地球科学进展 ›› 2008, Vol. 23 ›› Issue (10): 1027 -1036. doi: 10.11867/j.issn.1001-8166.2008.10.1027

研究论文 上一篇    下一篇

南海在1997/1998年El Niño事件后的异常变化
鲍颖,兰健,王毅   
  1. 中国海洋大学物理海洋教育部重点实验室,海洋学系,山东 青岛 266100
  • 收稿日期:2008-03-20 修回日期:2008-09-03 出版日期:2008-10-10
  • 通讯作者: 鲍颖 E-mail:baoying@ouc.edu.cn
  • 基金资助:

    国家重点基础研究发展计划项目“北太平洋副热带环流变异及其对我国近海动力环境的影响”(编号:2007CB411800)资助.

The Anomaly Response to the 1997/1998 El Niño Event in South China Sea

Bao Ying,Lan Jian,Wang Yi   

  1. Physical Oceanography Laboratory, Ocean Department, Ocean University of China, Qingdao 266100, China
  • Received:2008-03-20 Revised:2008-09-03 Online:2008-10-10 Published:2008-10-10

基于NOAA OISST.V2月平均SST资料和FSU月平均风应力资料对南海的SST和风场异常进行了分析,发现:南海对1997/1998年El Nio事件响应最为强烈,并在1997/1998年冬季和次年的夏季SST存在2个异常高峰值,风速存在2个异常减小的极值。为研究南海环流在1997/1998年的异常变化,利用ECOM水动力模型计算了1995—2000年的南海环流场,分析了1998年1月和8月南海水位和环流的异常分布,二者均存在显著的异常:①1月,整个南海海盆为正的水位异常,流场为反气旋异常环流,冬季控制整个南海海盆的气旋式环流减弱;②8月,南海海盆水位为正异常,特别是越南东部海区出现较强的正水位异常,南海南部的高水位中心扩大北移;异常流场表现为南部为气旋式异常环流,北部为反气旋的异常环流,且在越南东部海区形成非常强的反气旋异常环流中心,使得控制南海南部的反气旋环流和北部的气旋环流均减弱。风应力的分析表明,风应力旋度的异常变化是南海环流年际异常变化的主要因素。

Based on the NOAA OISST.V2 monthly SST dataset and FSU monthly windstress, the SST and windstress anomaly distributions in the South China Sea indicated that the South China Sea had been highly affected by the 1997/1998 El Niño event. The SSTA of February and August in 1998 had two peaks, while the wind speed reached its maximum minus anomalies in January and August. In order to find the circulation anomaly in the South China Sea, the circulation of 1995-2000 had been calculated by the ECOM hydrodynamic numerical model. The elevation and circulation of January and August in 1998 indicated that there were great anomaly of elevation and circulation after this El Niño event. (1)In January, the whole South China Sea had positive sea level anomaly and anti-cyclonic velocity anomaly, so the cyclonic circulation was weaker than normal. (2) In August, the South China Sea had positive sea level anomaly, especially stronger in the east of Vietnam, and cyclonic velocity anomaly in south, anti-cyclonic velocity in north, especially strong in the east of Vietnam. So the cyclonic gyre in the north and the anti-cyclonic gyre in the south were both weaker than normal, and an anti-cyclonic gyre appeared in the east of Vietnam. The analysis of wind stress curl indicate that the wind stress curl was the main reason for the anomaly of elevation and circulation.

中图分类号: 

[1] Dale W L. Wind and drift currents in the South China Sea[J]. Deep-Sea Research,1956,434:445-466.

[2] Wyrtki K. Physical Oceanography of the Southeast Asia Waters[R]. NAGA Report,1961,2:1-195.

[3] Xu Xizhen,Qu Zhang,Chen Huichang. The general descriptions of the horizontal circulation in the South China Sea[C]Proceedings of the 1980 Symposium on Hydrology and Meteorology of the Chinese Society for Oceanology and Limnology. Beijing: Science Press,1982:137-145.[徐锡桢,邱章,陈慧昌. 南海水平环流的概述[C]中国海洋湖沼学会水文气象学会学术会议论文集.北京:科学出版社,1982:137-145.]

