FORTRAN program for estimating constituent loads in streams and

developed by David Tarboton's research group, first in 1994, and updated over the years. The model uses a lumped representation of the snowpack and keeps

code Go to external source code site Model citations QR-code Link to this page Other models by author ParFlow

representation of soil moisture storage capacity (using a variable infiltration curve) and runoff generation processes (using linear reservoirs). The CREST model was

soil zone. PRMS is used to simulate hydrologic responses in the first region and MODFLOW-2005 is used to simulate hydrologic processes in the second and third

code View in CSDMS GitHub repository DOI Download GSDCalculator version: 1.0 Doi: 10.1594/IEDA/100134 Model citations QR-code Link to this page Other models

each cell over time by solving the shallow water wave governing equation using a finite-volume method. ANUGA also incorporates a mesh generator that allows

Source code View in CSDMS GitHub repository DOI Download MIDAS version: 0.1 Doi: 10.1594/IEDA/100147 Model citations QR-code Link to this page Other models

snow and soil model (Snowpack) using the assumption that lateral exchange is small in these media. The model can be used to force a distributed catchment

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

of hydrological functioning; generalized loss of nutrients in soils and groundwater; loss in rivers, reservoirs, and through consumptive water withdrawals

to describe the spatial patterns in water quality and the factors that affect it. SPARROW models are developed using mass balance constraints to quantify

code View in CSDMS GitHub repository DOI Download FallVelocity version: 1.0 Doi: 10.1594/IEDA/100117 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download SubsidingFan version: 1.0 Doi: 10.1594/IEDA/100170 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download RecircFeed version: 1.0 Doi: 10.1594/IEDA/100155 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download Acronym1 version: 0.1 Doi: 10.1594/IEDA/100078 Model citations QR-code Link to this page Other models

View in CSDMS GitHub repository DOI Download RouseVanoniEquilibrium version: 1.0 Doi: 10.1594/IEDA/100157 Model citations QR-code Link to this page Other

heat flow numerical model.The model uses fine vertical resolution grid which preserves the latent-heat effects in the phase transition zone, even under

code Go to external source code site Model citations QR-code Link to this page Other models by author QTCM

View in CSDMS GitHub repository DOI Download BackwaterCalculator version: 0.1 Doi: 10.1594/IEDA/100092 Model citations QR-code Link to this page Other

evolution models and was first developed by Prof Garry Willgoose at MIT, Boston in 1989. Since that time it has been extensively reworked, developed and extended

code View in CSDMS GitHub repository DOI Download MFDrouting version: 0.1 Doi: 10.1594/IEDA/100145 Model citations QR-code Link to this page Other models

version: 2.1 Doi: 10.1594/IEDA/100091 Model citations QR-code Link to this page Other models by author Avulsion Bing Bio Compact Diffusion Flexure Inflow

Source code View in CSDMS GitHub repository DOI Download WAVEREF version: 0.1 Doi: 10.1594/IEDA/100177 Model citations QR-code Link to this page Other models

inputs is implemented in order to be able to return surface temperature. The model GEOtop simulates the complete hydrological balance in a continuous way,

degradation of a river reach using the normal flow approximation. Extended model description This workbook computes 1D bed variation in rivers due to differential

degradation of a river reach using a backwater formulation. Extended model description This program computes 1D bed variation in rivers due to differential

E-book: Calculator for evolution of long profile of a river ending in a 1D migrating delta, using the normal flow approximation. Extended model description Calculator

E-book: Calculator for evolution of long profile of a river ending in a 1D migrating delta, using a backwater formulation. Extended model description Calculator

View in CSDMS GitHub repository DOI Download BackwaterWrightParker version: 1.0 Doi: 10.1594/IEDA/100093 Model citations QR-code Link to this page Other

code View in CSDMS GitHub repository DOI Download WPHydResAMBL version: 1.0 Doi: 10.1594/IEDA/100182 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download SteadyStateAg version: 1.0 Doi: 10.1594/IEDA/100165 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download Acronym1D version: 0.1 Doi: 10.1594/IEDA/100077 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download Acronym1R version: 0.1 Doi: 10.1594/IEDA/100079 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download Iceages version: 0.1 Doi: 10.1594/IEDA/100137 Model citations QR-code Link to this page Other models

web address http://wiki.manchester.ac.uk/sphysics/index.php/SPHYSICS_Home_Page Source csdms web address Program license type GPL v2 Program license type

View in CSDMS GitHub repository DOI Download Channel-Oscillation version: 0.1 Doi: 10.1594/IEDA/100101 Model citations QR-code Link to this page Other

information CHILD was originally developed in 1997 by Nicole Gasparini, Stephen Lancaster, and Greg Tucker, in a research group directed by Rafael Bras at

