热带气旋影响吕宋海峡输运的研究进展与展望*
杨磊(1977—), 女, 副研究员, 博士, 硕士生导师, 从事海洋大气相互作用研究。email: |
*感谢三位匿名审稿专家和编辑对稿件提出的修改意见 |
Copy editor: 林强
收稿日期: 2022-07-04
修回日期: 2022-08-15
网络出版日期: 2022-08-26
基金资助
国家自然基金重点项目(92158204)
广东省基础与应用基础研究基金(2022A1515010945)
国家重点研发计划资助(2022YFE0203500)
广东省科技计划资助(2022B1212050003)
Recent research progress in the influence of tropical cyclones on the Luzon Strait transport*
Copy editor: LIN Qiang
Received date: 2022-07-04
Revised date: 2022-08-15
Online published: 2022-08-26
Supported by
National Natural Science Foundation of China(92158204)
Guangdong Basic and Applied Basic Research Foundation(2022A1515010945)
National Key R&D Program of China(2022YFE0203500)
Science and Technology Program of Guangdong Province(2022B1212050003)
吕宋海峡是连接南海与西太平洋的唯一深水通道, 也是调节南海环流及其热力特征的关键海洋通道。在大尺度西边界流、中尺度涡、热带气旋等众多因子的共同影响下, 吕宋海峡输运表现出显著的多时间尺度变率特征, 其中热带气旋是影响该海域强烈且频繁的天气过程之一, 解析吕宋海峡输运与热带气旋之间的动力联系也是近年来南海海洋研究的热点之一。本文主要从吕宋海峡附近热带气旋活动特征及其对黑潮、吕宋海峡附近环流结构、吕宋海峡输运的影响等方面回顾最新的研究进展。最后, 本文认为接下来应当在热带气旋调制吕宋海峡输运的机制, 以及对吕宋海峡输运年际变化的贡献等方面加强研究。
杨磊 , 温金辉 , 王强 , 罗希 , 黄华明 , 何云开 , 陈举 . 热带气旋影响吕宋海峡输运的研究进展与展望*[J]. 热带海洋学报, 2023 , 42(3) : 40 -51 . DOI: 10.11978/2022150
As the unique deep channel that connects the South China Sea (SCS) with the western Pacific Ocean, Luzon Strait is also the key oceanic passage that modulates the SCS circulation and its thermodynamic characteristics. Influenced by large-scale western boundary current, meso-scale eddies, tropical cyclones and other factors, Luzon Strait transport (LST) exhibits significant multi timescale variability. Tropical cyclones are strong and localized low-pressure weather systems that occur frequently in the area, therefore, understanding the dynamic connection between tropical cyclones and LST is one of the most essential topics in oceanography research. This study reviews the research progress in the characteristics of tropical cyclones near the Luzon Strait and its impact on the Kuroshio, ocean circulation and LST, and reveals their recent development. We further suggest that the future study should focus on the modulating mechanisms of the tropical cyclones on the LST and evaluate their contributions to the interannual variations of LST.
图2 7月份台风Imbudo(2003)经过吕宋海峡时右侧位置(118°E, 19°45′N)的上层水深温度随时间的变化序列(a)及混合层深度随时间的变化序列(b)改自崔红 等(2009) Fig. 2 Time series of the upper ocean temperature (a) and mixed layer depth (b) at the location (118°E, 19°45′N) in the South China Sea in July, 2013 when the Typhoon Imbudo passed the Luzon Strait, after Cui et al (2009) |
图3 6月30日台风“蒲公英”(2004)到达吕宋海峡时位置对应的海面风场分布(箭头)、相应时间的风应力旋度分布(填色) (a)和上50m流速(箭头)及涡度场分布(填色) (b), 以及台风过境期间吕宋海峡垂直积分体积输运的时间演变(c)改自隋俊鹏 等(2011) Fig. 3 Surface wind (vector) and the corresponding wind stress curl (shadings) (a) and ocean current (vector) and vorticity (shading) (b) on June 30th when the Typhoon Dandelion (2001) arrived in the Luzon Strait, as well as vertical integration of Luzon Strait transport during the passage of Typhoon Dandelion (2004) (c). After Sui et al (2011) |
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