Guan, ShoudeShoudeGuanHuang, MengyaMengyaHuangLin, I-II-ILinWu, HuiHuiWuLin, YaotingYaotingLinWu, ZiyiZiyiWuZhang, YihanYihanZhangJin, Fei-FeiFei-FeiJinWang, WeiliWeiliWangHong, XinXinHongLi, ChengChengLiLiu, ZhenminZhenminLiuLin, XiaopeiXiaopeiLinZhao, WeiWeiZhaoTian, JiweiJiweiTian2025-12-192025-12-192025-05-02https://www.scopus.com/pages/publications/105004073226https://scholars.lib.ntu.edu.tw/handle/123456789/734803Riverine plumes greatly shape ocean environments and ecosystems. The Changjiang River plume, widely spreading in the Yellow and East China Seas in summer, induces extremely low surface salinity and threatens local aquaculture and fisheries. Passage of tropical cyclones potentially increases surface salinity by stirring upper oceans, yet the extent of cyclones’ effects on the Changjiang River Plume extension and its mechanisms remains less explored. Here, combining satellite and in-situ observations with numerical experiments, we reveal a widespread surface salinification induced by Lekima (2019), with the maximum salinification reaching 6.5 psu and an 83% Changjiang River Plume contraction. Tropical cyclone-induced vertical mixing contributes to this dramatic salinification, while horizontal advection can either contribute to or offset the salinification, depending on specific locations. Further examination of surface salinity during 2015–2022 suggests that tropical cyclones can effectively restrict the Changjiang River Plume extension, potentially shielding fishing and aquaculture industries from low-salinity-related disasters.ChinaEast China SeaPacific OceanYangtze RiverYellow Seanumerical modelsalinizationsatellite imagerysea surface salinitytropical cyclone[SDGs]SDG13[SDGs]SDG14journal article10.1038/s43247-025-02317-x