The viewer shows predictions of the timing and magnitude of water levels at the shoreline and potential impacts to coastal dunes.
Open the Operational Total Water Level and Coastal Change Viewer.
The USGS National Assessment of Coastal Change Hazards project is working with the National Weather Service (NWS) and the National Centers for Environmental Prediction (NCEP) to combine wave predictions from the Nearshore Wave Prediction System (NWPS) with USGS-derived beach morphology to provide regional weather offices detailed forecasts of wave-induced water levels. The interagency operational model is available at select pilot sites and model forecast can be accessed in the Total Water Level and Coastal Change Forecast viewer. The viewer includes predictions of the timing and magnitude of water levels at the shoreline and potential impacts to coastal dunes.
The primary components of total water level elevation along the coast include tides, surge, and wave-induced runup. However, existing operational water level models do not account for wave-driven water levels. The USGS National Assessment of Coastal Change Hazards project is working with the National Weather Service (NWS) and the National Centers for Environmental Prediction (NCEP) to combine wave predictions from the Nearshore Wave Prediction System (NWPS) with USGS-derived beach morphology to provide regional weather offices detailed forecasts of wave-induced water levels.
A pilot study is on-going at Duck, North Carolina, with additional sites to follow. For each study area, tides and subtidal water levels are provided by the Extratropical Surge and Tide Operations Forecast Systems (ESTOFS) and wave properties (wave height and period) are being provided along the 20-meter isobath by the NWPS. These wave characteristics provide input for the empirical wave runup model developed by Stockdon and others (2006). Beach slopes and slope uncertainty, also required by the wave runup model, are provided from multiple USGS lidar surveys in the same area. The method for determining average beach slope for U. S. sandy coastlines, along with published datasets, is published in Doran and others (2015). The spatial and temporal uncertainty in total water level due to variability in beach slope and wave height and period is also predicted using the methodology described in Doran and others (2015). Existing and future pilot sites will be instrumented with video remote sensing equipment to provide observations of total water levels for comparison to predicted values. In addition, processes driving extreme water levels and sediment transport under storm conditions will be explored to improve predictions.
Explore our geonarrative to learn more about research and tools developed to forecast real-time coastal change:

Below are other science projects associated with this project.
Forecasting Coastal Change
National Assessment of Coastal Change Hazards
Video Remote Sensing of Coastal Processes
Total Water Level and Coastal Change Forecast Viewer
Total water level (TWL) at the shoreline is the combination of tides, surge, and wave runup. A forecast of TWL is an estimate of the elevation where the ocean will meet the coast and can provide guidance on potential coastal erosion and flooding hazards.
Below are publications associated with this project.
A method for determining average beach slope and beach slope variability for U.S. sandy coastlines
Coastal topography–Northeast Atlantic coast, post-hurricane Sandy, 2012
Empirical parameterization of setup, swash, and runup
Real-Time Forecasts of Coastal Change
U.S. Geological Survey researchers develop tools to forecast coastal change hazards. This geonarrative features research and tools developed to forecast real-time coastal change.
Read news related to the Total Water Level and Coastal Change Forecast Viewer.
Below are partners associated with this project.
- Overview
The viewer shows predictions of the timing and magnitude of water levels at the shoreline and potential impacts to coastal dunes.
Open the Operational Total Water Level and Coastal Change Viewer.
The USGS National Assessment of Coastal Change Hazards project is working with the National Weather Service (NWS) and the National Centers for Environmental Prediction (NCEP) to combine wave predictions from the Nearshore Wave Prediction System (NWPS) with USGS-derived beach morphology to provide regional weather offices detailed forecasts of wave-induced water levels. The interagency operational model is available at select pilot sites and model forecast can be accessed in the Total Water Level and Coastal Change Forecast viewer. The viewer includes predictions of the timing and magnitude of water levels at the shoreline and potential impacts to coastal dunes.
Example screenshot of Total Water Level and Coastal Change Forecast Viewer on June 4, 2016, two days before Tropical Storm Colin was expected to hit Florida’s Gulf of Mexico coast. This forecast is for Treasure Island (blue balloon on map) on the day of Colin’s arrival (June 6, 2016). Top right: Expected mean (dashed line) and total (solid line) water levels for June 4 to June 9. Bottom right: expected height of water relative to height of beach dune. Map shows nearby sites where dunes were expected to erode (yellow balloons) or be overtopped by storm waves (orange balloons). (Credit: Joseph Long, St. Pete Coastal and Marine Science Center. Public domain.) The primary components of total water level elevation along the coast include tides, surge, and wave-induced runup. However, existing operational water level models do not account for wave-driven water levels. The USGS National Assessment of Coastal Change Hazards project is working with the National Weather Service (NWS) and the National Centers for Environmental Prediction (NCEP) to combine wave predictions from the Nearshore Wave Prediction System (NWPS) with USGS-derived beach morphology to provide regional weather offices detailed forecasts of wave-induced water levels.
