Abstract
Flood events significantly increase water discharges and terrigenous material inputs to coastal waters. Riverine nutrients in the Changjiang Estuary are transported by the dispersion of Changjiang Diluted Water (CDW) plumes and detached low-salinity water patches. However, the effects of flooding on nutrient offshore transports have not been well explored. Here, we present the nutrient conditions in the Changjiang Estuary and adjacent East China Sea in the historical flooding year 2020. Comparisons of nutrient distributions between flooding years, drought year and non-flooding years were also made. Our results showed that nitrate flux from the Changjiang River in August 2020 was 1.5 times that of the multi-year averaged flux in non-flooding years. Enormous riverine nutrient input resulted in much higher nutrient concentrations in the outer estuary than those in non-flooding years. In addition, a detached low-salinity water patch was observed, which made the salinity of the northern estuary even lower than that in the historical flooding year 1998. Surface dissolved inorganic nitrate (DIN) level in the low-salinity water patch was even ~16 times of that at nearby station in the drought year 2006. While phosphate (PO43−) concentrations were less than 0.1 μmol L−1 east of 123°E, which was probably caused by intensive biological uptake, as indicated by a high Chlorophyll a (Chl a) concentration (29.08 μg L−1). The depleted PO43− and high N/P of the low-salinity water patch suggested PO43− limitation even under flood conditions. A three end-member mixing model was adopted to identify the contributions of the CDW end-member (CDWend-member) and biological process to nutrient distributions. Our model results showed that the nutrient contribution of the CDWend-member to the estuary (122–124°E, 31–32.5°N) in flooding year 2020 was over double that in drought year 2006. Model-derived biological DIN uptake was as high as 24.65 μmol L−1 at the low-salinity water patch. Accordingly, the estimated net community production was 566–1131 mg C m−2 d−1 within the euphotic zone. The offshore transport of a low-salinity, high-DIN water patch during flooding could probably have a significant influence on biogeochemical cycles in the broad shelf, and even the adjacent Japan Sea.
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References
87
[1]
Anderson "Redfield ratios of remineralization determined by nutrient data analysis. global. biogeochem" Cycles (1994) 10.1029/93gb03318
[2]
Bai "Summertime changjiang river plume variation during 1998–2010" J. Geophys. Res. Oceans. (2014) 10.1002/2014jc009866
[3]
Beardsley "Discharge of the changjiang (Yangtze river) into the East China sea. cont" Shelf. Res. (1985) 10.1016/0278-4343(85)90022-6
[4]
Cao "Dynamics of the carbonate system in a large continental shelf system under the influence of both a river plume and coastal upwelling" J. Geophys. Res. (2011) 10.1029/2010jg001596
[5]
Chang "A numerical study on the changjiang diluted water in the yellow and East China seas" J. Geophys. Res. (2003) 10.1029/2002jc001749
[6]
Chang "Summer behavior of the changjiang diluted water to the East/Japan Sea: A modeling study in 2003" Cont. Shelf. Res. (2014) 10.1016/j.csr.2014.03.007
[7]
2022
[8]
Chen "The kuroshio intermediate water is the major source of nutrients on the East China Sea continental shelf" Oceanol. Acta (1996)
[9]
Chen "Chemical and physical fronts in the bohai, yellow and East China seas" J. Mar. Syst. (2009) 10.1016/j.jmarsys.2008.11.016
[10]
Chen "The behavior of nitrate and phosphate in changjiang river estuary and its adjacent East China Sea during summer of 2009 (in Chinese)" J. Mar. Sci. (2011)
[11]
Chen "Hypoxia in the East China Sea: One of the largest coastal low-oxygen areas in the world" Mar. Environ. Res. (2007) 10.1016/j.marenvres.2007.01.007
[12]
Chen "Redfield ratios and regeneration rates of particulate matter in the Sea of Japan as a model of closed system" Geophys. Res. Lett. (1996) 10.1029/96gl01676
[13]
Chen "Composition and supply of inorganic and organic nitrogen species in dry and wet atmospheric deposition: Use of organic nitrogen composition to calculate the ocean’s external nitrogen flux from the atmosphere" Cont. Shelf. Res. (2021) 10.1016/j.csr.2020.104316
[14]
Chen "Exchange of water masses between the East China Sea and the kuroshio off northeastern Taiwan" Cont. Shelf. Res. (1995) 10.1016/0278-4343(93)e0001-o
[15]
Chen "Effects of the changjiang (Yangtze) river discharge on planktonic community respiration in the East China Sea" J. Geophys. Res. Oceans (2009) 10.1029/2008jc004891
[16]
Chen "Impact of upwelling on phytoplankton blooms and hypoxia along the Chinese coast in the East China Sea" Mar. pollut. Bull. (2021) 10.1016/j.marpolbul.2021.112288
[17]
Chen "Physical mechanisms for the offshore detachment of changjiang diluted water in the East China Sea" J. Geophys. Res. Ocean (2008) 10.1029/2006jc003994
[18]
Chen "Nutrient concentrations and fluxes in the changjiang estuary during summer" Acta Oceanol. Sin. (2010) 10.1007/s13131-010-0029-8
[19]
