“…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).…”