2019
DOI: 10.1016/j.ecss.2019.03.006
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Between the tides: Modelling the elevation of Australia's exposed intertidal zone at continental scale

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Cited by 78 publications
(43 citation statements)
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“…Various applications of this method have been attempted, including the monitoring of coastline changes [10], estimation of sediment transport [11], and data assimilation in a coastal morphodynamic model [12]. At larger scale, Bishop-Taylor et al developed an intertidal digital elevation model (DEM) for Australia coast at 25 m resolution using a relative intertidal extent model developed from 30 years of Landsat archive and global tidal modeling [13,14].…”
Section: Introductionmentioning
confidence: 99%
“…Various applications of this method have been attempted, including the monitoring of coastline changes [10], estimation of sediment transport [11], and data assimilation in a coastal morphodynamic model [12]. At larger scale, Bishop-Taylor et al developed an intertidal digital elevation model (DEM) for Australia coast at 25 m resolution using a relative intertidal extent model developed from 30 years of Landsat archive and global tidal modeling [13,14].…”
Section: Introductionmentioning
confidence: 99%
“…This data is available as atmospherically and terrain corrected 'analysis-ready' data processed to surface reflectance, allowing reliable spectra to be extracted with no additional processing or calibration required [44]. We focused on five commonly studied environments to explore the influence of contrasting spectral properties on waterline extraction performance: a) sandy beaches [1,6,28,33,34,38,42], b) artificial shorelines [32,45], c) rocky shorelines [10,29,45], d) wetland vegetation [46][47][48], and Remote Sens. 2019, 11, 2984 5 of 23 e) tidal mudflats [7,10,19,49].…”
Section: Sample Spectra and Index Calculationmentioning
confidence: 99%
“…Initially, we computed a series of common water extraction indices. The normalised difference water index (NDWI, [50]) is one of the most commonly used remote sensing water indices, having been applied to facilitate waterline delineation in a wide range of papers across inland [23,24,26] and coastal environments [7,10,25,51]. This index ranges from -1.0 (land) to 1.0 (water), and uses the ratio of visible green and near-infrared (NIR) reflectance to separate water pixels from land based on water's high reflectance of visible green light and low reflectance of NIR, and the high reflectance of NIR by dry soil and terrestrial vegetation:…”
Section: Sample Spectra and Index Calculationmentioning
confidence: 99%
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