Source code View in CSDMS GitHub repository DOI Download STVENANT version: 0.1 Doi: 10.1594/IEDA/100168 Model citations QR-code Link to this page Other models

operates in tidal time. Variable horizontal and vertical resolution are facilitated by the use of unstructured meshes of linear triangles in the horizontal

geometry of (almost) any glacier in the world in a fully automated and extensible workflow. Publicly available data is used for calibration and validation

Source code View in CSDMS GitHub repository DOI Download FLDTA version: 0.1 Doi: 10.1594/IEDA/100119 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download STORM version: 0.1 Doi: 10.1594/IEDA/100166 Model citations QR-code Link to this page Other models

code Go to external source code site Model citations QR-code Link to this page Other models by author Erode Erode-D8-Local Shoreline TopoFlow TopoFlow-Channels-Diffusive

Source code View in CSDMS GitHub repository DOI Download YANGs version: 0.1 Doi: 10.1594/IEDA/100184 Model citations QR-code Link to this page Other models

occur in a specified fraction of time during which the river is in flood, specified by an intermittency. A Manning-Strickler formulation is used for bed

code View in CSDMS GitHub repository DOI Download AgDegNormalSub version: 0.1 Doi: 10.1594/IEDA/100085 Model citations QR-code Link to this page Other models

reach responds to change. In computing bed level change on the alluvial reach, the normal (steady, uniform) flow approximation is used. Base level is maintained

code View in CSDMS GitHub repository DOI Download DepDistTotLoadCalc version: 1.0 Doi: 10.1594/IEDA/100110 Model citations QR-code Link to this page Other

View in CSDMS GitHub repository DOI Download SuspSedDensityStrat version: 1.0 Doi: 10.1594/IEDA/100172 Model citations QR-code Link to this page Other

View in CSDMS GitHub repository DOI Download AgDegNormalGravMixHyd version: 0.1 Doi: 10.1594/IEDA/100083 Model citations QR-code Link to this page Other

View in CSDMS GitHub repository DOI Download MFDrouting-Successive version: 0.1 Doi: 10.1594/IEDA/100146 Model citations QR-code Link to this page Other

code View in CSDMS GitHub repository DOI Download Coupled1D version: 0.1 Doi: 10.1594/IEDA/100104 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download StreamPower version: 0.1 Doi: 10.1594/IEDA/100167 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download LOGDIST version: 0.1 Doi: 10.1594/IEDA/100142 Model citations QR-code Link to this page Other models

including MOM5). Most notably, it uses the Arbitrary-Lagrangian-Eulerian (ALE) algorithm in the vertical direction to allow the use of any vertical coordinate

Source code View in CSDMS GitHub repository DOI Download SETTLE version: 0.1 Doi: 10.1594/IEDA/100162 Model citations QR-code Link to this page Other models

code Go to external source code site Model citations QR-code Link to this page Other models by author Glimmer-CISM

Source code View in CSDMS GitHub repository DOI Download Flex2D version: 0.1 Doi: 10.1594/IEDA/100122 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download ADI-2D version: 0.1 Doi: 10.1594/IEDA/100080 Model citations QR-code Link to this page Other models

View in CSDMS GitHub repository DOI Download Bedrock Erosion Model version: 0.1 Doi: 10.1594/IEDA/100096 Model citations QR-code Link to this page Other

0.1 Doi: 10.1594/IEDA/100124 Model citations QR-code Link to this page Other models by author ADI-2D Bedrock Erosion Model Channel-Oscillation Coupled1D

Source code View in CSDMS GitHub repository DOI Download Flex1D version: 0.1 Doi: 10.1594/IEDA/100120 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download Spirals1D version: 0.1 Doi: 10.1594/IEDA/100164 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download FTCS2D version: 0.1 Doi: 10.1594/IEDA/100128 Model citations QR-code Link to this page Other models

version: 0.1 Doi: 10.1594/IEDA/100138 Model citations QR-code Link to this page Other models by author ADI-2D Bedrock Erosion Model Channel-Oscillation Coupled1D

code View in CSDMS GitHub repository DOI Download Eolian Dune Model version: 0.1 Doi: 10.1594/IEDA/100115 Model citations QR-code Link to this page Other models

info Authors Kevin Furlong Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author LITHFLEX1 LITHFLEX2

info Authors Kevin Furlong Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author LITHFLEX1 LITHFLEX2

calibration data::Validation was done using several fields experiment (see publications on http://poc.obs-mip.fr/pages/research_topics/modelling/symphonie/symphonie

