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Lynne Dingerson, The Baldwin Group at NOAA Coastal ... - GeoTools

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<strong>Coastal</strong> Applic<strong>at</strong>ions of High<br />

Resolution Elev<strong>at</strong>ion D<strong>at</strong>a<br />

Rebecca M<strong>at</strong>aosky<br />

<strong>NOAA</strong> <strong>Coastal</strong> Services Center


Purpose<br />

To highlight some of the common coastal<br />

applic<strong>at</strong>ions of high resolution elev<strong>at</strong>ion d<strong>at</strong>a<br />

<strong>Coastal</strong> Applic<strong>at</strong>ions<br />

• <strong>Coastal</strong> inund<strong>at</strong>ion prediction<br />

• Lake level drop impacts<br />

• <strong>Coastal</strong> change visualiz<strong>at</strong>ion<br />

• Shoreline deline<strong>at</strong>ion<br />

• Habit<strong>at</strong> mapping


High Resolution Elev<strong>at</strong>ion D<strong>at</strong>a:<br />

How to Define<br />

For this present<strong>at</strong>ion, high resolution elev<strong>at</strong>ion d<strong>at</strong>a:<br />

• Provide elev<strong>at</strong>ions of Earth’s surface on land or under w<strong>at</strong>er<br />

• Support a grid cell resolution of five meters (m) or less<br />

• Meet a vertical accuracy of one meter or less RMSE<br />

(root mean square error)<br />

• Meet a horizontal accuracy of five meters or less RMSE<br />

• Are d<strong>at</strong>a th<strong>at</strong> can be collected by aerial or b<strong>at</strong>hymetric surveys


Types of High Resolution Elev<strong>at</strong>ion D<strong>at</strong>a<br />

Topographic B<strong>at</strong>hymetric Topob<strong>at</strong>hy<br />

Land elev<strong>at</strong>ion Seafloor elev<strong>at</strong>ion Combines topographic and<br />

b<strong>at</strong>hymetric d<strong>at</strong>a to cre<strong>at</strong>e<br />

a seamless model of the<br />

interface between<br />

land and w<strong>at</strong>er


<strong>Coastal</strong> Inund<strong>at</strong>ion Prediction<br />

<strong>The</strong> condition under which w<strong>at</strong>er covers normally dry land<br />

• Caused by storm surges, tsunamis, inland flooding, high tides, sea level rise<br />

• Can result in severe onshore impacts<br />

• Predicting the extent of the inund<strong>at</strong>ion can aid in decision making<br />

<strong>The</strong> SLOSH (Sea, Lake, and Overland<br />

Surges from Hurricanes) model and<br />

other inund<strong>at</strong>ion prediction models use<br />

topob<strong>at</strong>hy d<strong>at</strong>a as a base of analysis.


<strong>Coastal</strong> Inund<strong>at</strong>ion Prediction<br />

<strong>The</strong> SLOSH results can then be mapped onto a high resolution<br />

topographic surface (lidar) to cre<strong>at</strong>e an inund<strong>at</strong>ion map th<strong>at</strong> shows<br />

which areas are likely to be inund<strong>at</strong>ed by each storm c<strong>at</strong>egory.<br />

Storm surge zones by<br />

hurricane c<strong>at</strong>egory for<br />

Ch<strong>at</strong>ham County, Georgia


<strong>Coastal</strong> Inund<strong>at</strong>ion Prediction<br />

SLOSH Run C<strong>at</strong>egory 1 Maximum of Maximums<br />

SLOSH Elev<strong>at</strong>ion on N<strong>at</strong>ional Elev<strong>at</strong>ion D<strong>at</strong>aset<br />

SLOSH Elev<strong>at</strong>ion on lidar


<strong>Coastal</strong> Inund<strong>at</strong>ion Prediction<br />

Mean sea level (MSL)<br />

Mean high w<strong>at</strong>er<br />

(MHW)<br />

MHW + 0.6 m (IPCC*)<br />

MHW + 0.8 m (IPCC)<br />

Hurricane Hugo<br />

Hugo + 0.8 m<br />

* IPCC – Intergovernmental Panel on Clim<strong>at</strong>e Change


<strong>Coastal</strong> Inund<strong>at</strong>ion Prediction<br />

Shallow <strong>Coastal</strong> Flooding<br />

High tides in Charleston, South Carolina, often cause shallow<br />

coastal flooding, which is defined by the N<strong>at</strong>ional We<strong>at</strong>her<br />

Service as a tide of 7.0 feet or more.


<strong>Coastal</strong> Inund<strong>at</strong>ion Prediction<br />

Shallow <strong>Coastal</strong> Flooding<br />

Shallow coastal flooding inund<strong>at</strong>ion and sea level rise map


Lake Level Drop Impacts<br />

Lake Ontario<br />

<strong>The</strong> N<strong>at</strong>ure Conservancy is examining the impacts of lake level<br />

drop on coastal habit<strong>at</strong> migr<strong>at</strong>ion and developing effective<br />

conserv<strong>at</strong>ion and management str<strong>at</strong>egies.


