This document discusses the use of LIDAR (Light Detection and Ranging) to analyze topographic changes caused by hurricanes. LIDAR uses light pulses to map surface elevations from aircraft. It was used to map areas in North Carolina before and after Hurricane Irene, allowing scientists to identify regions of erosion (shown in red) and accretion (shown in blue). Specifically, LIDAR data and aerial photographs of an area called "Location 1" on the Core Banks before and after the hurricane show widespread shoreline retreat and overwash deposits from storm waves and surge.
1. Overview
• What is LIDAR
• Example (schematic) LIDAR return and
interpretation
• Map of sites to be analyzed (1 shown here, 2-
5 as student exercises)
• Aerial photograph comparison of before and
after Hurricane Irene for the North Carolina
“Location 1”
2. What is LIDAR?
• Airborne Laser Altimeters, or LIDAR
(for light detection and ranging) use
light to measure distance from
plane to surface and back.
• Detailed (every few meters)
mapping of topographic surfaces
before and after an event allows
scientists to measure the changes.
• The image shown is from the
Experimental Advanced Airborn
Research LIDAR (EAARL) which is
adapted for coastal systems. More
information is available at
http://ngom.usgs.gov/dsp/tech/eaa
rl/
3. LIDAR can be used to map the canopy and the ground
surface, and in shallow water, the depth.
http://ngom.usgs.gov/dsp/tech/alps/images/fig2_waveform_resolving.JPG from Wright and
Brock, 2002
4. Location index for pre-storm and post-storm LIDAR elevations for the Outer Banks, NC.
Each location includes pre- and post-storm topography as well as topographic change. The
green line shows Hurricane Irene’s track. http://coastal.er.usgs.gov/hurricanes/irene/lidar/
On the elevation images below, red colors indicate topographic highs, while blues indicate
topographic lows. The differences between the pre- and post-storm elevation data sets show
where significant changes have occurred. Red colors indicate erosion. For example, oranges and
reds on the seaward side of the islands indicate wide-spread shoreline retreat. (In each image,
the Atlantic Ocean is on the bottom right.) Blue colors show areas of accretion, such as
overwash deposits where waves and surge have moved sand landward.
5. Location 1, Core
Banks, NC, Pre- and
Post Storm Aerial
Photographs,
courtesy of the
USGS
http://coastal.er.usg
s.gov/hurricanes/ire
ne/photo-comparisons/
6. Location 1, Core Banks, NC Pre-Storm
(August 11-15 2009)
RED = HIGH, BLUE = LOW
http://coastal.er.usgs.gov/hurricanes/irene/photo-comparisons/
7. Location 1, Core Banks, NC Post-Storm (August 28, 2011)
RED = HIGH, BLUE = LOW
http://coastal.er.usgs.gov/hurricanes/irene/photo-comparisons/
8. Location 1, Core Banks, NC Difference between Pre- and Post-Storm
RED = EROSION, BLUE = ACCRETION
http://coastal.er.usgs.gov/hurricanes/irene/photo-comparisons/
Editor's Notes
Location 1: LIDAR topography from August 11-15, 2009 (pre-storm) and August 28, 2011 (post-storm) and topographic change (difference) for a portion of Core Banks, NC. “A relatively low beach section near the center of the pre-storm image likely indicates where breaches have been cut through the barrier island at previous times. The Irene breach is clearly seen in the post-storm LIDAR data. The difference image shows over 1 m of vertical erosion in the beaches that were breached.” See pre- and post-storm photo comparisons at [http://coastal.er.usgs.gov/hurricanes/irene/photo-comparisons/] for additional discussion. [http://coastal.er.usgs.gov/hurricanes/irene/lidar/]
Location 1: LIDAR topography from August 11-15, 2009 (pre-storm) and August 28, 2011 (post-storm) and topographic change (difference) for a portion of Core Banks, NC. “A relatively low beach section near the center of the pre-storm image likely indicates where breaches have been cut through the barrier island at previous times. The Irene breach is clearly seen in the post-storm LIDAR data. The difference image shows over 1 m of vertical erosion in the beaches that were breached.” See pre- and post-storm photo comparisons at [http://coastal.er.usgs.gov/hurricanes/irene/photo-comparisons/] for additional discussion. [http://coastal.er.usgs.gov/hurricanes/irene/lidar/]
Location 1: LIDAR topography from August 11-15, 2009 (pre-storm) and August 28, 2011 (post-storm) and topographic change (difference) for a portion of Core Banks, NC. “A relatively low beach section near the center of the pre-storm image likely indicates where breaches have been cut through the barrier island at previous times. The Irene breach is clearly seen in the post-storm LIDAR data. The difference image shows over 1 m of vertical erosion in the beaches that were breached.” See pre- and post-storm photo comparisons at [http://coastal.er.usgs.gov/hurricanes/irene/photo-comparisons/] for additional discussion. [http://coastal.er.usgs.gov/hurricanes/irene/lidar/]