Source code View in CSDMS GitHub repository DOI Download ENTRAIN version: 0.1 Doi: 10.1594/IEDA/100114 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download ENTRAINH version: 0.1 Doi: 10.1594/IEDA/100113 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download BEDLOAD version: 0.1 Doi: 10.1594/IEDA/100094 Model citations QR-code Link to this page Other models

transport is assumed to take place when the river is in flood. Gravel transport is computed using the Parker (1979) approximation of the Einstein (1950)

transport of sand is used. If grain size D >= 2 mm the Parker (1979) bedload transport formulation for gravel is used. The flow is computed using the normal flow

code View in CSDMS GitHub repository DOI Download 2DFLOWVEL version: 0.1 Doi: 10.1594/IEDA/100076 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download DELTA version: 0.1 Doi: 10.1594/IEDA/100108 Model citations QR-code Link to this page Other models

Terrestrial One-line model description Read note in extended description. Filling in pits and flats in a DEM Extended model description This module code

code View in CSDMS GitHub repository DOI Download LavaFlow2D version: 0.1 Doi: 10.1594/IEDA/100140 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download Flex2D-ADI version: 0.1 Doi: 10.1594/IEDA/100121 Model citations QR-code Link to this page Other models

pathways in digital elevation models. The major aim of TopoToolbox is to offer stable and efficient analytical GIS utilities in a non-GIS environment in order

source code site Model citations QR-code Link to this page Other models by author Some use of "" in your query was not closed by a matching "".

numerical solution of the shallow water equations in spherical geometry. The shallow water equations are used as a kernel for both oceanic and atmospheric general

Source code View in CSDMS GitHub repository DOI Download SUSP version: 0.1 Doi: 10.1594/IEDA/100171 Model citations QR-code Link to this page Other models

Source code View in CSDMS GitHub repository DOI Download TURB version: 0.1 Doi: 10.1594/IEDA/100176 Model citations QR-code Link to this page Other models

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

Source code View in CSDMS GitHub repository DOI Download SVELA version: 0.1 Doi: 10.1594/IEDA/100173 Model citations QR-code Link to this page Other models

View in CSDMS GitHub repository DOI Download AgDegNormGravMixSubPW version: 0.1 Doi: 10.1594/IEDA/100087 Model citations QR-code Link to this page Other

of nodes in x direction (postive east), Maximum number of nodes in y direction (positive north), Space step in x direction (m), Space step in y direction

Source code View in CSDMS GitHub repository DOI Download LONGPRO version: 0.1 Doi: 10.1594/IEDA/100143 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download FractionalNoises2D version: 0.1 Doi: 10.1594/IEDA/100126 Model citations QR-code Link to this page Other

code View in CSDMS GitHub repository DOI Download FTCS1D-NonLinear version: 0.1 Doi: 10.1594/IEDA/100127 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download FractionalNoises1D version: 0.1 Doi: 10.1594/IEDA/100125 Model citations QR-code Link to this page Other

View in CSDMS GitHub repository DOI Download FTCS2D-TerraceDiffusion version: 0.1 Doi: 10.1594/IEDA/100129 Model citations QR-code Link to this page Other

(horizontal + vertical displacements) and climatic forces which can be used to simulate changes in base level, as well as effects of climate changes or sea-level

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

indirect (through changes in fire regime) effects of climate on the expansion rate, species composition, and extent of treeline in Alaska (Rupp et al. 2000b

code View in CSDMS GitHub repository DOI Download DredgeSlotBW version: 1.0 Doi: 10.1594/IEDA/100112 Model citations QR-code Link to this page Other models

gravel content only, in the case of the Parker (1990) relation. In the case of the Wilcock-Crowe (2003) relation, the sand is retained in the computation.

Source code View in CSDMS GitHub repository DOI Download Erode version: 3.0 Doi: 10.1594/IEDA/100116 Model citations QR-code Link to this page Other models

version: 2.1 Doi: 10.1594/IEDA/100111 Model citations QR-code Link to this page Other models by author Avulsion Bing Bio Compact Diffusion Flexure Inflow

Describe pre-processing software In cases where the standard required the use of a non-typical format (as in the use of the machine-independent binary

description LinearDiffuser is a Landlab component that models soil creep using an explicit finite-volume solution to a 2D diffusion equation.

version: 0.1 Doi: 10.1594/IEDA/100099 Model citations QR-code Link to this page Other models by author Avulsion Bing Bio Compact Diffusion Flexure Inflow

version: 2.1 Doi: 10.1594/IEDA/100139 Model citations QR-code Link to this page Other models by author Avulsion Bing Bio Compact Diffusion Flexure Inflow

