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Lidar (light detection and ranging), also known as scanning laser altimetry, is an airborne terrain mapping system, which is analogous to radar (radio detection and ranging) in its principle of operation. The system is usually fitted to a helicopter or fixed-wing aircraft, and by measuring the time taken for laser pulses to hit the ground and return, the distance to the ground directly under the flight path can be calculated. By scanning the laser perpendicular to the line of flight, the system can survey a swath some 250-700 m wide beneath the flight path. The compilation of multiple swaths allows the generation of a digital elevation model (DEM). Computer software can be used to extract topographic cross-sections and calculate sediment volumes, while comparison of successive surveys allow the rate and extent of topographic change to be computed. The examples below show the results of a lidar survey of the Alde-Ore estuary in 2003.
Beach volumes at 16 points on the coastline, calculated
from the lidar data. Click here for a summary of our coastal projects Recent Publications Pye,
K. and Blott, S.J.
(2006). Coastal processes and morphological change in the Dunwich - Sizewell
area, Suffolk, UK. Journal of Coastal Research 22, 453-473. Saye, S.E., van der
Wal, D., Pye,
K. and Blott, S.J.
(2005). Beach dune morphological relationships and erosion/accretion: an
investigation at five sites in England and Wales using LIDAR data. Geomorphology
72, 128-155. Blott, S.J.
and
Pye, K. (2004). Application of lidar digital terrain modelling to predict intertidal habitat
development at a managed retreat site: Abbotts Hall, Essex, UK. Earth Surface
Processes and Landforms 29, 893-905. Blott,
S.J.
and Pye, K.
(2004). Morphological and sedimentological changes on an artificially
nourished beach, Lincolnshire, UK. Journal of Coastal Research 20,
214-233. van der
Wal, D., Pye,
K. and Neal, A. (2002). Long-term morphological
change in the Ribble Estuary, northwest England. Marine
Geology 189, 249-266. |
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