2022
DOI: 10.1029/2022jg006967
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Long‐Term Patterns of Dissolved Oxygen Dynamics in the Pearl River Estuary

Abstract: Hypoxia, defined as dissolved oxygen (DO) in water <2 mg L −1 , has occurred worldwide in estuarine and coastal environments during the past five decades (Breitburg et al., 2018;Zhang et al., 2010). Estuarine and coastal hypoxia not only alters regional biogeochemical processes and also affects biodiversity and fisheries, which have attracted considerable attention globally (

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Cited by 12 publications
(7 citation statements)
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References 75 publications
(130 reference statements)
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“…The low oxygen conditions have also remarkably deteriorated in the bottom waters of the lower estuary (Qian et al, 2018;Su et al, 2017;Zhao et al, 2020), even though its shallow topography (averaged depth of ~10 m) and relatively strong mixing (induced by tides and wind) physically make the estuary less prone to develop large-scale hypoxic events (Harrison et al, 2008). A significant decline in bottom-water oxygenation, at a rate of ~2 ± 0.9 µmol kg -1 yr -1 , has been observed in the lower estuary over the past three decades (Qian et al, 2018;Qian et al, 2022), with an expansion of the hypoxic area over the last two decades (Figure S5d). Two prominent hypoxic centers have been found with a total area of ~ 700 km 2 in the coastal transition zone off the estuary (Hu et al, 2021;Su et al, 2017;Yin et al, 2004;Zhao et al, 2020;Zhao et al, 2021).…”
Section: Pearl River Estuarymentioning
confidence: 99%
“…The low oxygen conditions have also remarkably deteriorated in the bottom waters of the lower estuary (Qian et al, 2018;Su et al, 2017;Zhao et al, 2020), even though its shallow topography (averaged depth of ~10 m) and relatively strong mixing (induced by tides and wind) physically make the estuary less prone to develop large-scale hypoxic events (Harrison et al, 2008). A significant decline in bottom-water oxygenation, at a rate of ~2 ± 0.9 µmol kg -1 yr -1 , has been observed in the lower estuary over the past three decades (Qian et al, 2018;Qian et al, 2022), with an expansion of the hypoxic area over the last two decades (Figure S5d). Two prominent hypoxic centers have been found with a total area of ~ 700 km 2 in the coastal transition zone off the estuary (Hu et al, 2021;Su et al, 2017;Yin et al, 2004;Zhao et al, 2020;Zhao et al, 2021).…”
Section: Pearl River Estuarymentioning
confidence: 99%
“…In some cold periods, the DO concentrations were recorded up to ~15.0 mg/L at a salinity of 31.6 and 7.8 • C of water temperature (30 March 2015; 158% supersaturation of DO). This hyperoxic condition is commonly observed in areas with high nutrient supply [38], as well as in the semi-enclosed bays, which are typical along the Korean coast [12,13,39].…”
Section: Surface Do Distributionmentioning
confidence: 91%
“…Nevertheless, there are currently not many studies on the spectral signature of DO in water due to several factors that influence oxygen availability, such as temperature, salinity, pH, and organic matter. DO concentrations were summarized and analyzed as the crucial drivers of hypoxia in Northwestern and Southern Hong Kong and Mirs Bay over the past three decades [20].…”
Section: Related Workmentioning
confidence: 99%