Source code View in CSDMS GitHub repository DOI Download GOLEM version: 5:14 Doi: 10.1594/IEDA/100132 Model citations QR-code Link to this page Other models

two-dimensional terrain by solving equations for ice flux and mass conservation using explicit methods. A number of other authors have employed one- and two-dimensional

repository page for terrainbento. The 1.0 version is described in Barnhart et al. (2019) and the api documentation is available on our ReadTheDocs page. If you

testbed that solves the nonlinear shallow water equations on a rotating sphere using the spectral transform method. It is a parallel implementation of STSWM to

Edit Model information See also Model:Kudryavtsev_Model, another model in the Permamodel project.

of ground temperatures in permafrost environments. Extended model description The model calculates the surface energy balance in order to represent energy

version: 0.1 Doi: 10.1594/IEDA/100098 Model citations QR-code Link to this page Other models by author Avulsion Bing Bio Compact Diffusion Flexure Inflow

code Go to external source code site Model citations QR-code Link to this page Other models by author GISS AOM

Edit Model information See also Model:Frost Model, another model in the Permamodel project.

wind, daily minimum and maximum temperature. Built-in functions allow trading input variables (e.g. use cloud cover instead of solar radiation). Input format

version: 2.1 Doi: 10.1594/IEDA/100103 Model citations QR-code Link to this page Other models by author Avulsion Bing Bio Compact Diffusion Flexure Inflow

sets. Input format ASCII Other input format Describe output parameters A web page displaying skill scores for the models and plots (PNG) of the spatial distribution

test data sets: Treynor watershed, in the Nishnabotna River basin, Iowa, USA. (Two large rainfall events.) Small basin in Kentucky. Inclined plane for testing

Cheng, Nagel, Bonamy, Hsu Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author SedFoam-2.0

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

"Code IRF or not" property. WMT component Not yet"Not yet" is not in the list (Yes, In progress, No but possible, No not possible) of allowed values for

version: 2.1 Doi: 10.1594/IEDA/100169 Model citations QR-code Link to this page Other models by author Avulsion Bing Bio Compact Diffusion Flexure Inflow

code View in CSDMS GitHub repository DOI Download Cyclopath version: 0.1 Doi: 10.1594/IEDA/100106 Model citations QR-code Link to this page Other models

relative humidity (unitless) (in (0,1)) albedo = surface albedo (unitless) (in (0,1)) dust att. = dust attenuation factor (unitless) (in (0,1)) factor = cloud

Summary Contact Technical specs In/Output Process Testing Other Component info This part will be filled out by CSDMS staff

equation is used in the calculations of infiltration and pervious area rainfall excess. A Rosenbrock optimization procedure may be used to aid in calibrating

Arid_slope Bedrock: (download these 2 files and place Resist.in in the bedrock folder) Bedrock Resist.in Callisto Coastal Critical_shear_stress Deep_seepage Eolian

ID1 and ID2, in minutes) nd (number of durations and flow rates) durations (vector of durations in minutes) flow rates (vector of discharges in m^3/sec) Canals

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

Balance/Transport Model Extended model description Gridded water balance model using climate input forcings that calculate surface and subsurface runoff and ground

Hydrology One-line model description Component simulating overland flow using a 2-D numerical approximation of the shallow-water equations following the

code Go to external source code site Model citations QR-code Link to this page Other models by author DLBRM

code View in CSDMS GitHub repository DOI Download GEOMBEST version: 1.1 Doi: 10.5281/zenodo.16576 Model citations QR-code Link to this page Other models

applications to ecosystem and human health in the bay. Model validation is based on bay wide satellite remote sensing, real-time in situ measurements and historical

code Go to external source code site Model citations QR-code Link to this page Other models by author TOPOG

code Go to external source code site Model citations QR-code Link to this page Other models by author NearCoM REF-DIF

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

code Go to external source code site Model citations QR-code Link to this page Other models by author Hydromad

code Go to external source code site Model citations QR-code Link to this page Other models by author EF5

CSDMS, for conducting benchmarking studies of permafrost models. The PBS home page is located at https://permamodel.github.io/pbs. It contains links for registration

