2005
DOI: 10.2112/03-0071.1
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Shoreline Definition and Detection: A Review

Abstract: BioOne Complete (complete.BioOne.org) is a full-text database of 200 subscribed and open-access titles in the biological, ecological, and environmental sciences published by nonprofit societies, associations, museums, institutions, and presses.

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Cited by 1,104 publications
(771 citation statements)
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References 21 publications
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“…The shoreline evolution was determined by superimposing the shorelines extracted from aerial The location of the shoreline was defined based on the previous high tide high water level (Boak and Turner, 2005). As a basic approximation, considering a 1:8 reflective slope with 1.7 m tide range, we can assume a lateral error of about 6.8 m on the shoreline detection.…”
Section: Shoreline Variationmentioning
confidence: 99%
“…The shoreline evolution was determined by superimposing the shorelines extracted from aerial The location of the shoreline was defined based on the previous high tide high water level (Boak and Turner, 2005). As a basic approximation, considering a 1:8 reflective slope with 1.7 m tide range, we can assume a lateral error of about 6.8 m on the shoreline detection.…”
Section: Shoreline Variationmentioning
confidence: 99%
“…Third-grade 193 polynomic correction with two-dimensional ground control points (GCPs) was used for 194 photo georeferencing in ESRI® ArcGIS 9.3 software. GCPs were carefully chosen 195 feature that can serve as a shoreline indicator or proxy, so that it properly reflects real 204 shoreline position and evolution (Moore, 2000;Boak and Turner, 2005). In this work 205 the high-water line (HWL) and the dune foot were used as shoreline proxies.…”
Section: Approximate Position Of Table 1 188 189mentioning
confidence: 99%
“…In this work 205 the high-water line (HWL) and the dune foot were used as shoreline proxies. The HWL 206 constitutes the most widely used shoreline proxy (Boak and Turner, 2005), and is 207 usually considered equivalent to the last high tide mark or the wet/dry line identifiable 208 on beach sand on the photographs (Crowell et al, 1997). Despite its limitations 209 regarding short-term variability, it is generally deemed as a valid indicator of shoreline 210 position (Gorman et al, 1998), and so it was used along the whole Atlantic coast of 211…”
Section: Approximate Position Of Table 1 188 189mentioning
confidence: 99%
“…Shoreline is the line where the land and water bodies meet and is called boundary separation between both (Boak and Turner, 2005;Dolan et al, 1991). In the coastal area, it is considered to be one of the most dynamic regions because it is mainly attributed to the natural Earth phenomena such as tide effect, wind speed, wind direction, sea level rise, natural disaster and anthropogenic processes (Mustaqim et al, 2014;Luu et al, 2015;Li, et al, 2002).…”
Section: Introductionmentioning
confidence: 99%
“…Before shoreline is acquired, we have to determine the shoreline indicator which represents the true shoreline position. The shoreline indicators are categorized into three groups: Detectable visually features, tidal datum-based indicators and indicators based on processing method to extract shoreline (Boak and Turner, 2005;Li et al, 2002;Gens, 2010).…”
Section: Introductionmentioning
confidence: 99%