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基于卫星高度计资料的黑潮入侵南海流径的时间变化规律研究
引用本文:刘玉民,张志伟,张新城,孙忠斌,商巩,赵玮.基于卫星高度计资料的黑潮入侵南海流径的时间变化规律研究[J].海洋与湖沼,2023,54(4):951-962.
作者姓名:刘玉民  张志伟  张新城  孙忠斌  商巩  赵玮
作者单位:中国海洋大学三亚海洋研究院海南海洋立体观测与信息重点实验室 海南三亚 572024;中国海洋大学三亚海洋研究院海南海洋立体观测与信息重点实验室 海南三亚 572024;中国海洋大学物理海洋教育部重点实验室/深海圈层与地球系统前沿科学中心 山东青岛 266100
基金项目:国家重点研发计划, 2022YFC3105003号; 国家自然科学基金, 42076004号, 42222601号, 42206015号; 中央高校基本科研业务费, 202041009号, 202013028号; “泰山”学者计划, tsqn202103032号。
摘    要:黑潮入侵南海对南海的温盐平衡、环流、涡旋和局地气候等具有重要作用。基于吕宋海峡处黑潮不同流径的识别方法,对1993~2021年的卫星高度计资料进行识别,获取黑潮不同流径的发生时间,探究黑潮入侵南海流径的时间变化规律。结果表明:(1)黑潮主要以流套(Looping)和分支(Leaking)两种流径入侵南海,Leaking流径发生的时长(710周)和概率(46.9%)要远高于Looping流径(时长218周,概率14.4%)。(2) Looping流径和Leaking流径均可将高温高盐的西北太平洋水带入南海,Looping流径下的平均吕宋海峡上层通量(6.3×106 m3/s)略大于Leaking流径(5.6×106 m3/s)Looping和Leaking流径在4×106 m3/s~6×106 m3/s区间发生时间最长。(3)季节变化上,Looping流径主要发生在冬季,Leaking流径在冬半年均较强,夏季二者发...

关 键 词:黑潮入侵  流径  吕宋海峡  季节变化  年际变化
收稿时间:2022/11/30 0:00:00
修稿时间:2023/2/8 0:00:00

TEMPORAL VARIATION OF THE KUROSHIO INTRUSION PATH INTO THE SOUTH CHINA SEA BASED ON SATELLITE ALTIMETER DATA
LIU Yu-Min,ZHANG Zhi-Wei,ZHANG Xin-Cheng,SUN Zhong-Bin,SHANG Gong,ZHAO Wei.TEMPORAL VARIATION OF THE KUROSHIO INTRUSION PATH INTO THE SOUTH CHINA SEA BASED ON SATELLITE ALTIMETER DATA[J].Oceanologia Et Limnologia Sinica,2023,54(4):951-962.
Authors:LIU Yu-Min  ZHANG Zhi-Wei  ZHANG Xin-Cheng  SUN Zhong-Bin  SHANG Gong  ZHAO Wei
Affiliation:Key Laboratory of Ocean Observation and Information of Hainan Province, Sanya Oceanographic Institution, Ocean University of China, Sanya 572024, China;Key Laboratory of Ocean Observation and Information of Hainan Province, Sanya Oceanographic Institution, Ocean University of China, Sanya 572024, China;Key Laboratory of Physical Oceanography, MOE, China/Frontiers Science Center for Deep Ocean Multipheres and Earth System, Ocean University of China, Qingdao 266100, China
Abstract:The Kuroshio intrusion plays an important role in the thermohaline balance, circulation, mesoscale eddy, and local climate of the South China Sea. Based on the identification methods of different Kuroshio paths in the Luzon Strait and the altimeter data between 1993 and 2021, the occurrence time of different Kuroshio paths was identified and the temporal variation of the Kuroshio intrusion paths in the Luzon Strait was studied. Results show that (1) the Kuroshio mainly intrudes into the South China Sea in the paths of the Looping and Leaking. Leaking path occurs much longer (710 weeks) and more frequently (46.9%) than Looping paths (218 weeks, 14.4%); (2) both Looping and Leaking paths can carry warmer and saltier northwestern Pacific water into the South China Sea. In addition, the mean upper Luzon Strait flux in the Looping path is a little larger than that in the Leaking path. The Looping path and Leaking path both show longer occurrence time in the range 4×106~6×106 m3/s, respectively; (3) seasonally, the Looping path occurs mainly in winter and the Leaking path is strong in the whole winter half year, while both paths are weak in summer; (4) both Looping and Leaking paths have significant interannual variations. The Looping path occurred for the longest time in 1996 (up to 26 weeks), but almost disappeared in 2001; the Leaking path occurred for the longest time in 2005 (up to 40 weeks), but shortest in 2013; (5) the occurrence duration of the Looping path shows a long-term increasing trend of 0.15 weeks per year and the Leaking path shows a long-term decreasing trend of -0.17 weeks per year. The total occurrence time of Kuroshio intrusion presents a long-term decreasing trend; (6) The Looping path is modulated mainly by local wind and wind stress curl southwest of Taiwan Island at both seasonal and interannual scales, while the Leaking path is associated with the location of the North Equatorial Current Bifurcation.
Keywords:Kuroshio intrusion  paths  Luzon Strait  seasonal variation  interannual variation
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