首页 | 本学科首页   官方微博 | 高级检索  
     检索      

南海西北部半日内潮参量次谐频不稳定生成的近惯性波研究
引用本文:陈子飞,任强,胡贺岗,陈永华,王蓓,于非,南峰,王建丰,唐瑛.南海西北部半日内潮参量次谐频不稳定生成的近惯性波研究[J].海洋与湖沼,2022,53(1):62-73.
作者姓名:陈子飞  任强  胡贺岗  陈永华  王蓓  于非  南峰  王建丰  唐瑛
作者单位:中国科学院海洋研究所 山东青岛266071;中国科学院大学 北京 100049;中国科学院海洋环流与波动重点实验室 山东青岛 266071;中国科学院海洋研究所 山东青岛266071;中国科学院海洋环流与波动重点实验室 山东青岛 266071;中国科学院海洋大科学研究中心 山东青岛 266071;中国科学院海洋研究所 山东青岛266071;中国科学院海洋环流与波动重点实验室 山东青岛 266071;中国科学院海洋研究所 山东青岛266071;中国科学院大学 北京 100049;中国科学院海洋环流与波动重点实验室 山东青岛 266071;中国科学院海洋大科学研究中心 山东青岛 266071;青岛海洋科学与技术试点国家实验室海洋动力过程与气候功能实验室 山东青岛 266237;中国科学院海洋研究所 山东青岛266071;中国科学院海洋环流与波动重点实验室 山东青岛 266071;中国科学院海洋大科学研究中心 山东青岛 266071;青岛海洋科学与技术试点国家实验室海洋动力过程与气候功能实验室 山东青岛 266237
基金项目:国家重点研发计划项目,2017YFC1403401号;
摘    要:为了研究非临界纬度上参量次谐频不稳定(parametric subharmonic instability,PSI)过程生成的近惯性波(near-inertial wave,NIW),本文基于国家重点研发项目的 准实时传输深海潜标资料,对内波速度谱、近惯性流速和动能、D2-f(半日频减惯性频)流速和动能、半日内潮流速和...

关 键 词:南海西北部  半日内潮  近惯性波  参量次谐频不稳定  海洋混合
收稿时间:2021/8/2 0:00:00
修稿时间:2021/9/11 0:00:00

SEMIDIURAL TIDE PARAMETETRIC SUBHARMONIC INSTABILITY INDUCED NEAR-INERTIAL WAVES IN NORTHWESTERN SOUTH CHINA SEA
CHEN Zi-Fei,REN Qiang,HU He-Gang,CHEN Yong-Hu,WANG Bei,YU Fei,NAN Feng,WANG Jian-Feng,TANG Ying.SEMIDIURAL TIDE PARAMETETRIC SUBHARMONIC INSTABILITY INDUCED NEAR-INERTIAL WAVES IN NORTHWESTERN SOUTH CHINA SEA[J].Oceanologia Et Limnologia Sinica,2022,53(1):62-73.
Authors:CHEN Zi-Fei  REN Qiang  HU He-Gang  CHEN Yong-Hu  WANG Bei  YU Fei  NAN Feng  WANG Jian-Feng  TANG Ying
Institution:(Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;University of Chinese Academy of Sciences,Beijing 100049,China;CAS Key Laboratory of Ocean Circulation and Waves,Chinese Academy of Sciences,Qingdao 266071,China;Center for Ocean Mega-Science,Chinese Academy of Sciences,Qingdao 266071,China;Marine Dynamic Process and Climate Function Laboratory,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao 266237,China)
Abstract:In order to study the near-inertial wave(NIW) generated by the parametric subharmonic instability(PSI)process at non-critical latitudes, this paper examines the internal wave velocity spectrum, near inertial velocity and kinetic energy, D2-f(semidiurnal frequency minus inertial frequency) velocity and kinetic energy, semidiurnal tidal velocity and kinetic energy, and the time variation of turbulent mixing based on the data of quasi-real-time transmission subsurface mooring system. The slab model and bicoherence spectrum analysis show that the non-wind-generated near inertial waves appearing in the upper ocean are generated by the PSI of semidiurnal internal tides. The PSI not only generates diurnal internal waves, but also produces inertial frequency and D2-f motions in the non-critical latitudes of the Northwestern Slope of the South China Sea. At some depth where the PSI process is discernible, the near-inertial energy generated by the PSI is equivalent to the diurnal tidal energy, and the D2-f energy is equivalent to the semidiurnal tidal energy. In addition,significant PSI processes usually occur during strong semidiurnal movements. The results of the fine-scale parameterization method shows that the mixing is obviously enhanced during the PSI process, but the increase is moderate.
Keywords:Northwestern South China Sea  semidiurnal tides  near-inertial waves  parametric subharmonic instability(PSI)  turbulent mixing
本文献已被 维普 万方数据 等数据库收录!
点击此处可从《海洋与湖沼》浏览原始摘要信息
点击此处可从《海洋与湖沼》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号