Summary
| Also known as
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| Model type
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Single
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| Model part of larger framework
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| Note on status model
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| Date note status model
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fault, erosion, hillslope, facet, spur, scarp,
,
Technical specs
| Supported platforms
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Unix, Linux, Mac OS
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| Other platform
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| Programming language
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Python
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| Other program language
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| Code optimized
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Single Processor
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| Multiple processors implemented
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| Nr of distributed processors
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| Nr of shared processors
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| Start year development
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2010
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| Does model development still take place?
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No
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| If above answer is no, provide end year model development
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2010
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| Code development status
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| When did you indicate the 'code development status'?
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| Model availability
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As code
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Source code availability (Or provide future intension)
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Through CSDMS repository
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| Source web address
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| Source csdms web address
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| Program license type
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GPL v2
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| Program license type other
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| Memory requirements
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| Typical run time
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minutes
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In/Output
| Describe input parameters
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HILLSLOPE_LENGTH: length of hillslope, in meters
NUMBER_OF_NODES: number of model nodes (initially)
EROSION_RATE: slope-normal erosion rate in m/yr
THRESHOLD_SLOPE: threshold slope angle (m/m)
THROW_RATE: fault throw rate, meters per year
FAULT_DIP: fault dip angle, degrees
SEISMIC_INTERVAL: Time interval 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: amplitude of sinusoidal variation (m/yr)
PERIOD: period of sinusoidal variation (yr)
PHASE: phase offset for sinusoidal variation (degrees)
DEL18O_FILENAME: name of file containing oxygen isotope curve
DEL18O_POWER: exponent
MIN_ERORATE:
OPT_PLOT: option for plotting
OPT_EPS_PLOT: option for output to .eps file
PLOT_INTERVAL: time interval for plotting, in years
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| Input format
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ASCII
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| Other input format
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| Describe output parameters
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Simple ascii files containing x and z coordinates of points at end of run. Optional output of figure in .eps format.
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| Output format
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ASCII
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| Other output format
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| Pre-processing software needed?
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No
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| Describe pre-processing software
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| Post-processing software needed?
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No
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| Describe post-processing software
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| Visualization software needed?
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No
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| If above answer is yes
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| Other visualization software
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Process
| Describe processes represented by the model
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Weathering and erosion of bedrock on a hillslope; vertical and horizontal displacement due to earthquakes.
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| Describe key physical parameters and equations
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See:
Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:10.1029/2010JF001861.
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| Describe length scale and resolution constraints
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Resolution on order of one to a few meters. Domain length grows over time, reaching order tens to hundreds of meters long.
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| Describe time scale and resolution constraints
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Typical time scale of order tens to hundreds of thousands of years.
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| Describe any numerical limitations and issues
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Testing
| Describe available calibration data sets
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For case study see:
Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster, and R. Phillips (2011), Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022, doi:10.1029/2010JF001861.
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| Upload calibration data sets if available:
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| Describe available test data sets
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| Upload test data sets if available:
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| Describe ideal data for testing
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Other
| Do you have current or future plans for collaborating with other researchers?
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| Is there a manual available?
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No
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| Upload manual if available:
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| Model website if any
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| Model forum / discussion board
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Download statistics
<pbars ytitle=Downloads Title='Monthly Downloads bedrock_fault_scarp' xlabels=true size=900x200 ymax=10 grid=true box=true cubic=true plots=open xformat=number connected=true angle=90 legend>
,Total downloads: 22
2008 - Jan,0
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2009 - Jan,0
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2010 - Jan,0
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2011 - Jan,0
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2014 - Jan,0
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2015 - Jan,0
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</pbars>
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History
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Input Files
Output Files
Download source code |