Model:Shoreline

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Shoreline

Introduction

History

Papers

Shoreline Questionnaire

Contact Information

Model: Shoreline
Contact person: Scott Peckham
Institute: CSDMS, INSTAAR, University of Colorado
City: Boulder, CO
Country: USA
Email: Scott.Peckham@colorado.edu
2nd person involved: --
3rd person involved: --

Model description

Model type: Modular model for the coastal domain.
Description: 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.

Technical information

Supported platforms: UNIX, Linux, Mac OSX, Windows
Programming language: IDL
Model development started at: 2003 and was finished in 2007.
To what degree will the model become available: Source code will be available, and will be available as teaching tool a
Current license type: Apache public license
Memory requirements: Standard
Typical run time: minutes to hours

Input / Output description

Input parameters: 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
Input format: ASCII
Output parameters: The new coastline at the end of the simulation is plotted. Results are not currently saved to files.
Output format: Graphical
Post-processing software (if needed): No
Visualization software (if needed): Yes, IDL

Process description

Processes represented by model: (1) Wave properties derived from wind speed, wind angle and equations that describe a "fully-developed" sea state.
(2) Longshore sediment transport as modeled by the CERC or Kamphuis formulas.
(3) Conservation of mass for sediment.
(4) Simple methods to model cross-shore sediment transport.
Key physical parameters & equations: CERC formula for sediment transport rate (see Komar)

Kamphuis formula for sediment transport rate.
Conservation of sediment mass.

Length scale & resolution constraints: Spatial resolution of coastline is typically 1 to 50 meters.
Time scale & resolution constraints: The model is typically driven by hourly wind data (speed and angle) and models coastal change over a period of 10 to 100 years.
Numerical limitations and issues : The model cannot yet fully handle complex coastline geometries, such as those that cannot be represented (after rotation) by a single-valued function.

Testing

Available calibration data sets: This model is not calibrated, but uses physically-based (measurable) parameters and measured data for validation. See next box.
Available test data sets: 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.
Ideal data for testing: High-resolution coastal change data, for example, digitized from aerial photography or measured with GPS.

User groups

Currently or plans for collaborating with: Have collaborated somewhat with Brad Murray and Andrew Ashton.

Documentation

Key papers of the model: Peckham, S.D. (2009) Modeling longshore transport and coastal erosion due to storms at Barrow, Alaska, to be submitted with model source code to Computers and Geosciences.
Is there a manual available: no
Model website if any: no

Additional comments

Comments: --

Issues

Help

Input Files

Output Files

Download

Source