Role of Freshwater-Driven Stratification in Bottom Cold Water Intrusion in the Southeastern Yellow Sea
编号:1088 访问权限:仅限参会人 更新:2026-08-31 22:21:02 浏览:0次 口头报告

报告开始:暂无开始时间(Asia/Shanghai)

报告时间:暂无持续时间

所在会场:[暂无会议] [暂无会议段]

暂无文件

摘要
In the southeastern Yellow Sea, the summer intrusion of bottom cold water induces temperature fluctuations in the coastal bottom layer, which are closely linked to regional fisheries productivity. Therefore, it is important to analyze the physical factors driving the onshore intrusion of bottom cold water. This study utilizes the Finite Volume Community Ocean Model (FVCOM) to analyze the relationship between summer freshwater discharge from major rivers along the Korean west coast, including the Han, Geum, and Yeongsan Rivers, and the onshore intrusion of bottom cold water over the period 2019–2023. Among the study years, the two years with the highest freshwater discharge were designated as high-discharge periods (2020, 2023), and the two years with the lowest discharge were designated as low-discharge periods (2019, 2021). Model results indicate that during high-discharge periods, the horizontal density gradient in the direction from the estuary toward the open sea increases compared to low-discharge periods. This enhanced density gradient drives an onshore bottom flow through density-induced circulation, where the offshore surface plume is compensated by the onshore flow at depth. Flux analysis shows that onshore bottom velocity and volume flux increase during high-discharge periods relative to low-discharge periods, serving as the primary mechanism for accelerated onshore transport of bottom cold water. Consequently, bottom cold water intrudes further onshore during high-discharge periods compared to low-discharge periods, resulting in a decrease in coastal bottom water temperatures. However, the extent of this bottom cold water intrusion may be reinforced or suppressed depending on wind direction and intensity, suggesting that the combined effects of freshwater discharge and wind stress need to be considered together. In conclusion, this study demonstrates that freshwater discharge from rivers along the Korean west coast is an important physical factor regulating coastal bottom water temperature variability in the southeastern Yellow Sea, and may serve as foundational data for understanding future variability in the coastal fisheries environment.

This research was a part of the project titled 'BEACON for Future Marine Workforce : Integrating Spatial and Resource Utilization(RS-2025-02220608)', funded by the Ministry of Oceans and Fisheries, Korea.
 
关键词
暂无
报告人
Minwoo Park
Student Department of Ocean Science, Inha University

稿件作者
Minwoo Park Department of Ocean Science, Inha University
发表评论
验证码 看不清楚,更换一张
全部评论
重要日期
  • 会议日期

    01月12日

    2027

    01月15日

    2027

  • 07月21日 2026

    初稿截稿日期

  • 01月15日 2027

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University (MEL)
Department of Earth Sciences, National Natural Science Foundation of China (NSFC)
联系方式
历届会议
移动端
在手机上打开
小程序
打开微信小程序
客服
扫码或点此咨询