风和波浪对长江口盐水入侵的影响:数值模拟研究

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Zhengjin Tao, Yongping Chen, Shunqi Pan, Ao Chu, Chunyang Xu, Peng Yao, Samuel Rowely
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引用次数: 0

摘要

长江口的盐水入侵多发生在冬季,此时河水流量小,风浪大。然而,风浪对长江口盐水入侵的影响尚不清楚。本研究采用基于 Delft3D 的风-波-流耦合数值模式,研究了风浪对长江口咸潮入侵的影响。结果表明,强烈的北风会引起逆时针环流并减少分层,从而增强河口盐水入侵。然而,在风浪的共同作用下,北航道外侧的分层作用减弱,而北航道内侧的分层作用增强,从而导致河口盐分迁移量增加约 40%。这些结果突出表明,如果不考虑波浪,长江口的盐水入侵可能会被大大低估。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Influence of Wind and Waves on Saltwater Intrusion in the Yangtze Estuary: A Numerical Modeling Study

Saltwater intrusion occurs frequently in the Yangtze Estuary during winter, when the river discharges are low along with strong wind and waves. However, the influence of wind and waves on saltwater intrusion in the Yangtze Estuary remains unclear. This study uses a coupled wind-wave-current numerical model based on Delft3D to investigate the impacts of wind and waves on saltwater intrusion in the Yangtze Estuary. The results show that the strong northerly wind alone enhances saltwater intrusion in the estuary by inducing a counterclockwise circulation and reducing the stratification. However, with the combined effect from wind and waves, it is found that stratification is reduced in the outer North Channel, but enhanced in the inner North Channel, which results in an increase of salt transport in the estuary by approximately 40%. The results highlight the fact that saltwater intrusion in the Yangtze Estuary could be significantly underestimated without considering waves.

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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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