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| == D'Alpaos model ==
| | ==Introduction== |
| __TOC__
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| ===Introduction===
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| === History ===
| | == History == |
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| === Papers ===
| | == Papers == |
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| === D'Alpaos model Questionnaire === | | == Issues == |
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| ==== Contact Information ==== | | == Help == |
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| {| class="wikitable"
| | == Input Files == |
| | class="model_col1"| Model:
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| | class="model_col2"| D'Alpaos model
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| |-
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| | class="model_col1"| Contact person:
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| | class="model_col2"| Andrea D'Alpaos
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| |-
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| | class="model_col1"| Institute:
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| | class="model_col2"| University of Padova
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| |-
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| | class="model_col1"| City:
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| | class="model_col2"| Padova
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| |-
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| | class="model_col1"| Country:
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| | class="model_col2"| Italy
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| |-
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| | class="model_col1"| Email:
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| | class="model_col2"| adalpaos@idra.unipd.it
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| |-
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| | class="model_col1"| 2nd person involved:
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| | class="model_col2"| --
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| |-
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| | class="model_col1"| 3rd person involved:
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| | class="model_col2"| --
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| |}
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| ==== Model description ==== | | == Output Files == |
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| {| class="wikitable"
| | == Download == |
| | class="model_col1"| Model type:
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| | class="model_col2"| Single model for the coastal domain.
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| |-
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| | class="model_col1"| Description:
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| | class="model_col2"| 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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| |}
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| ==== Technical information ====
| | == Source == |
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| {| class="wikitable"
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| | class="model_col1"| Supported platforms:
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| | class="model_col2"| Windows
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| |-
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| | class="model_col1"| Programming language:
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| | class="model_col2"| Fortran77, Fortran90
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| |-
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| | class="model_col1"| Model development started at:
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| | class="model_col2"| 2003 and is still in development
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| |-
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| | class="model_col1"| To what degree will the model become available:
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| | class="model_col2"| Executable will be available
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| |-
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| | class="model_col1"| Current license type:
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| | class="model_col2"| GPL v2
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| |-
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| | class="model_col1"| Memory requirements:
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| | class="model_col2"| --
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| |-
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| | class="model_col1"| Typical run time:
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| | class="model_col2"| hours-days
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| |}
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| ==== Input / Output description ====
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| {| class="wikitable"
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| | class="model_col1"| Input parameters:
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| | class="model_col2"| 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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| |-
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| | class="model_col1"| Input format:
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| | class="model_col2"| ASCII
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| |-
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| | class="model_col1"| Output parameters:
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| | class="model_col2"| Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features
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| |-
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| | class="model_col1"| Output format:
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| | class="model_col2"| ASCII
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| |-
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| | class="model_col1"| Post-processing software (if needed):
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| | class="model_col2"| no
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| |-
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| | class="model_col1"| Visualization software (if needed):
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| | class="model_col2"| Yes, Matlab
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| |}
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| | |
| ==== Process description ====
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| {| class="wikitable"
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| | class="model_col1"| Processes represented by model:
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| | class="model_col2"| 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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| |-
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| | class="model_col1"| Key physical parameters & equations:
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| | class="model_col2"| --
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| |-
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| | class="model_col1"| Length scale & resolution constraints:
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| | class="model_col2"| --
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| |-
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| | class="model_col1"| Time scale & resolution constraints:
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| | class="model_col2"| --
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| |-
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| | class="model_col1"| Numerical limitations and issues :
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| | class="model_col2"| --
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| |}
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| ==== Testing ====
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| {| class="wikitable"
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| | class="model_col1"| Available calibration data sets:
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| | class="model_col2"| --
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| |-
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| | class="model_col1"| Available test data sets:
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| | class="model_col2"| --
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| |-
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| | class="model_col1"| Ideal data for testing:
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| | class="model_col2"| --
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| |}
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| ==== User groups ====
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| {| class="wikitable"
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| | class="model_col1"| Currently or plans for collaborating with:
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| | class="model_col2"| Yes
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| |}
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| ==== Documentation ====
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| {| class="wikitable"
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| | class="model_col1"| Key papers of the model:
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| | class="model_col2"|
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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.
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| *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.
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| *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.
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| *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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| |-
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| | class="model_col1"| Is there a manual available:
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| | class="model_col2"| no
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| |-
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| | class="model_col1"| Model website if any:
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| | class="model_col2"| ftp://ftp.geosc.psu.edu/sling/SimSedBasinsBook/
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| |}
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| ==== Additional comments ====
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| {| class="wikitable"
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| | class="model_col1"| Comments:
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| | class="model_col2"| --
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| |}
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| === Issues ===
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| === Help ===
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| === Input Files ===
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| === Output Files ===
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| === Download ===
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| === Source ===
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| [[Category:Coastal]] | | [[Category:Coastal]] |
Contact
Name
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Andrea D'Alpaos
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Type of contact
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Model developer
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Institute / Organization
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University of Padova
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Postal address 1
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via Loredan, 20
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Postal address 2
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via Giotto, 1
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Town / City
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Padova
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Postal code
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35131
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State
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NO STATE
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Country
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Italy
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Email address
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adalpaos@idra.unipd.it
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Phone
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+390498275757
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Fax
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+390498275446
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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
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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
|
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.
|
Input format
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ASCII
|
Other input format
|
|
Describe output parameters
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Channel network configuration and morphology, marsh platform elevations, erosion and accretion rates, relevant geomorphological features
|
Output format
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ASCII
|
Other output format
|
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Pre-processing software needed?
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No
|
Describe pre-processing software
|
|
Post-processing software needed?
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No
|
Describe post-processing software
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Visualization software needed?
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Yes
|
If above answer is yes
|
Matlab
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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
|
--
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Other
Do you have current or future plans for collaborating with other researchers?
|
Yes
|
Is there a manual available?
|
No
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Upload manual if available:
|
|
Model website if any
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|
Model forum / discussion board
|
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Introduction
History
Papers
Issues
Help
Input Files
Output Files
Download
Source |