Wendell S.; 2002. Role of convection in winter mixed layer formation in the Gulf of Maine, February 1987: ROLE OF CONVECTION IN WINTER MIXED LAYER. Journal of

code Go to external source code site Model citations QR-code Link to this page Other models by author ELCIRC SELFE

lithologies; weathering and transport of discrete rock blocks; transport of soil using linear diffusion; boundary incision Describe key physical parameters and

code Go to external source code site Model citations QR-code Link to this page Other models by author ECSimpleSnow

code View in CSDMS GitHub repository DOI Download AquaTellUs version: 1.0 Doi: 10.1594/IEDA/100089 Model citations QR-code Link to this page Other models

evolution in the presence of large blocks of rock on hillslopes and in channels. Extended model description Blocklab treats landscape evolution in landscapes

cells in the top layer, and the percent of coarse material in those top cells. Furthermore, there is output for the percent coarse of every cell in the domain

centerline - measure and map changes (in width, migration areas or rates, centerline elongation, accreted/eroded areas) in space and time

endorheic) basins and finds the equilibrium between precipitation in drainage basins and evaporation in terminal lakes. Orographic precipitation is also calculated

View in CSDMS GitHub repository DOI Download ModelParameterDictionary version: 0.1 Doi: 10.1594/IEDA/100148 Model citations QR-code Link to this page Other

Source code View in CSDMS GitHub repository DOI Download MARM5D version: 1.0 Doi: 10.5281/zenodo.258080 Model citations QR-code Link to this page Other models

performance on clusters of workstations and massively parallel machines using the PVM message passing library.

code Go to external source code site Model citations QR-code Link to this page Other models by author DROG3D

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

information Development of the model began in 2005 as an Excel Visual Basic programme. Conversion to Matlab started in 2008. Downloadable version here is still

erosion Soil creep Organic sediment production Increase in effective settling due to vegetation Increase in drag due to vegetation Describe key physical parameters

the modeling objective. If plume is used in stand-alone mode, it runs events of a single day. If you are interested in exploring deposits of changing plumes

going negative.]] Input format Other input format Passed in as arguments in Landlab component call Describe output parameters Returns/updates Landlab grid

climate-based approaches. The programs are developed in C for Linux platforms, graphic output is produced using GMT scripts, and standard PCs match the CPU and

optional. default = 2 number of terms in the Taylor expansion. Two terms (default) gives the behavior described in Ganti et al. (2012). Input format ASCII

"discharge_field". If using stochastic hydrology, determines whether component is supplied with drainage area or discharge. area_field : string or array Used if discharge_method

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

version: 2.1 Doi: 10.1594/IEDA/100158 Model citations QR-code Link to this page Other models by author Sakura

Marius Huber Schwanghart Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Manningseq-bouldersforpaleohydrology

Bob Hoogendoorn Overeem Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author DeltaSIM

Giulio Mariotti Fagherazzi Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author CMFT CoastMorpho2D

Terrain analysis. One equation is the resolution of a hexagon can be estimated using its area instead of edge length. Describe length scale and resolution constraints

for simulating aeolian sediment transport in situations where supply-limiting factors are important, like in coastal environments. Extended model description

version: 1.0 Doi: 10.5281/zenodo.821601 Model citations QR-code Link to this page Other models by author Meander Centerline Migration Model

R.; Chao, S.-Y.; Sanford, L.P.; 2006. Using a random displacement model to simulate turbulent particle motion in a baroclinic frontal zone: A new implementation

between earthquakes, in years RUN_DURATION: duration of run in years DT: time step duration in years OPT_ERO_VAR: option for time variation in erosion rate AMPLITUDE:

Source code View in CSDMS GitHub repository DOI Download Hyper version: 0.1 Doi: 10.1594/IEDA/100136 Model citations QR-code Link to this page Other models

code Go to external source code site Model citations QR-code Link to this page Other models by author HIM

code View in CSDMS GitHub repository DOI Download MarshPondModel version: 1.0 Doi: 10.5281/zenodo.4085606 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download SLEPIAN Alpha version: 1.0.0 Doi: 10.5281/zenodo.15704 Model citations QR-code Link to this page Other models

Through web repository Source web address https://www.myroms.org/index.php?page=login Source csdms web address Program license type Other Program license

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

Describe ideal data for testing One of the case studies in Cohen et al (2017). Flood event in Lyons, CO.

