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A list of all pages that have property "Describe output parameters model" with value "Please see:". Since there have been only a few results, also nearby values are displayed.

Showing below up to 26 results starting with #1.

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  • Model:DeltaRCM  + (Matrices of: Water surface elevation; Water unit discharge and velocity field; Delta surface elevation and bathymetry; Stratigraphy (User can choose which time step to output))
  • Model:Manningseq-bouldersforpaleohydrology  + (Microsoft Excel tables)
  • Model:TOPMODEL  + (Model Interface Capabilities: There are thModel Interface Capabilities:</br>There are three options available in the program interface: </br>* The Hydrograph Prediction Option: This option allows the model to be run and hydrographs displayed. If a Topographic Index Map File is available, then a map button is displayed that allows the display of predicted simulation, either as a summary over all timesteps or animated. </br>* The Sensitivity Analysis Option: This screen allows the sensitivity of the objective functions to changes of one or more of the parameters to be explored. </br>* The Monte Carlo Analysis 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. Check boxes can be used to choose the variables and objective functions to be saved for each run. The results file produced will be compatible with the GLUE analysis software package.e with the GLUE analysis software package.)
  • Model:REF-DIF  + (Model output: * Complex amplitude, * Wave Heights and angles * Radiation stresses and forcing terms * Wave induced mass flux * Velocity moments for bottom stress calculation)
  • Model:ErosionDeposition  + (Model returns modified 'topographic__elevation', the model grid field holding model node elevations.)
  • Model:MIDAS  + (Morphodynamic evolution of a quasi-2D single-thread channel)
  • Model:AnugaSed  + (NetCDF file (.sww) of x, y, elevation, flow depth, x and y momentum, and sediment concentration (all optional))
  • Model:Cliffs  + (Netcdf binaries of velocities and elevatioNetcdf binaries of velocities and elevation screenshots in Master grid</br>�Netcdf binary of maximum water surface elevation in Master grid</br>�Netcdf Time histories of the water surface elevation at virtual gages;</br>Netcdf binaries of boundary input time-series for the enclosed grids, one �file for each boundary (east, west, north, south)r each boundary (east, west, north, south))
  • Model:SNAC  + (Nodal field data: velocity, temperature Element-centered (discontinuous) field data: strain rate, stress, plastic strain, etc.)
  • Model:AlluvStrat  + (Numpy array of channel and overbank deposit)
  • Model:Mrip  + (Options (can be turned on or off): Print eOptions (can be turned on or off):</br>Print evolving bed to screen.</br>A file with the bed with each time step, or at intermediate steps.</br>A file with the spectra of bed at each time step, or at intermediate steps.</br>A file with statistics (eg, rms roughness of bed)with statistics (eg, rms roughness of bed))
  • Model:KWAVE  + (Output Files: 1. stage -- array containingOutput Files:</br>1. stage -- array containing information on flow at the edges of the model domain</br>2. depth -- flow depth at each grid cell at the end of the simulation</br>3. vel -- flow velocity at each grid cell at the end of the simulation</br>4. maxdepth -- maximum flow depth at each grid cell</br>4. maxvel -- maximum flow velocity at each grid cell-- maximum flow velocity at each grid cell)
  • Model:ESCAPE  + (Output are grids of 3D surface evolution in HDF5)
  • Model:KnickZone-Picker  + (Output data are written as GeoTIFF files, shapefiles, CSV files.)
  • Model:IDA  + (Output drainage area, true drainage area, Output drainage area, true drainage area, and initial guess:</br> 64 bit float ('double')</br></br> Row major order is used.</br> The drainage area of cells with no drainage to or from them, such as ocean</br> cells, will be the area of the cell itself (1.0, if all cells are given</br> unit area).(1.0, if all cells are given unit area).)
  • Model:SBM  + (Output files provide snapshots of the bedfOutput files provide snapshots of the bedform domain during its evolution. They containing elevation of bedform domain, the percentage full of sediment for all 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 (not just the top layer) for analyzing stratigraphic profiles.yer) for analyzing stratigraphic profiles.)
