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From CSDMS
No but possible +
No but possible +
No but possible +
Single Processor +
Creation date"Creation date" is a predefined property that corresponds to the date of the first revision of a subject and is provided by <a target="_blank" rel="nofollow noreferrer noopener" class="external text" href="https://www.semantic-mediawiki.org/wiki/Help:Special_properties">Semantic MediaWiki</a>.
18:09:50, 20 February 2009 +
Have collaborated somewhat with Brad Murray and Andrew Ashton. +
This model is not calibrated, but uses physically-based (measurable) parameters and measured data for validation. See next box. +
Model was only used for modeling coastline … Model was only used for modeling coastline change in the vicinity of Barrow, Alaska. Hourly wind data from a met station at the Barrow Airport was used to drive the model. High-resolution coastline data digitized from aerial photos by Manley et al. (2006) was used for initial and final coastlines. The latter was used for validation purposes. High-resolution DEMs were also used.oses. High-resolution DEMs were also used. +
High-resolution coastal change data, for example, digitized from aerial photography or measured with GPS. +
Initial coastline curve (array of xy pairs), depth of closure, a time series of wind speeds and angles, sediment grainsize, coastal bluff heights, a variety of configuration flags +
CERC formula for sediment transport rate (see Komar)
Kamphuis formula for sediment transport rate.
Conservation of sediment mass. +
Spatial resolution of coastline is typically 1 to 50 meters. +
The model cannot yet fully handle complex coastline geometries, such as those that cannot be represented (after rotation) by a single-valued function. +
The new coastline at the end of the simulation is plotted. Results are not currently saved to files. +
Processes:
# Wave properties derived from … Processes:</br># Wave properties derived from wind speed, wind angle and equations that describe a "fully-developed" sea state.</br># Longshore sediment transport as modeled by the CERC or Kamphuis formulas.</br># Conservation of mass for sediment.</br># Simple methods to model cross-shore sediment transport.s to model cross-shore sediment transport. +
The model is typically driven by hourly wind data (speed and angle) and models coastal change over a period of 10 to 100 years. +
Shoreline is a "line model" for modeling t … Shoreline is a "line model" for modeling the evolution of a coastline as the result of wind/wave-driven longshore sediment transport. It is based on conservation of mass and a semi-empirical sediment transport formula known as the CERC formula. This model was specifically adapted for modeling the evolution of the coastline near Barrow, Alaska.tion of the coastline near Barrow, Alaska. +
Scott +
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ASCII +
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0 +
Standard +
Coastal +
Single +
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02:19:03, 17 September 2020 +
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Coastal evolution model +
Graphical +
1560 30th street +
80309 +
false +
false +
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Apache public license +
Matlab +
Minutes to hours +
1.5D +
2002 +
Model developer +
