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| | {{Modeler information |
| | |First name=Andrea |
| | |Last name=D'Alpaos |
| | |Type of contact=Model developer |
| | |Institute / Organization=University of Padova |
| | |Postal address 1=via Loredan, 20 |
| | |Postal address 2=via Giotto, 1 |
| | |Town / City=Padova |
| | |Postal code=35131 |
| | |State=NO STATE |
| | |Country=Italy |
| | |Email address=adalpaos@idra.unipd.it |
| | |Phone=+390498275757 |
| | |Fax=+390498275446 |
| | }} |
| | {{Model identity |
| | |Model type=Single |
| | |Categories=Coastal |
| | |One-line model description=Tidal network and marsh model |
| | |Extended model description=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 |
| | }} |
| | {{Model technical information |
| | |Supported platforms=Windows |
| | |Programming language=Fortran77, Fortran90 |
| | |Code optimized=Single Processor |
| | |Start year development=2003 |
| | |Does model development still take place?=Yes |
| | |Model availability=As executable |
| | |Program license type=GPL v2 |
| | |OpenMI compliant=No but possible |
| | |CCA component=No but possible |
| | |IRF interface=No but possible |
| | |Typical run time=hours to days |
| | }} |
| | {{Input - Output description |
| | |Describe input parameters=Sediment availability, vegetation characteristics, tidal forcing, rate of relative sea level rise, tidal network configuration and marsh topography if an actual domain is considered. |
| | |Input format=ASCII |
| | |Describe output parameters=Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features |
| | |Output format=ASCII |
| | |Pre-processing software needed?=No |
| | |Post-processing software needed?=No |
| | |Visualization software needed?=Yes |
| | |If above answer is yes=Matlab |
| | }} |
| | {{Process description model |
| | |Describe processes represented by the model=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. |
| | |Describe key physical parameters and equations=-- |
| | |Describe length scale and resolution constraints=-- |
| | |Describe time scale and resolution constraints=-- |
| | |Describe any numerical limitations and issues=-- |
| | }} |
| | {{Model testing |
| | |Describe available calibration data sets=-- |
| | |Describe available test data sets=-- |
| | |Describe ideal data for testing=-- |
| | }} |
| | {{Users groups model |
| | |Do you have current or future plans for collaborating with other researchers?=Yes |
| | }} |
| | {{Documentation model |
| | |Provide key papers on model if any=Papers: |
| | *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 |
| | |Manual model available=No |
| | }} |
| | {{Additional comments model}} |
| {{Infobox Model | | {{Infobox Model |
| |model name = D'Alpaos model | | |model name = D'Alpaos model |
Contact
Name
|
Andrea D'Alpaos
|
Type of contact
|
Model developer
|
Institute / Organization
|
University of Padova
|
Postal address 1
|
via Loredan, 20
|
Postal address 2
|
via Giotto, 1
|
Town / City
|
Padova
|
Postal code
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35131
|
State
|
NO STATE
|
Country
|
Italy
|
Email address
|
adalpaos@idra.unipd.it
|
Phone
|
+390498275757
|
Fax
|
+390498275446
|
D'Alpaos model
This code has been community reviewed and published in the open access Journal of Open Source Software (JOSS)
Metadata
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
|
Windows
|
Other platform
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|
Programming language
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Fortran77, Fortran90
|
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
|
hours to days
|
In/Output
Describe input parameters
|
Sediment availability, vegetation characteristics, tidal forcing, rate of relative sea level rise, tidal network configuration and marsh topography if an actual domain is considered.
|
Input format
|
ASCII
|
Other input format
|
|
Describe output parameters
|
Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features
|
Output format
|
ASCII
|
Other output format
|
|
Pre-processing software needed?
|
No
|
Describe pre-processing software
|
|
Post-processing software needed?
|
No
|
Describe post-processing software
|
|
Visualization software needed?
|
Yes
|
If above answer is yes
|
Matlab
|
Other visualization software
|
|
Process
Describe processes represented by the model
|
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.
|
Describe key physical parameters and equations
|
--
|
Describe length scale and resolution constraints
|
--
|
Describe time scale and resolution constraints
|
--
|
Describe any numerical limitations and issues
|
--
|
Testing
Describe available calibration data sets
|
--
|
Upload calibration data sets if available:
|
|
Describe available test data sets
|
--
|
Upload test data sets if available:
|
|
Describe ideal data for testing
|
--
|
Other
Do you have current or future plans for collaborating with other researchers?
|
Yes
|
Is there a manual available?
|
No
|
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:
|
D'Alpaos model
|
Contact person:
|
Andrea D'Alpaos
|
Institute:
|
University of Padova
|
City:
|
Padova
|
Country:
|
Italy
|
Email:
|
adalpaos@idra.unipd.it
|
2nd person involved:
|
--
|
3rd person involved:
|
--
|
Model description
Model type:
|
Single model for the coastal domain.
|
Description:
|
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
|
Technical information
Supported platforms:
|
Windows
|
Programming language:
|
Fortran77, Fortran90
|
Model development started at:
|
2003 and is still in development
|
To what degree will the model become available:
|
Executable will be available
|
Current license type:
|
GPL v2
|
Memory requirements:
|
--
|
Typical run time:
|
hours-days
|
Input / Output description
Input parameters:
|
Sediment availability, vegetation characteristics, tidal forcing, rate of relative sea level rise, tidal network configuration and marsh topography if an actual domain is considered.
|
Input format:
|
ASCII
|
Output parameters:
|
Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features
|
Output format:
|
ASCII
|
Post-processing software (if needed):
|
no
|
Visualization software (if needed):
|
Yes, Matlab
|
Process description
Processes represented by model:
|
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.
|
Key physical parameters & equations:
|
--
|
Length scale & resolution constraints:
|
--
|
Time scale & resolution constraints:
|
--
|
Numerical limitations and issues :
|
--
|
Testing
Available calibration data sets:
|
--
|
Available test data sets:
|
--
|
Ideal data for testing:
|
--
|
User groups
Currently or plans for collaborating with:
|
Yes
|
Documentation
Key papers of the model:
|
- 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
|
Is there a manual available:
|
no
|
Model website if any:
|
ftp://ftp.geosc.psu.edu/sling/SimSedBasinsBook/
|
Issues
Help
Input Files
Output Files
Download
Source |