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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Technical specs
Supported platforms
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Windows
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Other platform
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Programming language
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Fortran77, Fortran90
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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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2003
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Does model development still take place?
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Yes
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If above answer is no, provide end year model development
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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 executable"As executable" is not in the list (As code, As teaching tool) of allowed values for the "Model availability" property.
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Source code availability (Or provide future intension)
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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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hours to days
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In/Output
Describe input parameters
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Sediment availability, vegetation characteristics, tidal forcing, rate of relative sea level rise, tidal network configuration and marsh topography if an actual domain is considered.
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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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Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features
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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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Yes
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If above answer is yes
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Matlab
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Other visualization software
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Process
Describe processes represented by the model
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The model describes the tidal-network initiation and development, and the vertical accretion of the adjacent marsh platform. Tidal network development is driven by the exceedance of a local hydrodynamic bottom shear stress, controlled by water surface gradients. Marsh vertical growth is modeled by using a sediment balance equation acconting for erosion and deposition terms. The deposition terms account for sediment settling, trapping and organic production.
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Describe key physical parameters and equations
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--
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Describe length scale and resolution constraints
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--
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Describe time scale and resolution constraints
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--
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Describe any numerical limitations and issues
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--
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Testing
Describe available calibration data sets
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--
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Upload calibration data sets if available:
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Describe available test data sets
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--
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Upload test data sets if available:
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Describe ideal data for testing
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--
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Other
Do you have current or future plans for collaborating with other researchers?
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Yes
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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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D'Alpaos model
Introduction
History
Papers
D'Alpaos model Questionnaire
Contact Information
Model:
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D'Alpaos model
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Contact person:
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Andrea D'Alpaos
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Institute:
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University of Padova
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City:
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Padova
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Country:
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Italy
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Email:
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adalpaos@idra.unipd.it
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2nd person involved:
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--
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3rd person involved:
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--
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Model description
Model type:
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Single model for the coastal domain.
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Description:
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Long-term ecomorphodynamic model of the initiation and development of tidal networks and of the adjacent marsh platform, accounting for vegetation influence and relative sea level rise effects
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Technical information
Supported platforms:
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Windows
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Programming language:
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Fortran77, Fortran90
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Model development started at:
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2003 and is still in development
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To what degree will the model become available:
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Executable will be available
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Current license type:
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GPL v2
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Memory requirements:
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--
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Typical run time:
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hours-days
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Input / Output description
Input parameters:
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Sediment availability, vegetation characteristics, tidal forcing, rate of relative sea level rise, tidal network configuration and marsh topography if an actual domain is considered.
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Input format:
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ASCII
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Output parameters:
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Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features
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Output format:
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ASCII
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Post-processing software (if needed):
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no
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Visualization software (if needed):
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Yes, Matlab
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Process description
Processes represented by model:
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The model describes the tidal-network initiation and development, and the vertical accretion of the adjacent marsh platform. Tidal network development is driven by the exceedance of a local hydrodynamic bottom shear stress, controlled by water surface gradients. Marsh vertical growth is modeled by using a sediment balance equation acconting for erosion and deposition terms. The deposition terms account for sediment settling, trapping and organic production.
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Key physical parameters & equations:
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--
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Length scale & resolution constraints:
|
--
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Time scale & resolution constraints:
|
--
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Numerical limitations and issues :
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--
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Testing
Available calibration data sets:
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--
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Available test data sets:
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--
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Ideal data for testing:
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--
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User groups
Currently or plans for collaborating with:
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Yes
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Documentation
Key papers of the model:
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- D'Alpaos, A., S. Lanzoni, M. Marani, S. Fagherazzi, and A. Rinaldo (2005), Tidal network ontogeny: channel initiation and early development, Journal of Geophysical Research--Earth Surface, 110, F02001, doi:10.1029/2004JF000182.
- D'Alpaos, A., S. Lanzoni, S. M. Mudd, and S. Fagherazzi (2006), Modeling the influence of hydroperiod and vegetation on the cross-sectional formation of tidal channels, Estuarine Coastal Shelf Science, 69, 311-324, doi:10.1016/j.ecss.2006.05.02.
- D'Alpaos, A., S. Lanzoni, M. Marani, and A. Rinaldo (2007), Landscape evolution in tidal embayments: modelling the interplay of erosion, sedimentation, and vegetation dynamics, Journal of Geophysical Research- Earth Surface, 112, F01008, doi:10.1029/2006JF000537.
- D'Alpaos, A., S. Lanzoni, M. Marani, A. Bonometto, G. Cecconi, and A. Rinaldo (2007), Spontaneous tidal network formation within a constructed salt marsh: observations and morphodynamic modelling, Geomorphology, 91, 186–197, doi: 10.1016/j.geomorph.2007.04.013
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Is there a manual available:
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no
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Model website if any:
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ftp://ftp.geosc.psu.edu/sling/SimSedBasinsBook/
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Issues
Help
Input Files
Output Files
Download
Source |