2018
DOI: 10.1016/j.rse.2018.03.024
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An algorithm for optically-deriving water depth from multispectral imagery in coral reef landscapes in the absence of ground-truth data

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Cited by 94 publications
(62 citation statements)
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“…While correction schemes by Gordon (1997), Chavez (1988), and others effectively reduce atmospheric effects, the physics-based algorithms typically are unable to achieve depth estimates with root-mean-square errors less than ∼1-2 m in shallow waters ≤20 m (Adler-Golden et al, 2005;Lyzenga et al, 2006). Kerr and Purkis (2018) provide a bridge between the empirical and physics-based approaches, coupling forward modeling of the water column (Lee et al, 1999) with the ratio algorithm of Stumpf et al (2003) that is widely applied in empirical studies. The model of Kerr and Purkis (2018) enables the estimation of water depths up to 15 m in tropical carbonate environments without the need for in situ water depth measurements as calibration data, an important result considering that the lack of ground truth data often is the primary obstacle for estimating bathymetry in shallow-water environments.…”
Section: 1029/2018ea000539mentioning
confidence: 99%
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“…While correction schemes by Gordon (1997), Chavez (1988), and others effectively reduce atmospheric effects, the physics-based algorithms typically are unable to achieve depth estimates with root-mean-square errors less than ∼1-2 m in shallow waters ≤20 m (Adler-Golden et al, 2005;Lyzenga et al, 2006). Kerr and Purkis (2018) provide a bridge between the empirical and physics-based approaches, coupling forward modeling of the water column (Lee et al, 1999) with the ratio algorithm of Stumpf et al (2003) that is widely applied in empirical studies. The model of Kerr and Purkis (2018) enables the estimation of water depths up to 15 m in tropical carbonate environments without the need for in situ water depth measurements as calibration data, an important result considering that the lack of ground truth data often is the primary obstacle for estimating bathymetry in shallow-water environments.…”
Section: 1029/2018ea000539mentioning
confidence: 99%
“…Kerr and Purkis (2018) provide a bridge between the empirical and physics-based approaches, coupling forward modeling of the water column (Lee et al, 1999) with the ratio algorithm of Stumpf et al (2003) that is widely applied in empirical studies. The model of Kerr and Purkis (2018) enables the estimation of water depths up to 15 m in tropical carbonate environments without the need for in situ water depth measurements as calibration data, an important result considering that the lack of ground truth data often is the primary obstacle for estimating bathymetry in shallow-water environments. An application of the Kerr and Purkis (2018) method to RapidEye imagery from Andros Island yields a root-mean-squared error of of 1.43 m in regions shallower than 15 m (Kerr & Purkis, 2018).…”
Section: 1029/2018ea000539mentioning
confidence: 99%
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