Model:D'Alpaos model: Difference between revisions

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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

Revision as of 17:18, 19 September 2009

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 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
Model type Single
Model part of larger framework
Note on status model
Date note status model

Technical specs

Supported platforms
Windows
Other platform
Programming language

Fortran77, Fortran90

Other program language
Code optimized Single Processor
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 2003
Does model development still take place? Yes
If above answer is no, provide end year model development
Code development status
When did you indicate the 'code development status'?
Model availability As executable"As executable" is not in the list (As code, As teaching tool) of allowed values for the "Model availability" property.
Source code availability
(Or provide future intension)
Source web address
Source csdms web address
Program license type GPL v2
Program license type other
Memory requirements
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:
Model website if any
Model forum / discussion board
Comments


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/

Additional comments

Comments: --

Issues

Help

Input Files

Output Files

Download

Source