Numerical modeling of shoreline processes is an integral component of the Lake Michigan Potential Damages study. The objective is to develop a defensible deterministic analytical model for predicting erosion at a range of spatial and temporal scales for the Lake Michigan shoreline. The Flood and Erosion Prediction System that has been developed as part of FY1998 activities by Baird:
- Accounts for changes in forcing (wave and water level conditions);
- Accounts for changes in resisting factors (sand supply, sand cover and shore protection);
- Describes erosion on a temporal scale (several months to 30 years or more) that captures bluff stability detail;
- Relies on the wealth of existing recession rate data for model calibration and verification; and
- Is coupled with a ArcView GIS (through the use of tools created through Avenue scripting) to assess economic and environmental implications of "what-if" scenarios.
The GIS based Flood and Erosion Prediction System that has been developed by Baird & Associates recognizes and accounts for the inherent differences between erosion dynamics at sandy shores and cohesive shores.
The Flood and Erosion Prediction System includes links between existing numerical models (wave climate, wave propagation, COSMOS nearshore coastal processes and bluff failure) and modifications to produce a versatile model for describing and predicting erosion for short to long term time scales. The model has been tested at the eight study sites where detailed data have been collected (see 4.3 above). The model will then be applied basin wide across the Lake Michigan shoreline to estimate the degree that beach erosion and bluff recession would be expected to take place in response to various hydrologic/control scenarios over the planning horizon of the study. A schematic of the model is found in Figure 1.
The development of the coastal process model / Flood and Erosion Prediction System is expected to be continual over the course of the Study. Work to date has included refining prior modeling approaches, the development of a new conceptual model, and the development and testing of an updated model using field data collected at the Lake Michigan study sites. Anticipated work for FY 1999 and beyond will include basin-wide model application to the alternative hydrologic/control scenarios, and linkages of the GIS - Based Flood and Erosion Prediction System a comprehensive GIS context (including land based economic attributes).

- The GIS-Based Flood and Erosion Prediction System has several applications as a coastal zone management tool, following the LMPDS including:
- The ability to determine 30 and 60 year setbacks under "what if" scenarios, relying on predictive rather than extrapolated recession rates;
- Application as a management tool to assess the impacts of shore protection, jetties, breakwaters, and other shore structures;
- The ability to provide a scientifically defensible planning tool that will be accessible to the public and other stakeholders; and,
- The capability to prioritize and justify public funding of shoreline projects.
1996-1998 Activities
Over the course of the first two phases of the LMPDS (1996-1998), Baird & Associates have completed development of the core of a GIS linked Flood and Erosion Prediction System. A summary of progress by Baird & Associates and is presented here.
A Flood and Erosion Prediction System has been developed to provide a graphical, geographically referenced database of information required to predict future shoreline position. To date, the system the following key components: ArcView GIS, Nearshore wave transformation, coastal process, flood and erosion predictions (the latter with the COSMOS model). Linkages, Graphical User Interfaces and data analysis requirements have been addressed through the development of tools using Avenue scripting to enhance the ArcView GIS. The system allows users to create "projects" for studying any specified section of shoreline using the built-in data and coastal process modeling tools. Projects for eight detailed study sites around Lake Michigan have been created and the coastal process tools have been used to simulate the historical trends at these sites.
Base data that has been integrated to form part of the system includes:
- shoreline classification data (geomorphic, nearshore subaqueous, and structural classifications);
- "single value" shoreline recession rates;
- more detailed estimates of shoreline recession rates at study sites;
- lakewide digital bathymetry from NOAA;
- base map information and topography for study sites (lakewide pending);
- SHOALS bathymetry for 7 of 8 study sites (Fischer Creek, WI is not available);
- hourly WIS hindcast data for the period 1957-1987 (1987 to 1997 is pending);
- hourly water levels at 8 gauge stations for varying periods;
- weekly ice cover data for the period 1972-1995;
- ground penetrating radar at study sites (pending);
- grain size information at study sites;
- boreholes and stratigraphy at study sites; and
- available dredging records;
Added data analysis functionality has been incorporated into the GIS with the development of automated procedures to:
- extract cross-shore profiles from bathymetric and topographic data;
- conduct surface and volume comparisons of bathymetric data;
- create digital scatter plots of wave and water level data for any reach (both nearshore and offshore information), with the option of omitting periods when shore ice is present; and
- generate historical hourly water level files for any reach based on the water levels measured at the 8 available gauges.
The COSMOS coastal process model has been linked to LMPDS GIS system. The model link provides the ability to:
- automatically create the COSMOS model input file using reach-specific data and profiles;
- automatically create a cohesive profile at each reach based on the shoreline classification (sand cover);
- estimate the longshore transport at each reach which is used in the sediment budget calculations;
- estimate profile change in response to storm conditions;
- estimates long-term bluff recession rates (and confidence intervals on rates); and
- manually edit model parameters to provide flexible input for modeling "what" if scenarios;
The system as described above has been applied to the study sites to model historical shoreline trends. Analysis completed to date includes:
- surface comparisons of offshore bathymetry for the New Buffalo, Warren Dunes, and Shoreham study sites for the period from 1945 to 1997;
- generation of historical wave/water level/ice data for each reach at each study site;
- estimation of longshore transport rates and shoreline change at each study site using the COSMOS model and developed tools;
- calibration of the newly-revised bluff recession capability of COSMOS using erodibility factors derived from physical model tests (performed during FY98) and recession rates measured from historical aerial photos; and
- development of a sediment budget for each study site
1999 Activities
A key task in FY99 will be to test the ability of FEPS to predict the historic recession rates for the prototype counties. This task is critical to building confidence in the ability of the system to predict future erosion. Baird and Associates has explained that there are two primary sources of error in prediction of recession rates: 1) input data for the shoreline classification scheme being the weakest component; and 2) how processes are predicted in the model.
A Classification and Regression Tree (CART) analysis shall be completed to assess the quality and caliber of input data as it relates to recession rates. It is expected that an extension of this CART investigation from the five prototype counties to a lake-wide assessment will not be required as the selected prototype counties comprise a wide range of backshore and nearshore conditions.
FEPS will be applied to predict historic recession rates for each reach in the five prototype counties. Discrepancies between predicted and measured recession rates shall be investigated to resolve any problems with the input data and the prediction models. FEPS will also be refined to be able to shift a bluff crest line landward to represent the shore recession for a given prediction period and to then add an uncertainty band about this recession line.
Additional details will be posted here as they become available.
Using screen capture technology, animated demos of various tools being developed for the LMPDS are now available and can be viewed directly in your browser. Click on the animated links below and the demo will run. To learn more on the background behind these demos, visit the LMPDS Coastal Studies link.
The Development of Flood and Erosion Prediction (FEPS) Subpage
Click to return to the GIS Analyses Home Page.