2019
DOI: 10.1016/j.rse.2019.111302
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Adaptive bathymetry estimation for shallow coastal waters using Planet Dove satellites

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Cited by 108 publications
(71 citation statements)
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References 58 publications
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“…With below-surface reflectance calculated, water bathymetry was predicted using an adaptive bathymetry estimation method with self-tuning parameters (m 0 , m 1 ) as described in Li et al [20]: H = m 0 ln(1000 * r rs blue) ln(1000 * r rs green) − m 1 ,…”
Section: Of 16mentioning
confidence: 99%
“…With below-surface reflectance calculated, water bathymetry was predicted using an adaptive bathymetry estimation method with self-tuning parameters (m 0 , m 1 ) as described in Li et al [20]: H = m 0 ln(1000 * r rs blue) ln(1000 * r rs green) − m 1 ,…”
Section: Of 16mentioning
confidence: 99%
“…The water is clear; thus, the energy arrives from the bottom through the water column and the water column is homogenous [89]. The relationship between the water-leaving reflectance and the depth is z = m· + n where m and n do not vary with depth (they are constant when the properties of the water column and the bottom are constant, too), but RBlue and RGreen do vary [60,90], since they are the reflectances below the surface with bottom influence and the reflectance below the surface without bottom influence (that is, in deep water), respectively.…”
Section: Satellite Datamentioning
confidence: 99%
“…where m and n do not vary with depth (they are constant when the properties of the water column and the bottom are constant, too), but R Blue and R Green do vary [60,90], since they are the reflectances below the surface with bottom influence and the reflectance below the surface without bottom influence (that is, in deep water), respectively. In this study, 22 Pleiades images-taken between 15 October 2012 and 5 December 2019-were used ( Table 2) ( Figure A1).…”
Section: Satellite Datamentioning
confidence: 99%
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“…These methods are inherently limited to the resolution of the satellite sensor, and are unable to resolve changes in waterline positions occurring at a scale of less than a whole pixel (e.g., 10 m for Sentinel-2 or 30 m for Landsat; [28]). Although high resolution satellite data from commercial providers such as Planet Labs and DigitalGlobe are increasingly available for these applications [29,30], these sources of data are typically prohibitively expensive to implement across regional to global extents, and lack either the temporal depth or systematic revisit frequency that are available for medium resolution satellite programs with coarser pixel resolutions (e.g., Landsat imagery available since 1972, [31]). Accordingly, there is a pressing need for the development of operational methods for extracting waterline information from freely available medium resolution satellite imagery at spatial scales relevant to coastal and environmental management.…”
Section: Introductionmentioning
confidence: 99%