2022
DOI: 10.1016/j.ecoenv.2022.113223
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Short-term changes in algal blooms and phytoplankton community after the passage of Super Typhoon Lekima in a temperate and inner sea (Bohai Sea) in China

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Cited by 32 publications
(9 citation statements)
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“…The number of observation points at different layers in each characteristic month from 2016 to 2018 is shown in Table 1. The sampling locations in this study are all over the Bohai Sea, and the number of observation sites in each month is more than 300, far more than that in previous studies (Zhang et al, 2017;Pei et al, 2019;Xie et al, 2021;Jiang et al, 2022).…”
Section: Observation Datamentioning
confidence: 90%
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“…The number of observation points at different layers in each characteristic month from 2016 to 2018 is shown in Table 1. The sampling locations in this study are all over the Bohai Sea, and the number of observation sites in each month is more than 300, far more than that in previous studies (Zhang et al, 2017;Pei et al, 2019;Xie et al, 2021;Jiang et al, 2022).…”
Section: Observation Datamentioning
confidence: 90%
“…Moreover, the total Chl-a in LZB and CBS are higher in 2018 than that in the previous two years, possibly due to typhoon "Wimbiya" which started on August 19th. After the typhoon, the concentration of dissolved inorganic nitrogen and dissolved inorganic silicon in the surface increased, which led to the increase of Chl-a concentration in the surface (Jiang et al, 2022). In October, the total Chl-a in BHB and LDB decreases significantly from 2016 to 2018, while its change in LZB and CBS is not obvious.…”
Section: Marine Ecological Environment Assessment In Four Sub-regions...mentioning
confidence: 99%
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“…For example, phytoplankton responses to increased nutrient supplies during TC periods are widely observed compared with non‐TC periods, despite TC passages in summer and autumn affecting phytoplankton dynamics differently (Ko et al., 2016, 2017; Zhao et al., 2008). After TCs, large amounts of dissolved nutrients frequently occur due to runoff and hydrological alteration, e.g., currents and upward mixing, are induced, which probably limit phytoplankton growth (Baleani et al., 2021; Havens et al., 2011; Jiang et al., 2022; Stockwell et al., 2020). Moreover, TCs show significant associations with gelatinous and carnivorous zooplankton at varying time intervals (López‐López et al., 2012), but an understanding of how they affect a planktonic food chain is lacking because of limited plankton indices derived from a single trophic level, e.g., focusing merely on phytoplankton or zooplankton (Chai et al., 2021; Ko et al., 2016; López‐López et al., 2012).…”
Section: Introductionmentioning
confidence: 99%
“…The natural disasters in the SCBHS mostly result from storm surges. The catastrophic storms in the Bohai Sea usually occur in summer and autumn, on an average frequency of once every 4 years, and smaller storms happen on the average frequency of 1-2 times a year, yet which have caused inestimable losses (Feng et al, 2018;Jiang et al, 2022). In particular, the coastal regions of the Bohai Bay and Laizhou Bay have undergone several severe storm disasters.…”
Section: Introductionmentioning
confidence: 99%