Difference between revisions of "Terrestrial Mo"

From CSDMS
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| class="model_col1"| Input parameters:
 
| class="model_col1"| Input parameters:
| class="model_col2" colspan="2"| --
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| class="model_col2" colspan="2"| A grid with initial elevation
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Hydrologic time step and geomorphic time step
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Hydrologic paramters:
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average rainfall intensity, rainall duration, interstorm period, infiltration capacity, porosity, hydraulic conductivity, aquifer depth, specific yield, PET
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Geomorphic parameters:
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baselevel lowering rate, diffusivity for hillslope processes, weathering rate, parameters for erosion and sediment transport model
 
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| class="model_col1"| Input format:
 
| class="model_col1"| Input format:
| class="model_col2" colspan="2"|  
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| class="model_col2" colspan="2"| ASCII
 
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| class="model_col1"| Output parameters:
 
| class="model_col1"| Output parameters:
| class="model_col2" colspan="2"| --
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| class="model_col2" colspan="2"| Elevations of all nodes, elevation changes of all nodes   
 
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|-
 
| class="model_col1"| Output format:
 
| class="model_col1"| Output format:
| class="model_col2" colspan="2"|  
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| class="model_col2" colspan="2"| ASCII
 
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| class="model_col1"| Description of post-processing software (if needed):
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| class="model_col1"| Post-processing software (if needed):
| class="model_col2" colspan="2"|  
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| class="model_col2" colspan="2"| No
 
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| class="model_col1"| Description of visualization software (if needed):
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| class="model_col1"| Visualization software (if needed):
| class="model_col2" colspan="2"|  
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| class="model_col2" colspan="2"| No
 
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| class="model_section_header" colspan="3" | Process description
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| class="model_col1"| Processes represented by model:
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| class="model_col2" colspan="2"| Hydrologic processes: Precipitation, infiltration, evapotranspiration, overland flow, saturation-excess runoff, groundwater flow
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Geomorphic processes: Baselevel lowering, weathering, hillslope processes, erosion, sediment transport   
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| class="model_col1"| Key physical parameters & equations:
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| class="model_col2" colspan="2"| Infiltration capacity, water balance equation
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Hydraulic conductivity, 2-D Dupuit groundwater movement equation
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|-
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| class="model_col1"| Length scale & resolution constraints:
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| class="model_col2" colspan="2"| A grid with 100x100 cells. Typical cells with a resolution of 40x40m
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| class="model_col1"| Numerical limitations and issues :
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| class="model_col2" colspan="2"| Time scale of 10,000 years. Typical time step is 3 hour
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| class="model_section_header" colspan="3" | Testing
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| class="model_col1"| Available calibration data sets:
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| class="model_col2" colspan="2"| The hydrologic model was calibrated using hydrologic measurements of WE-38 watershed in PA
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|-
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| class="model_col1"| Available test data sets:
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| class="model_col2" colspan="2"| N/A
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|-
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| class="model_col1"| Ideal data for testing:
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| class="model_col2" colspan="2"| N/A
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| class="model_section_header" colspan="3" | User groups
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| class="model_col1"| Currently or plans for collaborating with:
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| class="model_col2" colspan="2"| None
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| class="model_section_header" colspan="3" | Documentation
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| class="model_col1"| Key papers of the model:
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| class="model_col2" colspan="2"|  Huang, X., and J. D. Niemann, How do streamflow generation mechanisms affect watershed hypsometry? Earth Surface Processes and Landforms, 2007, doi:10.1002/esp.1573 (currently published online).
 +
Huang, X., and J. D. Niemann, An evaluation of the geomorphically effective event for fluvial processes over long periods, Journal of Geophysical Research, 111, F03015, 2006, doi:10.1029/2006JF000477.
 +
Huang, X., and J. D. Niemann, Modeling the potential impacts of groundwater hydrology on long-term drainage basin evolution, Earth Surface Processes and Landforms, 31(14), 1802-1823, 2006, doi:10.1002/esp.1369.
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| class="model_col1"| Is there a manual available:
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| class="model_col2" colspan="2"|  No
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|-
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| class="model_col1"| Model website if any:
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| class="model_col2" colspan="2"|  No
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|-
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| class="model_section_header" colspan="3" | Additional comments
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|-
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| class="model_col1"| Comments:
 +
| class="model_col2" colspan="2"|  No
  
 
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Revision as of 15:39, 18 February 2008

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