of a specific land use (e.g. cropland) and global population. The equation is used to extrapolate that land use are into the future in each grid cell with

simulate hydrologic state variables in space and time while using information regarding heterogeneity in climate, land use, topography and hydrogeology. However

code View in CSDMS GitHub repository DOI Download SLEPIAN Charlie version: 1.0.0 Doi: 10.5281/zenodo.15706 Model citations QR-code Link to this page Other

sediment loads in Minnesota Rivers are a plausible cause of observed mussel population declines. The model and results are described in detail in the following

code View in CSDMS GitHub repository DOI Download SLEPIAN Bravo version: 1.0.0 Doi: 10.5281/zenodo.15705 Model citations QR-code Link to this page Other models

code View in CSDMS GitHub repository DOI Download Point-Tidal-flat version: 0.1 Doi: 10.1594/IEDA/100153 Model citations QR-code Link to this page Other models

the "Blocky River and Knickpoint Evolution" model developed by Charles Shobe in collaboration with Greg Tucker and Bob Anderson at the University of Colorado

info Authors Jonathan Czuba Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Nitrate Network Model

version: 1.0.0 Doi: 10.5281/zenodo.1705386 Model citations QR-code Link to this page Other models by author GRLP GSFLOW-GRASS HydroRaVENS OTTAR

version: 2.0 Doi: 10.5281/zenodo.847746 Model citations QR-code Link to this page Other models by author Coastal Dune Model

tool that researchers and students can learn to use quickly and easily, whether or not they are experts in high-performance computing. Icepack is built on

code Go to external source code site Model citations QR-code Link to this page Other models by author Detrital Thermochron

significant control on water temperature, especially in shallow rivers, and perhaps even more so in rivers in permafrost terrain. Riverbed heat flux consists

Source code View in CSDMS GitHub repository DOI Download PsHIC version: 0.1 Doi: 10.1594/IEDA/100154 Model citations QR-code Link to this page Other models

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

version: 0.1 Doi: 10.1594/IEDA/100090 Model citations QR-code Link to this page Other models by author Area-Slope Equation Calculator FwDET GLUDM MARM5D PsHIC

Leave as the default in most normal use cases. soil_pore_size_distribution_index : An index describing the distribution of pore sizes in the soil, and controlling

Through web repository Source web address https://www.myroms.org/index.php?page=login Source csdms web address Program license type Other Program license

code Go to external source code site Model citations QR-code Link to this page Other models by author AquaTellUs CMIP Frost Model Kudryavtsev Model River

temperature time series at variable depths into the subsurface in deg C lake depth in m ice thickness in m Output format Other output format matlab plots and variables

Source code View in CSDMS GitHub repository DOI Download FVshock version: 0.1 Doi: 10.1594/IEDA/100130 Model citations QR-code Link to this page Other models

info Authors Luke McGuire Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author KWAVE SWEHR

info Authors Peter Burgess Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author CarboCAT Cyclopath

code View in CSDMS GitHub repository DOI Download Pllcart3d version: 0.1 Doi: 10.1594/IEDA/100151 Model citations QR-code Link to this page Other models

capable of running Monte Carlo simulations (in parallel to reduce computational time) to quantify uncertainty in model predictions.

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

code View in CSDMS GitHub repository DOI Download WILSIM version: 30-03-03 Doi: 10.1594/IEDA/100180 Model citations QR-code Link to this page Other models

deforming elasto-visco-plastic solid in 3D. Extended model description SNAC can solve momentum and heat energy balance equations in 3D solid with complicated rheology

observations from physical experiments. A single plain text file in the directory, called "input", provides parameters for the model. The contents of this

= z (in m) and column 2 = salinity (in PSU) seatemp_summer.txt: summer water temperature profile: column 1 = z (in m) and column 2 = salinity (in deg C)

info Authors Gerard Salter Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Bifurcation

version: 1.0.0 Doi: 10.5281/zenodo.1487716 Model citations QR-code Link to this page Other models by author GRLP GSFLOW-GRASS HydroRaVENS OTTAR

The code is build on top of PETSc and the current version of the code uses a marker-in-cell approach with a staggered finite difference discretization.

code View in CSDMS GitHub repository DOI Download SLEPIAN Delta version: 1.0.0 Doi: 10.5281/zenodo.15707 Model citations QR-code Link to this page Other models

Version 4.0 Doi: 10.5281/zenodo.10563890 Model citations QR-code Link to this page Other models by author CMFT CoastMorpho2D MCPM MarshMorpho2D MarshPondModel

code Go to external source code site Model citations QR-code Link to this page Other models by author CAM-CARMA

Blom Chavarrias, Arkesteijn Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Elv-GST GST-extendedmodel

tectonic uplift or changes in base-level and climate effects in terms of precipitation. A full technical description is reported in Refice et al. 2011 . The

fluid, rock, and grain aggregates that are either stationary or in a state of motion in one of the six cardinal lattice directions. Cells representing near-surface

version: v1.0 Doi: 10.5281/zenodo.1218142 Model citations QR-code Link to this page Other models by author Barrier Inlet Environment (BRIE) Model

the channel bed, exist within a river cell. The river course is determined using a steepest-descent methodology, and erosion and deposition along the river