  • Model:Coastal Dune Model  + (Output is '.dat' files showing vegetation cover density and DEM of the model domain at specified time intervals)
  • Model:GEOMBEST-Plus  + (Output parameters: * Marsh boundary - giveOutput parameters:</br>* Marsh boundary - gives the position of the backbarrier marsh edge through time</br>* Shorelines - gives the position of the barrier shoreline through time</br>* step number - saves the surface morphology and stratigraphy for the model at each time stepratigraphy for the model at each time step)
  • Model:OrderID  + (Outputs are m and r values, plus p values Outputs are m and r values, plus p values indicating the probability that the calculated m and r values could occur by chance. Graphical output is produced showing the vertical section of strata, a transition probability matrix for the facies, a histogram of facies frequency, a plot of the m value calculated from observed strata versus the m values calculated from Monte Carlo modelling of shuffled equivalent strata, and a plot of the r value calculated from observed strata versus the r values calculated from Monte Carlo modelling of shuffled equivalent strata.o modelling of shuffled equivalent strata.)
  • Model:OptimalCycleID  + (Outputs are plots of the vertical succession input along with a series of transition probability matrices and facies orders indicating the more and less ordered arrangements of facies)
  • Model:LEMming2  + (Outputs complete Matlab workspace at user-defined intervals. Outputs surface plots at user-defined intervals. Some scripts are included for additional visualization of output.)
  • Model:CHILD  + (Outputs include grids of surface elevationOutputs include grids of surface elevation, drainage area, gradient, stratigraphy, drainage direction, Voronoi cell areas, sediment texture; data on mesh configuration; total landscape volume and change in volume at each storm (time step); list of storm durations, timing, and intensities. storm durations, timing, and intensities.)
  • Model:PIHM  + (PIHM v2.0 uses Net_CDF for state and flux output. Details are under development (April 2009) and will be complete July 2009)
  • Model:1D Hillslope MCMC  + (Parameters used for simulations by the MCMC algorithm and their likelihood compared to the field data.)
  • Model:GEOtop  + (Please see:
  • Model:Instructed Glacier Model  + (Predict the evolution of glaciers, icefields, or ice sheets)
  • Model:GNE  + (Primary outputs: N, P, Si, and C yields and loads by river basin and nutrient form. Secondary outputs: Source attribution by nutrient form and main natural and anthropogenic inputs to watersheds. Total Suspended Solids are also predicted.)
  • Model:PsHIC  + (Produce 5 output files (ESRI ASCII format)Produce 5 output files (ESRI ASCII format):</br># HI.txt - pixel scale hypsometric integral;</br># max_elev.txt - the maximum elevation of the catchment flowing thorough each pixel;</br># Elev_Acc.txt - the sum of the elevation (m) of all the pixels flowing thorough each pixel;</br># flowacc.txt - Contributing area in pixels;</br></br>To change the names of the output files, edit the last section of the source code.</br># junctions.txt - how many of a pixel's 8 neighbors flow into it;any of a pixel's 8 neighbors flow into it;)
  • Model:MARSSIM  + (RAW image files of elevation and shaded relief. ASCII file of elevations at specified times. ASCII files of other state variables as desired at specified times. Iteration-by-iteration summary file)
  • Model:ROMSBuilder  + (ROMSBuilder creates the new component in hROMSBuilder creates the new component in home directory under "~/.cmt/components". It is safer not to edit the directory. Once a component is successfully created the next one goes relatively faster. To open the project user should go to "My Project > ROMSBuilder". The new project can only be seen by the owner. To share the project with the rest of the community please contact CSDMS.</br>Notes:</br>Please wait for ROMSBuilder to finish before creating the next component. Overall run time is almost an hour for the first component.</br>"Performance efficient mode" is not meant for ROMSBuilder, hence please avoid setting it on the tab dialogs.</br>Default configuration settings is always that of UPWELLING. Please edit the config values to run your new roms component.config values to run your new roms component.)
  • Model:GLUDM  + (Rasters containing the relative area of a specific land use in the future.)
