南海北部深层近惯性振荡信号研究  被引量:1

DEEP NEAR-INERTIAL WAVE IN THE NORTHERN SOUTH CHINA SEA

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作  者:侯华千 于非[1] 李彬[3] 任强[1] 魏传杰[1] HOU Hua-Qian;YU Fei;LI Bin;REN Qiang;WEI Chuan-Jie(Institute of Oceanology,Chinese Academy of Science,Qingdao 266071,China;University of Chinese Academy of Science,Beijing100049,China;State Key Laboratory of Robotics,Shenyang Institute of Automation,Chinese Academy of Sciences,Shenyang 110016,China)

机构地区:[1]中国科学院海洋研究所,青岛266071 [2]中国科学院大学,北京100049 [3]中国科学院沈阳自动化研究所机器人学国家重点实验室,沈阳110016

出  处:《海洋与湖沼》2019年第5期948-957,共10页Oceanologia Et Limnologia Sinica

基  金:国家自然科学基金委员会-山东省人民政府联合资助海洋科学研究中心项目,U1406401号;国家自然科学基金委员会-创新研究群体科学基金,41421005号;国家重点研发计划-准实时传输深海剖面锚系观测潜标研发,2017YFC1403400号

摘  要:本研究通过分析布放在南海北部的着陆器流速数据,研究一支蓝移的近惯性振荡信号,发现该信号可以传到600m水深以下,持续时间为11月3 16日。该信号的最大的东向流速为0.133m/s,最大南向流为0.124m/s。谱分析发现垂向流速呈现出5个不同的流核,最强流核发生在600 650m位置。近惯性能量下传速度为67±5m/d,从600m下传到1000m的位置能量耗散18%。经验正交函数(empirical orthogonal function,EOF)分解结果显示,这次近惯性振荡信号开始是第一模态占主导,随后变成高阶模态为主导的形式。由于不知道其信号生成的源头,所以无法确定近惯性振荡形成原因,结合前人的研究结果,可以排除台风引起此次近惯性振荡信号的生成。卫星的海表高度异常显示,此时的正涡度有利于此次近惯性振荡发生蓝移特征。Based on the ADCP data in the lander located in the northern South China Sea(SCS),a blue shift near-inertial wave signal is studied.The lander was deployed in the northern SCS at 22.10°N/119.28°E in 1135m depth working from July 2017 to January 2018.This near-inertial wave signal transmitted to 600m depth during September 3 16.The maximum meridional velocity was 0.133m/s and the maximum zonal velocity was 0.133m/s.Five different energy cores in the near-inertial frequency band were recognized in spectrum analysis.The maximum energy core was in 600 650m depth.The vertical group velocity was 67±5m/d downward.The energy dissipation was 18%from 600 to 1000m.This near-inertial signal began with the first EOF mode dominant,and then became a combination of higher-order EOF mode dominant.Combined with the results of previous studies,we found that the near-inertial oscillation signal was not caused by a typhoon.As the source of the signal generation was unknown,the cause of the near-inertial oscillation could not be determined.The sea level anomaly data by satellite show that the positive vorticity at that time was conducive to the blue shift of the near-inertial waves.

关 键 词:南海北部 近惯性振荡 谱分析 经验正交函数分解(empirical ORTHOGONAL function EOF) 

分 类 号:P732.3[天文地球—海洋科学]

 

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