Froelich "Kinetic control of dissolved phosphate in natural rivers and estuaries" Limnol. Oceanogr. (1988) 10.4319/lo.1988.33.4_part_2.0649
[20]
Gao "Using water age to study the biogeochemistry of nutrients in a large-river estuary and the adjacent shelf area" J. Mar. Res. (2021)
[21]
Gong "Chemical hydrography and chlorophyll a distribution in the East China Sea in summer: implications in nutrient dynamics" Cont. Shelf. Res. (1996) 10.1016/0278-4343(96)00005-2
[22]
Gong "Yangtze River floods enhance coastal ocean phytoplankton biomass and potential fish production" Geophys. Res. Lett. (2011) 10.1029/2011gl047519
[23]
Gong "Prediction of nitrate concentration from two end member mixing in the southern East China Sea" Cont. Shelf. Res. (1995) 10.1016/0278-4343(94)00039-p
[24]
Grasshoff (1999) 10.1002/9783527613984
[25]
Guo "Air-sea CO2 fluxes in the East China Sea based on multiple-year underway observations" Biogeosciences (2015) 10.5194/bg-12-5495-2015
[26]
Han "Nutrients dynamics and biological consumption in a large continental shelf system under the influence of both a river plume and coastal upwelling" Limnol. Oceanogr. (2012) 10.4319/lo.2012.57.2.0486
[27]
Hirabayashi "Global flood risk under climate change" Nat. Clim. Change (2013) 10.1038/nclimate1911
[28]
Ichikawa "The current system in the yellow and East China seas" J. Oceanogr. (2002) 10.1023/a:1015876701363
[29]
Kim "Contribution of ocean current to the increase in n abundance in the northwestern pacific marginal seas" Geophys. Res. Lett. (2013) 10.1029/2012gl054545
[30]
Largier "Estuarine fronts-how important are they" Estuaries (1993) 10.2307/1352760
[31]
Li "Contribution of outer-shelf deep water to the nutrient inventories in the euphotic zone of the changjiang river plume during summer" J. Coast. Res. (2016) 10.2112/jcoastres-d-15-00056.1
[32]
Lie "Structure and eastward extension of the changjiang river plume in the East China Sea" J. Geophys. Res. Oceans. (2003) 10.1029/2001jc001194
[33]
Li "Effects of dual fronts on the spatial pattern of chlorophyll-a concentrations in and off the changjiang river estuary" Estuaries Coasts. (2021) 10.1007/s12237-020-00893-z
[34]
Liu (2021)
[35]
Liu "Progress on circulation dynamics in the East China Sea and southern yellow Sea: Origination, pathways, and destinations of shelf currents" Prog. Oceanogr. (2021) 10.1016/j.pocean.2021.102553
[36]
Liu "Nutrient budgets for large Chinese estuaries" Biogeosciences (2009) 10.5194/bg-6-2245-2009
[37]
Liu "Nutrient dynamics from the changjiang (Yangtze river) estuary to the East China Sea" J. Mar. Syst. (2016) 10.1016/j.jmarsys.2015.05.010
[38]
Liu "Dispersal and fate of dredged materials disposed of in the changjiang estuary determined by use of an in situ rare earth element tracer" China. Ocean. Eng. (2011) 10.1007/s13344-011-0040-7
[39]
Mao "A preliminary study of the Yangtze diluted water and its mixing process (in Chinese)" Oceanol. Limnol. Sin. (1963)
[40]
Meng "Distribution, mixing behavior, and transformation of dissolved inorganic phosphorus and suspended particulate phosphorus along a salinity gradient in the changjiang estuary" Mar. Chem. (2015) 10.1016/j.marchem.2014.09.016
[41]
Moon "Offshore detachment process of the low-salinity water around changjiang bank in the East China Sea" J. Phys. Oceanogr. (2010) 10.1175/2010jpo4167.1
[42]
Ning "Physical-biological oceanographic coupling influencing phytoplankton and primary production in the south China Sea" J. Geophys. Res. (2004) 10.1029/2004jc002365
[43]
Ning "Standing stock and production of phytoplankton in the estuary of the changjiang river (Yangtze river) and adjacent East China Sea" Mar. Ecol. Prog. Ser. (1988) 10.3354/meps049141
[44]
Pu "A preliminary study on expansion mechanism of the changjiang diluted water in summer" J. Mar. Sci. (1983)
[45]
Redfield (1963)
[46]
Ren "Analyzing dynamic characteristics of river plume in the modaomen mouth, pearl river estuary" J. Oceanogr (2020) 10.1007/s10872-020-00542-w
[47]
Saba "Toward a better understanding of fish-based contribution to ocean carbon flux" Limnol. Oceanogr. (2021) 10.1002/lno.11709
[48]
Shen "Preliminary study on the changjiang river mainstream nutrients fluxes (in Chinese)" Oceanol. Limnol. Sin. (1997)
[49]
Shen "An estimation on budget and control of phosphorus in the changjiang river catchment" Ennviron. Monit. Assess. (2012) 10.1007/s10661-011-2435-6
[50]
Shen "Transfer and transport of phosphorus and silica in the turbidity maximum zone of the changjiang estuary" Estuari. Coast. Shelf. Sci. (2008) 10.1016/j.ecss.2008.01.010

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Published
Jan 27, 2023
Vol/Issue
10
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Funding
National Natural Science Foundation of China Award: U1709201, 42276046, 41806095, 41706120
Cite This Article
Qianwen Sun, Dewang Li, Bin Wang, et al. (2023). Massive nutrients offshore transport off the Changjiang Estuary in flooding summer of 2020. Frontiers in Marine Science, 10. https://doi.org/10.3389/fmars.2023.1076336
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