2015
DOI: 10.1117/1.jrs.9.096024
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Hourly turbidity monitoring using Geostationary Ocean Color Imager fluorescence bands

Abstract: Abstract. The Geostationary Ocean Color imager (GOCI) is the first geostationary ocean color satellite sensor that collects hourly images eight times per day during daylight. This high frequency image acquisition makes it possible to study more detailed dynamics of red tide blooms, sediment plumes, and colored dissolved organic matter plumes, and can aid in the prediction of biophysical phenomena. We apply the red band difference and the fluorescence line height algorithms to GOCI imagery to separate waters wi… Show more

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Cited by 5 publications
(5 citation statements)
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References 34 publications
(58 reference statements)
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“…GOCIs produce eight images at a 500 m spatial resolution and hourly interval from 8:15 a.m. to 3:45 p.m. local time every day, and the images cover eight spectral bands with blue to near-infrared wavelengths [22]. Due to their wide coverage and high spatiotemporal resolution, the GOCI data have been used to study the optical characteristics of water [21,23,24], ocean surface currents [25][26][27][28], biological features of waters [29][30][31], water quality [32][33][34], harmful algal bloom [35,36], sea surface salinity [37], and sea fog [38]. However, these high-quality data have not yet been applied to the characteristics of Bohai Sea ice, where fast-changing first-year ice poses challenges for traditional satellites.…”
Section: Bandmentioning
confidence: 99%
“…GOCIs produce eight images at a 500 m spatial resolution and hourly interval from 8:15 a.m. to 3:45 p.m. local time every day, and the images cover eight spectral bands with blue to near-infrared wavelengths [22]. Due to their wide coverage and high spatiotemporal resolution, the GOCI data have been used to study the optical characteristics of water [21,23,24], ocean surface currents [25][26][27][28], biological features of waters [29][30][31], water quality [32][33][34], harmful algal bloom [35,36], sea surface salinity [37], and sea fog [38]. However, these high-quality data have not yet been applied to the characteristics of Bohai Sea ice, where fast-changing first-year ice poses challenges for traditional satellites.…”
Section: Bandmentioning
confidence: 99%
“…The nflh algorithm, for example, uses 748 nm for Band 3, which is over 60 nm away from the fluorescence peak. Such a distant anchor point works reasonably well for average Chlorophyll waters (Figure 3A), but produces an order of magnitude higher nflh under high suspended sediment load with no fluorescence peak (Figure 3B) (e.g., Zhao and Ghedira, 2014;Amin and Shulman, 2015).…”
Section: Band Mathmentioning
confidence: 74%
“…Water clarity is a critical parameter for the optical properties of ICWs [146,[164][165][166][167], vital for characterizing the turbidity and absorption/scattering of light by water bodies. It directly relates to the inherent optical properties of waterbodies, such as Chla, SPM, and phytoplankton biomass [168][169][170][171][172][173].…”
Section: Water Claritymentioning
confidence: 99%