Lake Level Drop Impacts<br />

Topob<strong>at</strong>hy Surface of Lake Ontario<br />

Cre<strong>at</strong>ed from<br />

gridded <strong>NOAA</strong><br />

hydrographic survey<br />

d<strong>at</strong>a combined with<br />

U.S. Geological<br />

Survey topographic<br />

grids, ~90 m<br />

resolution


Lake Level Drop Impacts<br />

Developing an inventory of available topo and b<strong>at</strong>hy d<strong>at</strong>a<br />

sources to produce topob<strong>at</strong>hy surfaces for areas of interest


Lake Level Drop Impacts<br />

From this USACE topob<strong>at</strong>hy lidar, new site-specific<br />

topob<strong>at</strong>hy surfaces will be constructed for TNC’s areas of interest


<strong>Coastal</strong> Change Visualiz<strong>at</strong>ion<br />

Monitoring shoreline change allows coastal resource managers to keep the<br />

public informed, invest time and effort in <strong>at</strong> risk areas, prioritize habit<strong>at</strong><br />

restor<strong>at</strong>ion, and model the success of potential protective measures.<br />

Pre-nourishment<br />

Post -nourishment


<strong>Coastal</strong> Change Visualiz<strong>at</strong>ion<br />

1997<br />

2000<br />

2007<br />

Isle of Palms – Wild Dunes


<strong>Coastal</strong> Change Visualiz<strong>at</strong>ion<br />

High resolution topob<strong>at</strong>hy d<strong>at</strong>a collected <strong>at</strong> different times<br />

allows for assessment of coastal change in beach<br />

volume and extent.


<strong>Coastal</strong> Change Visualiz<strong>at</strong>ion<br />

1997<br />

2000<br />

2007<br />

Folly Beach


Shoreline Deline<strong>at</strong>ion<br />

A topob<strong>at</strong>hy surface allows for a legally defensible,<br />

reproducible shoreline and reduces subjectivity


Shoreline Deline<strong>at</strong>ion<br />

<strong>NOAA</strong> is experimenting with using a topob<strong>at</strong>hy surface cre<strong>at</strong>ed<br />

from lidar elev<strong>at</strong>ion d<strong>at</strong>a sets to deline<strong>at</strong>e shoreline<br />

Advantages<br />

• Provides a defined, measurable accuracy<br />

• Provides ancillary d<strong>at</strong>a on shoreline aspects,<br />

slopes, and morphology<br />

• Can be cre<strong>at</strong>ed economically under wider range<br />

of tidal stages<br />

Shoreline derived from a topob<strong>at</strong>hy surface near San Francisco, CA, 2008


Shoreline Deline<strong>at</strong>ion<br />

Setback Lines<br />

South Carolina has<br />

used a topob<strong>at</strong>hy<br />

surface to determine<br />

the crest of the<br />

primary dune.


Shoreline Deline<strong>at</strong>ion<br />

Something to Consider<br />

Using different methods to cre<strong>at</strong>e the topob<strong>at</strong>hy<br />

surface can introduce some bias and uncertainty.


Habit<strong>at</strong> Mapping<br />

High resolution elev<strong>at</strong>ion d<strong>at</strong>a, such as lidar, can produce a high level of<br />

detail for analyzing how n<strong>at</strong>ural and manmade thre<strong>at</strong>s such as sea level<br />

rise, drought, storm flooding, and development may affect a wetland.<br />

China Camp<br />

Typical marsh elev<strong>at</strong>ion p<strong>at</strong>tern<br />

Stege Marsh<br />

Atypical marsh elev<strong>at</strong>ion p<strong>at</strong>tern<br />

Ustin, 2007


Conclusion<br />

High resolution elev<strong>at</strong>ion d<strong>at</strong>a<br />

• Provides a solid base for coastal analysis<br />

• Provides valuable inform<strong>at</strong>ion and visualiz<strong>at</strong>ion capability<br />

to researchers and coastal managers<br />

• Can be used to predict inund<strong>at</strong>ion extents, visualize<br />

coastal change, establish a repe<strong>at</strong>able shoreline, and map<br />

habit<strong>at</strong>s


For More Inform<strong>at</strong>ion<br />

A Roadmap to a Seamless Topob<strong>at</strong>hy Surface<br />

A series of products to help users cre<strong>at</strong>e seamless coastal maps<br />

Includes:<br />

• D<strong>at</strong>a inventory<br />

• Topographic and B<strong>at</strong>hymetric<br />

D<strong>at</strong>a Consider<strong>at</strong>ions<br />

• Examples of coastal applic<strong>at</strong>ions<br />

www.csc.noaa.gov/topob<strong>at</strong>hy


Contact Inform<strong>at</strong>ion<br />

Lindy Betzhold or Rebecca M<strong>at</strong>aosky<br />

<strong>Lynne</strong>.Betzhold@noaa.gov<br />

Rebecca.M<strong>at</strong>aosky@noaa.gov

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