A pilot study is on-going at Duck, North Carolina, with additional sites to follow. For each study area, tides and subtidal water levels are provided by the Extratropical Surge and Tide Operations Forecast Systems (ESTOFS) and wave properties (wave height and period) are being provided along the 20-meter isobath by the NWPS. These wave characteristics provide input for the empirical wave runup model developed by Stockdon and others (2006). Beach slopes and slope uncertainty, also required by the wave runup model, are provided from multiple USGS lidar surveys in the same area. The method for determining average beach slope for U. S. sandy coastlines, along with published datasets, is published in Doran and others (2015). The spatial and temporal uncertainty in total water level due to variability in beach slope and wave height and period is also predicted using the methodology described in Doran and others (2015). Existing and future pilot sites will be instrumented with video remote sensing equipment to provide observations of total water levels for comparison to predicted values. In addition, processes driving extreme water levels and sediment transport under storm conditions will be explored to improve predictions.
Explore our geonarrative to learn more about research and tools developed to forecast real-time coastal change:
Sources/Usage: Some content may have restrictions. Visit Media to see details.U.S. Geological Survey researchers develop tools to forecast coastal change hazards. This geonarrative features research and tools developed to forecast real-time coastal change. This is just part of the story. See full Geonarrative - Science
Below are other science projects associated with this project.
Forecasting Coastal Change
This project focuses on understanding the magnitude and variability of extreme storm impacts on sandy beaches. The overall objective is to improve real-time and scenario-based predictions of coastal change to support management of coastal infrastructure, resources, and safety.National Assessment of Coastal Change Hazards
Research to identify areas that are most vulnerable to coastal change hazards including beach and dune erosion, long-term shoreline change, and sea-level rise.Video Remote Sensing of Coastal Processes
Video observations of the coast are used to monitor a range of coastal processes, for example changes in the shoreline position, both seasonally and due to long-term effects such as sea-level rise, and instances of beach and dune erosion during extreme storm events. - Data
Total Water Level and Coastal Change Forecast Viewer
Total water level (TWL) at the shoreline is the combination of tides, surge, and wave runup. A forecast of TWL is an estimate of the elevation where the ocean will meet the coast and can provide guidance on potential coastal erosion and flooding hazards.
- Multimedia
- Publications
Below are publications associated with this project.
A method for determining average beach slope and beach slope variability for U.S. sandy coastlines
The U.S. Geological Survey (USGS) National Assessment of Hurricane-Induced Coastal Erosion Hazards compares measurements of beach morphology with storm-induced total water levels to produce forecasts of coastal change for storms impacting the Gulf of Mexico and Atlantic coastlines of the United States. The wave-induced water level component (wave setup and swash) is estimated by using modeled offsAuthorsKara S. Doran, Joseph W. Long, Jacquelyn R. OverbeckCoastal topography–Northeast Atlantic coast, post-hurricane Sandy, 2012
This Data Series contains lidar-derived bare-earth (BE) topography, dune elevations, and mean-high-water shoreline position datasets for most sandy beaches for Fire Island, New York, and from Cape Henlopen, Delaware to Cape Lookout, North Carolina. The data were acquired post-Hurricane Sandy, which made landfall as an extratropical cyclone on October 29, 2012.AuthorsHilary F. Stockdon, Kara S. Doran, Kristin L. Sopkin, Kathryn E. L. Smith, Xan FredericksEmpirical parameterization of setup, swash, and runup
Using shoreline water-level time series collected during 10 dynamically diverse field experiments, an empirical parameterization for extreme runup, defined by the 2% exceedence value, has been developed for use on natural beaches over a wide range of conditions. Runup, the height of discrete water-level maxima, depends on two dynamically different processes; time-averaged wave setup and total swasAuthorsH.F. Stockdon, R.A. Holman, P.A. Howd, A. H. Sallenger - Web Tools
Real-Time Forecasts of Coastal Change
U.S. Geological Survey researchers develop tools to forecast coastal change hazards. This geonarrative features research and tools developed to forecast real-time coastal change.
- News
Read news related to the Total Water Level and Coastal Change Forecast Viewer.
- Partners
Below are partners associated with this project.