[4]  Liu Yonggang,Yuan Yaochu,Su Jilan,et al. South China Sea circulation during the summer of 1998[J]. Chinese Science Bulletin,2000,452):1 252-1 259.[刘勇刚,袁耀初,苏纪兰,. 1998年夏季南海环流[J]. 科学通报,2000,452):1 252-1 259.]

[5] Bu Xianwei,Yuan Yaochu,Liu Yonggang. Application of P-vector method to the diagnostic calculation of circulation in the South China Sea in summer[J]. Acta Oceanologica Sinica,2001,233:8-17.[卜献卫,袁耀初,刘勇刚. P矢量方法在南海夏季环流诊断计算中的应用[J]. 海洋学报,2001,233):8-17.]

[6] Yuan Yaochu,Liu Yonggang,Lou Ruyun,et al. Calculation of circulation in the South China Sea during the summer of 2000 by the modified inverse method[J]. Acta Oceanologica Sinica,2004,261):1-13. [袁耀初,刘勇刚,楼如云,. 2000年夏季南海环流的改进逆方法计算[J]. 海洋学报,2004,261):1-13.]

[7] Yuan Yaochu,Bu Xianwei,Lou Ruyun,et al. Diagnostic calculation of the upper-layer circulation in the South China Sea during the winter of 1998[J]. Acta Oceanologica Sinica,2004,262):1-9.[袁耀初,献卫,楼如云,. 1998年冬季南海上层环流诊断计算[J]. 海洋学报,2004,262):1-9.]

[8] Liao Guanghong,Yuan Yaochu,Xu Xiaohua. The three dimensional structure of the circulation in the South China Sea during the winter of 1998[J]. Acta Oceanologica Sinica,2005,272):8-17.[廖光洪,袁耀初,徐晓华. 1998年冬季南海环流的三维结构[J]. 海洋学报,2005,272):8-17.]

[9] Shaw P T,Chao S Y. Surface circulation in the South China Sea[J]. Deep Sea Research,1994,411 663-1 683.

[10] Metzger E J,Hurlburt H E. Coupled dynamics of the South China Sea,the Sulu Sea and the Pacific Ocean[J]. Journal of Geophysical Research,1996,10112):331-352.

[11] Cai Shuqun,Su Jilan,Gan Zijun. The numerical study on the dynamic mechanism of the South China sea upper circulation in winter[J]. Acta Oceanologica Sinica,2001,235):14-23.[蔡树群,苏纪兰,甘子钧,. 冬季南海上层环流动力机制的数值研究[J]. 海洋学报,2001,235):14-23.]

[12] Cai Shuqun,Su Jilan,Gan Zijun. The numerical study of the dynamic mechanism of the South China sea upper circulation in summer[J]. Acta Oceanologica Sinica,2002,241):1-7.[蔡树群,苏纪兰,甘子钧,. 夏季南海上层环流动力机制的数值研究[J]. 海洋学报,2002,241):1-7.]

[13] Li Li,Wu Risheng,Guo Xiaogang. Seasonal circulation in the South China Sea—A TOPEX/POSEIDON satellite altimetry study[J]. Acta Oceanologica Sinica,2000,226):13-25. [李立,吴日升,郭小钢.南海的季节环流——TOPEX/POSEITON卫星测高应用研究[J]. 海洋学报,2000,226):13-25.]

[14] Chao S Y,Shaw P T,Wu S Y. El Niño modulation of the South China Sea Circulation[J]. Progress in Oceanography,1996,3851-93.

[15] Wu C R,Shaw P T,Chao S Y. Seasonal and Interannual Variations in the Velocity Field of the South China Sea[J]. Journal of Oceanography,1998,54361-372.

[16] Wang Weiqiang,Wang Dongxiao,Shi Ping. Annual and interannual variations of large-scale dynamic in South China Sea[J]. Journal of Tropical Oceanography,2001,201):61-68.[王卫强,王东晓,施平.南海大尺度动力场年循环和年际变化[J].热带海洋学报,2001,201):61-68.]

[17] Wang C,Wang W,Wang D,et al. Interannual variability of the South China Sea associated with El Niño[J]. Journal of Geophysical Research,2006,111,C03023,doi:10.1029/2005JC003333.