  • Model:AeoLiS  + (Real-world grid cell surface area Wind velReal-world grid cell surface area</br>Wind velocity</br>Wind shear velocity</br>Wind direction</br>Bed level above reference</br>Water level above reference</br>Wave height</br>Equilibrium sediment concentration integrated over saltation height</br>Instantaneous sediment concentration integrated over saltation height</br>Instantaneous sediment flux</br>Sediment entrainment</br>Weights of sediment fractions</br>Weights of sediment fractions based on grain size distribution in the air</br>Weights of sediment fractions based on grain size distribution in the bed</br>Shear velocity threshold</br>Bed composition layer thickness</br>Moisure content</br>Salt content</br>Sediment mass in bed content Salt content Sediment mass in bed)
  • Model:BITM  + (Resultant barrier island configuration andResultant barrier island configuration and sediment distribution along the continental shelf as results of the effects of five different processes: reworking of the beach profile, inner-shelf sediment redistribution, overwash, laggonal deposition and aeolian sediment reworking.deposition and aeolian sediment reworking.)
  • Model:SPACE  + (Returns/updates Landlab grid fields: 'topographic__elevation' : Topographic surface elevation 'bedrock__elevation' : Bedrock surface elevation 'soil__depth' : Depth of alluvial layer on river bed 'sediment__flux' : Sediment flux out of each grid node)
  • Model:Avulsion  + (River positions with time)
  • Model:MRSAA  + (River profiles, sediment transport rates, alluvial cover depths and channel bed elevations.)
  • Model:OTTAR  + (River width)
  • Model:SPARROW  + (SPARROW is designed to describe the spatiaSPARROW is designed to describe the spatial patterns in water quality and the factors that affect it. SPARROW models are developed using mass balance constraints to quantify the relation between stream constituent load (the mass of the constituent being transported by the stream) and the sources and losses of mass in watersheds. Thus the models are inherently designed to predict load (mass per time) for all stream reaches in the modeling region. However, the predictions of stream load can be modified to provide a variety of water-quality metrics that can support various types of assessments.</br></br>The SPARROW prediction metrics include constituent yields, concentrations, and source contributions to stream loads: </br>*Constituent yields</br>*Constituent concentrations</br>*Source contributions to stream loadsions *Source contributions to stream loads)
  • Model:SWAN  + (SWAN can provide output on uniform, recti-SWAN can provide output on uniform, recti-linear spatial grids that are independent from the input grids and from the computational grid. In the computation with a curvi-linear computational grid, curvi-linear output grids are available in SWAN. This also holds for triangular meshes. An output grid has to be specified by the user with an arbitrary resolution, but it is of course wise to choose a resolution that is fine enough to show relevant spatial details. It must be pointed out that the information on an output grid is obtained from the computational grid by bi-linear interpolation (output always at computational time level). This implies that some inaccuracies are introduced by this interpolation. It also implies that bottom or current information on an output plot has been obtained by interpolating twice: once from the input grid to the computational grid and once from the computational grid to the output grid. If the input-, computational- and output grids are identical, then no interpolation errors occur.</br></br></br>In the regions where the output grid does not cover the computational grid, SWAN assumes output values equal to the corresponding exception value. For example, the default exception value for the significant wave height is -9. The exception values of output quantities can be changed by means of the QUANTITY command.</br></br></br>In nonstationary computations, output can be requested at regular intervals starting at a given time always at computational times. given time always at computational times.)
  • Model:Sedflux  + (Sediment properties that include (but are Sediment properties that include (but are not limited to) bulk density, grain size, porosity, and permeability. These are averaged over are user-specified vertical resolution (typically mm to cm).</br></br>Sea-floor properties that include slope, water depth, and sand fraction.ude slope, water depth, and sand fraction.)
  • Model:SRH-1D  + (Sediment transport rates, cross section geometry, bed material, flow and sediment output)
  • Model:NearCoM  + (See documentation.)
  • Model:GeoTiff Data Component  + (See documentation:
  • Model:Topography Data Component  + (See documentation:
  • Model:GridMET Data Component  + (See documentation:
  • Model:Hilltop and hillslope morphology extraction  + (See included readme)
  • Model:FUNWAVE  + (See manual, that is uploaded.)
  • Model:Glimmer-CISM  + (See paper)
  • Model:Nitrate Network Model  + (See results of related publication by J. A. Czuba.)
  • Model:River Network Bed-Material Sediment  + (See results of related publications by J. A. Czuba.)