Authors Sadegh Jafarinik Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Mixed bedrock-alluvial

formation of strike valleys, cuestas, and cliffbands in heterogeneous stratigraphy". Given the inputs in that paper it should generate the same results.

code Go to external source code site Model citations QR-code Link to this page Other models by author Mocsy

This means that instead of using bed slope in Manning's equation or the law of the wall, the water-surface slope is used.

visualization software. Grid sequences saved in netCDF files can be viewed as animations and saved as movies using VisIt. Visualization software needed? Yes

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

info Authors Nathan Brown Source code Model citations QR-code Link to this page Other models by author LuSS

info Authors Jonathan Czuba Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Nitrate Network Model

Authors Mohamad Nasr-Azadani Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author TURBINS

comparison (in dimensionless E* R* format; see Roering et al. 2007 or Hurst et al. 2012). Input format ASCII Other input format command line arguments Describe

channel that are soil in Pascals) lenzone (the length of channel that is bare soil in Meters) Pmmphr (Rainfall to be used for erosion in Millimeters per Hour)

Source code View in CSDMS GitHub repository DOI Download CVPM version: 1.1 Doi: 10.5281/zenodo.1237889 Model citations QR-code Link to this page Other models

Sawai (1981) and Johannesson and Parker (1989). Those using the program should refer to the papers in the Bibliography for more specific descriptions of the

"Code IRF or not" property. WMT component Not yet"Not yet" is not in the list (Yes, In progress, No but possible, No not possible) of allowed values for

files; The 'MINTEQ Input file' is created using the Proteq utility; remaining input files may be created using a text editor Post-processing software needed

info Authors Peter Burgess Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author CarboCAT Cyclopath

code View in CSDMS GitHub repository DOI Download LEMming version: 0.1.5 Doi: 10.1594/IEDA/100141 Model citations QR-code Link to this page Other models

grid spacing in metres PARAMETER (DELT=1d0), c time step in years Input format ASCII Other input format Describe output parameters change in topographic

migration rate. In the 'meanderpy' module we use a simple linear relationship between the nominal migration rate and curvature, as recent work using time-lapse

for a slightly narrower channel. Using these values, erosion potential is calculated for all three scenarios (no change in width, slightly wider, slightly

View in CSDMS GitHub repository] DOI Download DeltaRCM Vegetation version: 1.0 Doi: 10.5281/zenodo.143243 Model citations QR-code Link to this page Other

info Authors Brian Yanites Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author CosmoLand OTTER

Authors giulio mariotti Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Wetland3P

Summary Contact Technical specs In/Output Process Testing Other Component info This part will be filled out by CSDMS staff

Authors Astrid Blom Chavarrias Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author Elv-GST GST-extendedmodel

simply put all the files in the same directory, set that directory as the default directory for Matlab, and type "WSGFAM_131" in the MatLab Command Window

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

model run script to create unique conditions for each run - e.g., instead of using the same storm history by drawing from the a single barrier3d-storms.npy

scheme and dimensional splitting as in (Titov and Synolakis, 1998), and reflection and inundation computations as in (Tolkova, 2014). References: Titov

code Go to external source code site Model citations QR-code Link to this page Other models by author Auto marsh

code Go to external source code site Model citations QR-code Link to this page Other models by author Sedtrans05

Summary Contact Technical specs In/Output Process Testing Other Component info This part will be filled out by CSDMS staff

boundary segment information and hole (or island) information in form of a .poly file, as described in the Triangle manual (http://www.cs.cmu.edu/~quake/triangle

info Authors Martin Hurst Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author 1D Hillslope MCMC

of the mesh Line9: inputs the time step in seconds Line10: inputs the starting date (day, month, year), time (in seconds after midnight). The value of time

code View in CSDMS GitHub repository DOI Download MRSAA version: 1.0.0 Doi: 10.5281/zenodo.893093 Model citations QR-code Link to this page Other models

can be modified in the source code and re-compiling. Describe time scale and resolution constraints The model is abstract. Time given in iterations, relating

0.1 Doi: 10.5281/zenodo.18772 Model citations QR-code Link to this page Other models by author GreenAmptInfiltrationModel

