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- W2314542023 abstract "The Oregon Coast can be divided into compartments by large headlands forming littoral cells that restrict the flow of sediments. Most of these sediments have reached a state of equilibrium controlled largely by the relative sea level rise and disrupted only by episodic storm events, man made changes to the sediment supply, and climatic shifts such as El Nino and La Nina. Shoreline change occurs on spatial scales of centimeters to kilometers and operates on time scales ranging from seconds to decades. As a result of new high-resolution LIDAR technologies, we are able to identify and quantify these large-scale changes and examine some of the smaller scale changes. Erosion on the Oregon coast caused by the 1997–98 El Nino event produced an observable pattern of shoreline change. In October of 1997 and then again in April of 1998, LIDAR was flown over the Oregon Coast, bracketing the El Nino and enabling us to quantify the erosion at a variety of scales. The objective of this paper is to show how different applications of LIDAR are used to perform shoreline change analyses in Oregon; the Netarts Littoral Cell in the north and the Bandon Littoral Cell in the south. The results of these shoreline change analyses have implications for coastal management issues and have facilitated regional hazard planning." @default.
- W2314542023 created "2016-06-24" @default.
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- W2314542023 date "2002-02-21" @default.
- W2314542023 modified "2023-09-22" @default.
- W2314542023 title "An Application of Lidar to Multiple Scales of Shoreline Change in Oregon" @default.
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- W2314542023 doi "https://doi.org/10.1061/40605(258)52" @default.
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