华东师范大学学报(自然科学版) ›› 2025, Vol. 2025 ›› Issue (6): 141-151.doi: 10.3969/j.issn.1000-5641.2025.06.015

• • 上一篇    

杭州湾北岸登陆台风对长江口咸潮入侵的影响——以2024年9月台风“贝碧嘉”“普拉桑”为例

裘诚()   

  1. 上海市海洋监测预报中心, 上海 200062
  • 收稿日期:2025-06-13 接受日期:2025-08-05 出版日期:2025-11-25 发布日期:2025-11-29
  • 作者简介:裘 诚, 男, 博士, 高级工程师, 研究方向为河口海岸学. E-mail: 594393411@qq.com
  • 基金资助:
    国家重点研发计划 (2023YFC3206003)

Effects of typhoons landfalling on the north bank of Hangzhou Bay, Shanghai, on saltwater intrusion in the Changjiang River Estuary: A case study of typhoons “Bebinca” and “Pulasan” in September 2024

Cheng QIU()   

  1. Shanghai Marine Monitoring and Forecasting Centre, Shanghai 200062, China
  • Received:2025-06-13 Accepted:2025-08-05 Online:2025-11-25 Published:2025-11-29

摘要:

长江口咸潮入侵是威胁城市供水安全的关键问题, 尤其在台风与低径流量叠加的极端天气条件下风险加剧. 以2024年9月连续由杭州湾北岸登陆上海的台风“贝碧嘉”和“普拉桑”为例, 基于高分辨率三维河口咸潮入侵数值模型, 模拟台风对长江口咸潮入侵的差异化影响. 模拟结果表明, 台风“贝碧嘉”登陆期间, 向陆的风生环流显著增强北港咸潮正面上溯, 而南槽咸潮因向海的风生环流作用减弱. 相比之下, “普拉桑”因强度较弱且路径转向, 对北港正面入侵影响有限. 台风引发的短期风暴增水虽与大潮叠加, 但受限于持续时间, 对北支咸潮倒灌的促进作用不显著. 本研究揭示了长江口咸潮入侵对杭州湾北岸登陆台风的响应机制, 为极端天气下河口水源地精准防御台风叠加咸潮的复合型灾害提供科学依据.

关键词: 长江口, 咸潮入侵, 登陆台风, 风生环流, 数值模拟

Abstract:

Saltwater intrusion in the Changjiang River Estuary is generally considered a key threat to urban water supply security, and the risks may be exacerbated under the weather conditions of concurrent typhoons and low river discharge. Taking the successive landfalls of typhoons “Bebinca” and “Pulasan” along the north bank of Hangzhou Bay, Shanghai, in September 2024, as examples, we employed a high-resolution 3D estuarine saltwater intrusion numerical model to simulate the differential impacts of the typhoons on saltwater intrusion in the Changjiang River Estuary. The results indicated that whereas the onshore wind-driven circulation promoted a significant enhancement of the frontal intrusion upstream of saltwater in the North Channel during the landfall of typhoon “Bebinca,” the circulation weakened the saltwater intrusion in the South Passage. In contrast, given its less intense strength and deflected track, typhoon “Pulasan” had a comparatively limited impact on the frontal intrusion in the North Channel. Given their limited duration, the short-term storm surges induced by the typhoons, which coincided with spring tides, caused comparatively little saltwater spillover from the North Branch into the South Branch. The findings of this study reveal the response mechanisms of saltwater intrusion to the landfall of typhoons on the north bank of Hangzhou Bay. This will provide a scientific basis for defense against compound natural disasters involving the combined effects of typhoons and saltwater intrusion on urban water supplies under extreme climate conditions.

Key words: the Changjiang River Estuary, saltwater intrusion, landfalling typhoons, wind-driven circulation, numerical simulation

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