Model:Kirwan marsh model: Difference between revisions
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{{ | {{Model identity | ||
| | |Model type=Single | ||
}} | }} | ||
{{Model identity2 | |||
|ModelDomain=Coastal | |||
|One-line model description=Ecomorphoydamic model of marsh elevation and channel evolution | |||
|Extended model description=Spatially explicit model of the development and evolution of salt marshes, including vegetation influenced accretion and hydrodynamic determined channel erosion. | |||
}} | |||
{{Start model keyword table}} | |||
{{Model keywords | |||
|Model keywords=coastal morphdynamics | |||
}} | |||
{{Model keywords | |||
|Model keywords=salt Marsh - tidal Flat evolution | |||
}} | |||
{{End a table}} | |||
{{Modeler information | |||
|First name=Matthew | |||
|Last name=Kirwan | |||
|Type of contact=Model developer | |||
|Institute / Organization=University of Virginia | |||
|Postal address 1=PO Box 400123 | |||
|Town / City=Charlottesville | |||
|Postal code=22904 | |||
|State=Virginia | |||
|Country=United States | |||
|Email address=mkirwan@usgs.gov | |||
}} | |||
{{Model technical information | |||
|Supported platforms=Linux | |||
|Programming language=C | |||
|Code optimized=Single Processor | |||
|Start year development=2003 | |||
|Does model development still take place?=Yes | |||
|Program license type=GPL v2 | |||
|Memory requirements=-- | |||
|Typical run time=hour to days | |||
}} | |||
{{Input - Output description | |||
|Describe input parameters=Does not require any input data, but if desired, model can run from files describing sea level and/or the elevations of an existing marsh. | |||
|Input format=ASCII | |||
|Describe output parameters=Elevation, Biomass, Accretion Rate, Erosion Rate, and other characteristics of every cell in domain. Also outputs spatially averaged statistics. | |||
|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 calculates changes in elevation and vegetation growth for a hypothetical salt marsh. In each cell, elevation change is calculated as the difference between accretion and erosion. Accretion rates are a function of inundation depth, vegetation growth, and suspended sediment concentration. Water routed according to Rinaldo et al. (1999) scheme. Erosion rates calculated according to excess sheer stress. Channels widen according to a diffusion-like routine where downslope transport is inversely proportional to vegetation. Vegetation grows according to Morris et al. (2002) where biomass is proportional to inundation depth up until an optimum depth. Episodic vegetation disturbance is simulated by removing vegetation from randomly selected cells (Kirwan et al., 2008). Another version of the model treats wave erosion in a simplistic manner (Kirwan and Murray, 2008). | |||
|Describe key physical parameters and equations=Key parameters include the rate of sea level rise, suspended sediment concentration, tidal range (which controls vegetation distribution), critical shear stress for sediment erosion, and the period of time that erosion takes place during each tidal cycle. Parameters controlling the growth pattern of vegetation can easily be modified. | |||
|Describe length scale and resolution constraints=Domain size is 3 km by 3 km, grid cell is 5 m by 5m. | |||
|Describe time scale and resolution constraints=The model explicitly runs on an individual tidal cycle time step, which we scale up to 2 months. But, results most meaningful at timescales greater than a couple years. | |||
|Describe any numerical limitations and issues=-- | |||
}} | |||
{{Model testing | |||
|Describe available calibration data sets=Biomass productivity and marsh accretion rates from 1984-present, described in Morris et al. (2002). | |||
|Describe available test data sets=A couple high resolution Pb210 curves that span ~100 years are currently being constructed and used to test model. | |||
|Describe ideal data for testing=Long term, high resolution (annual to couple years) datasets of marsh accretion. Similar time series of channel characteristics would be useful. | |||
}} | |||
{{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=Key Papers: | |||
* '''Kirwan, M.L., and Murray, A.B., 2007. A coupled geomorphic and ecological model of tidal marsh evolution, Proc. Natl. Acad. Sci., 104, 6118-6122. Doi: ([http://dx.doi.org/10.1073/pnas.0700958104 10.1073/pnas.0700958104]). | |||
* '''Kirwan, M.L., Murray, A.B., and Boyd, W.S., 2008. Temporary vegetation disturbance as an explanation for permanent loss of tidal wetlands, Geophys. Res. Lett., 35, L05403, Doi: ([http://dx.doi.org/10.1029/2007GL032681 10.1029/2007GL032681]).''' | |||
=== | * '''Kirwan, ML and Murray, AB, 2008. Ecological and morphological response of brackish tidal marshland to the next century of sea level rise: Westham Island, British Columbia. Global and Planetary Change 60: 471-486. Doi: ([http://dx.doi.org/10.1016/j.gloplacha.2007.05.005 10.1016/j.gloplacha.2007.05.005]).''' | ||
|Manual model available=No | |||
}} | |||
{{Additional comments model | |||
|Comments=-- | |||
}} | |||
{{CSDMS staff part | |||
|OpenMI compliant=No but possible | |||
|CCA component=No but possible | |||
|IRF interface=No but possible | |||
|CMT component=No but possible | |||
}} | |||
{{Start coupled table}} | |||
{{End a table}} | |||
{{End headertab}} | |||
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== | ==Introduction== | ||
== | == History == | ||
== | == References == | ||
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== | == Issues == | ||
== | == Help == | ||
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== | == Input Files == | ||
== Output Files == | |||
[[Category: | [[Category:Source code not available]] |
Latest revision as of 20:14, 16 September 2020
Kirwan marsh model
Metadata
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Template:Kirwan marsh model autokeywords
Introduction
History
References
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