other high resolution imagery to further enhance the information on coral reef
structure, and exploiting the information that can be derived from LiDAR-derived
seafloor intensity surfaces. In the future, as the technology advances, and research
efforts continue to refine signal processing techniques and algorithms, the capabilities and products that can be derived from LiDAR will similarly improve and
expand.
Acknowledgments This chapter was made possible with contributions from Tim Battista
(NOAA Biogeography Branch), Alan M. Friedlander (University of Hawaii/USGS), Curt D.
Storlazzi (USGS), Michael E. Field and (USGS) and Christopher L. Conger. Support for the
authors was provided by NOAA’s Coral Reef Conservation Program.
Suggested Reading
Brock JC, Purkis SJ (2009) The emerging role of LiDAR remote sensing in coastal research and
resource management. J Coast Res SI 53:1–5
Conger CL, Fletcher CH, Hochberg EH, Frazer N, Rooney J (2009) Remote sensing of sand
distribution patterns across an insular shelf: Oahu, Hawaii. Mar Geo 267:175–190
Costa BM, Battista TA, Pittman SJ (2009) Comparative evaluation of airborne LiDAR and shipbased multibeam sonar bathymetry and intensity for mapping coral reef ecosystems. Remote
Sens Environ 113:1082–1100
Pittman SJ, Costa BM, Battista TA (2009) Using LiDAR bathymetry and boosted regression trees
to predict the diversity and abundance of fish and corals. J Coast Res 53(SI):27–38
Pittman SJ, Brown KA (2011) Multiscale approach for predicting fish species distributions across
coral reef seascapes. PLoS ONE 6(5):e20583. doi:10.1371/journal.pone.0020583
Storlazzi CD, Logan JB, Field ME (2003) Quantitative morphology of a fringing reef tract from
high-resolution laser bathymetry: Southern Molokai, Hawaii. Geol Soc Am Bull 115:1344
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