"Code IRF or not" property. WMT component Not yet"Not yet" is not in the list (Yes, In progress, No but possible, No not possible) of allowed values for

for unvegetated areas Increase in τcr with depth below MLW Settling velocity in unvegetated areas Settling velocity in vegetated areas Tidal range Tidal

start. Nothing yet, but it might be incorporated in some work with Francis Rengers on gully incision in West Bijou Creek: see http://cires.colorado.edu

momentum term in equation for Δv T_4 = A_w * (g * d(i,t) * S(i,t)) = gravity term in equation for Δv T_5 = -A_w * (f(i,t) * v(i,t)^2) = friction term in equation

kilometers to tens of kilometers using a range of wave parameters as inputs. It calculates the cross-shore sediment flux using both shallow water wave assumptions

coefficient of friction, wave friction factor, density, etc) most are in there using values from the literature, but easily modified. Flow. (Sinusoidal,

vertical load in the geomechanical module as well as the hydraulic head boundary condition at the land surface in the hydrologic module. In this study we

need to be specified (in order) in a file called "input.txt": nx – number of grid cells in x direction ny – number of grid cells in y direction dx – grid

parameters are defined in a well-documented and commented Matlab parameter file. Only a Digital Elevation Model, preferable in GeoTIFF format is needed

solves the momentum balance and the heat transfer in Lagrangian form using unstructured meshes. It can be used to study the long-term deformation of Earth's

Authors Alan Richardson Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author IDA

specifies the underlying asymmetry in the particle dynamics. The process of determining these parameters is described in the simulation section of a corresponding

info Authors Luca Malatesta Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author LateralVerticalIncision

Integrating thermokarst features in the Upper Kuparuk and Imnavait Basin using remote sensing and ground-truth data in TopoFlow, Poster H21A-0199, Fall

can be used to map out areas of hillslopes where the emergence of bedrock drives an increase in surface roughness. The tool requires an input DEM in float

code Go to external source code site Model citations QR-code Link to this page Other models by author WACCM-EE

experiments which are described in Eke's MS thesis. The results are summarized in her thesis and in a conference paper that she presented in Vancouver. Upload calibration

events such as impact cratering or base-level changes. The program is written in Fortran and involves multiple process modules. A Python-based GUI is included

Fiona Clubb Mudd, Milodowski Source code View in CSDMS GitHub repository Model citations QR-code Link to this page Other models by author DrEICH algorithm

map the floodplain extent using a Height Above Nearest Drainage (HAND) approach, and calculate stream and floodplain metrics using three approaches.

View in CSDMS GitHub repository DOI Download DeltaClassification version: v1.0 Doi: 10.5281/zenodo.3926763 Model citations QR-code Link to this page Other

statistics from the HYDRO.IN file will be used when there is no HYDRO.CLIMATE file in the input directory. This is the format of the file in case you want to create

purpose of the instructions on this page are to explain how to download, compile, and use the model. Please keep in mind this is an open-source project

code Go to external source code site Model citations QR-code Link to this page Other models by author SiStER

Describe input parameters The input files are a DEM in .flt format, a channel heads file generated using the DrEICH algorithm (https://csdms.colorado.edu

among others, which are input to the model either using a config file or via command line arguments.

code View in CSDMS GitHub repository DOI Download GEOMBEST-Plus version: 1.0 Doi: 10.5281/zenodo.16687 Model citations QR-code Link to this page Other models

user to select the solution method. This page contains some information on gFlex, but its main documentation is in the README.md file, displayed at the gFlex

code View in CSDMS GitHub repository DOI Download CrevasseFlow version: 0.0.1 Doi: 10.1594/IEDA/100105 Model citations QR-code Link to this page Other models

pre-1930 Minnesota River between Mankato and Jordan, Minnesota, using data available in the literature and on the USGS website. Upload calibration data

Cardiff University began beta testing in May 2013. The working version of the code used in the manuscript was finished in June 2013. If you find bugs, email

SFINCS solves the SSWE and thus includes advection in the momentum equation. However, it can also run using the LIE without advection. Processes such as spatially

debris-flow prone catchment in the Swiss Alps (Illgraben). It consists of two connected sediment reservoirs on the hillslope and in the channel, where sediment

Model is built using the Landlab software package. The HyLands model builds on three new components: water and sediment is routed using the PriorityFloodFlowRouter

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

network, where local divergence in sediment flux drives bed elevation change. The model represents hydrodynamics using rules for flow routing and stress

Edit Model information This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)

"Code IRF or not" property. WMT component Not yet"Not yet" is not in the list (Yes, In progress, No but possible, No not possible) of allowed values for

contain other user-specified agent outputs as long as users use this data collector object in their ABM modules. Output format ASCII Other output format

the order of kilometers. Main geomorphic processes are featured in Kirwan et al. 2016 in GRL, and carbon processes track allochthonous and autocthonous

implemented in a particular framework are reusable in other models within the same framework, with little migration effort. One advantage of using a modeling