[18] Blumberg A F,Mellor G L. A description of a three-dimensional coastal ocean circulation model, in Three-Dimensional Coastal Ocean Models[J]. Coastal and Estuarine Sciences,1987,4:1-16.

[19] Fang Wendong,Guo Zhongxin,Huang Yuting. The observation study on the southern South China sea[J]. Chinese Science Bulletin,1997,4221:2 264-2 271.[方文东,郭忠信,黄羽庭. 南海南部海区的环流观测研究[J]. 科学通报,1997,4221):2 264-2 271.]

[20] Fang Wendong,Fang Guohong. The recent progress in the study of the southern South China Sea circulation[J]. Advances in Earth Science,1998,132):166-172.[方文东,方国洪. 南海南部海洋环流研究的新进展[J]. 地球科学进展,1998,132):166-172.]

[21] Liu Z H,Yang H,Liu Q. Regional dynamics of Seasonal Variability in the South China sea[J]. Journal of Physical Oceanography,2001,31:272-284.

[22] Liu Q,Huang R X,Wang D,et al. Interplay between the Indonesian Throughflow and the Luzon Strait Throughflow[J]. Chinese Science Bulletin,2006,51supp. II:50-58.

[23] Wang D,Liu Q,Huang R X,et al. Interannual variability of the South China Sea throughflow inferred from wind data and an ocean data assimilation product[J]. Geophysical Research Letters,2006,33,L14605,doi:10.1029/2006GL026316.

[1] 李欣泽, 金会军, 吴青柏, 魏彦京, 温智. 北极多年冻土区埋地输气管道周边温度场数值分析[J]. 地球科学进展, 2021, 36(1): 69-82.
[2] 董治宝,吕萍,李超. 火星风沙地貌研究方法[J]. 地球科学进展, 2020, 35(8): 771-788.
[3] 张晓辉,彭亚兰,黄根华. 南海碳源汇的区域与季节变化特征及控制因素研究进展[J]. 地球科学进展, 2020, 35(6): 581-593.
[4] 李琼,王姣姣,潘保田. 构造和降水对祁连山北麓冲积扇演化影响的数值模拟研究[J]. 地球科学进展, 2020, 35(6): 607-617.
[5] 王蓉, 张强, 岳平, 黄倩. 大气边界层数值模拟研究与未来展望[J]. 地球科学进展, 2020, 35(4): 331-349.
[6] 王冰笛, 李清泉, 沈新勇, 董李丽, 汪方, 王涛, 梁信忠. 区域气候模式 CWRF对东亚冬季风气候特征的模拟[J]. 地球科学进展, 2020, 35(3): 319-330.
[7] 张成晨,许长海,何敏,高顺莉. 东海到南海晚中生代岩浆弧及陆缘汇聚体制综述[J]. 地球科学进展, 2019, 34(9): 950-961.
[8] 王坚红,张萌,任淑媛,王兴,苗春生. 太行山脉地形坡度对下山锋面气旋暴雨影响模拟研究[J]. 地球科学进展, 2019, 34(7): 717-730.
[9] 汪品先. 深水珊瑚林[J]. 地球科学进展, 2019, 34(12): 1222-1233.
[10] 黄恩清,孔乐,田军. 冷水珊瑚测年与大洋中—深层水碳储库[J]. 地球科学进展, 2019, 34(12): 1243-1251.
[11] 王萌,张艳伟,刘志飞,吴家望. 南海北部中尺度涡的时空分布特征:基于卫星高度计资料的统计分析[J]. 地球科学进展, 2019, 34(10): 1069-1080.
[12] 张晨,王清,赵建民. 海洋微塑料输运的数值模拟研究进展[J]. 地球科学进展, 2019, 34(1): 72-83.
[13] 王世红, 赵一丁, 尹训强, 乔方利. 全球海洋再分析产品的研究现状[J]. 地球科学进展, 2018, 33(8): 794-807.
[14] 李正泉, 宋丽莉, 马浩, 冯涛, 王阔. 海上风能资源观测与评估研究进展[J]. 地球科学进展, 2016, 31(8): 800-810.
[15] 陆雯茜, 吴涧. 气溶胶影响印度夏季风和东亚夏季风的研究进展[J]. 地球科学进展, 2016, 31(3): 248-257.
阅读次数
全文


摘要