南海18&#176;N断面中层水的年代际变化

赵德平; 王卫强; 覃慧玲; 毛庆文; 王东晓; 陈荣裕

doi:10.3969.issn.0253-4193.2014.09.007

南海18°N断面中层水的年代际变化

doi: 10.3969.issn.0253-4193.2014.09.007

1.
中国科学院南海海洋研究所热带海洋环境国家重点实验室,广东广州 510301;中国科学院大学,北京 100049
2.
中国科学院南海海洋研究所热带海洋环境国家重点实验室,广东广州 510301

基金项目: 国家自然科学基金项目(41376024,41276108,41206010);中国科学院战略性先导科技专项(A类)资助(XDA11010301);科学基础性工作专项——南海海洋断面科学考察(2008FY110100海洋)。

计量
- 文章访问数: 1672
- HTML全文浏览量: 21
- PDF下载量: 1229
- 被引次数: 0
出版历程
- 收稿日期: 2013-09-11
- 修回日期: 2013-12-10

Decadal changes of the intermediate water at 18°N in the South China Sea

1.
State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Sciences, Beijing 100049, China
2.
State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

摘要

摘要: 利用中国科学院南海海洋研究所历史温盐剖面观测资料和WOD09(World Ocean Database 2009)中的CTD、OSD、PFL温盐剖面资料，分析了1965-2012年间南海18°N跨海盆断面中层水的变化特征。研究结果表明:中层水平均盐度呈现显著的年代际变化，20世纪60年代中期至70年代末，中层水平均盐度约为34.432，80年代盐度增加至34.440，90年代之后至今盐度明显降低;在年代际尺度变异调制下，不同年代中层水盐度变化有不同的变化趋势，1967-1977年呈现显著的下降趋势，1990-1997年中层水盐度从34.450迅速降为34.414，而在1997年之后表现出明显上升趋势，与此同时，中层水温度有着相似的变化特征，与90年代之前相比，21世纪以来温度与盐度同步下降，并且变化幅度变小。与大洋的中层水团年代际变异相比，南海18°N断面中层水呈现出与大洋不同的特征。另外，中层水盐度有着十分显著的年际变化，其振幅远大于年代际尺度变异，并且与ENSO密切相关，在厄尔尼诺年达到极小值。
- 南海 /
- 18° /
- N /
- 中层水 /
- 年代际变化
Abstract: Decadal change characteristics of the intermediate water at 18°N in the South China Sea during 1965 and 2012 were investigated using the historical temperature and salinity profile data from SCSIO (South China Sea Institute of Oceanology) and WOD09 (World Ocean Database 2009). This study revealed the significant decadal changes of the intermediate water based on the analysis of its decadal averaged salinity. The salinity was 34.432 on average in the period of 1965 to 1977 and increased to 34.440 in the 1980s, followed by an evident decrease after the 1990s. Modulated by the decadal scale changes, the salinity variation presented different trends in different periods. There was a significant decrease trend from 1967 to 1977, followed by a further decrease from 34.450 to 34.414 during 1990 and 1997. Thereafter there appeared a significant increase. Meanwhile, the temperature presented the same changing trends. Both temperature and salinity decreased in the 21st century with smaller amplitude of variation compared those in 1990s. The decadal changes of the intermediate water at 18°N were found to present different characteristics than those of Indian Ocean and the Pacific Ocean. In addition, the significant decadal changes of the intermediate water have greater amplitudes than those of the decadal scale variations. In addition, it is found that the salinity was closely related with ENSO that it reached its minimum in El Niño years.
- South China Sea /
- 18° /
- N /
- intermediate water /
- decadal changes

HTML全文

参考文献(24)

Sverdrup H, Johnson M, Fleming R. The Oceans[M]. New York: Prentice-Hall Inc, 1942: 1087.

Talley L D. An Okhotsk Sea water anomaly: implications for ventilation in the North Pacific[J]. Deep Sea Research Part A: Oceanographic Research Papers, 1991, 38: S171-S190.

Talley L D. Distribution and formation of North Pacific intermediate water[J]. J Phys Oceanogr, 1993, 23: 517-537.

Yasuda T, Hanawa K. Decadal changes in the mode waters in the midlatitude North Pacific[J]. J Phys Oceanogr, 1997, 27: 858-870.

You Y, Suginohara N, Fukasawa M, et al. Roles of the Okhotsk Sea and Gulf of Alaska in forming the North Pacific Intermediate Water[J]. Journal of Geophysical Research: Oceans, 2000, 105(C2): 3253-3280.

You Y Z, Chern C S, Yang Y, et al. The South China Sea, a cul-de-sac of North Pacific Intermediate Water[J]. Journal of Oceanography, 2005, 61(3): 509-527.

Bryden H L, Griffiths M J, Lavin A M, et al. Decadal changes in water mass characteristics at 24°N in the subtropical North Atlantic ocean[J]. J Climate, 1996, 9(12): 3162-3186.

Wong A P S, Bindoff N L, Church J A. Large-scale freshening of intermediate waters in the Pacific and Indian oceans[J]. Nature, 1999, 400(6743): 440-443.

Bryden H L, McDonagh E L, King B A. Changes in ocean water mass properties: Oscillations or trends？[J]. Science, 2003, 300(5628): 2086-2088.

张艳慧, 王凡, 臧楠. 基于Argo浮标和历史资料的热带西太平洋次表层与中层水年代变化分析[J]. 海洋学报, 2009, 30(6): 17-23.

Qu T, Mitsudera H, Yamagata T. Intrusion of the North Pacific waters into the South China Sea[J]. Journal of Geophysical Research: Oceans, 2000, 105(C3): 6415-6424.

Chen C T A, Huang M H. A mid-depth front separating the South China Sea water and the Philippine Sea water[J]. Journal of Oceanography, 1996, 52(1): 17-25.

Chen C T A. Tracing tropical and intermediate waters from the South China Sea to the Okinawa Trough and beyond[J]. Journal of Geophysical Research: Oceans, 2005, 110(C5).

Nitani H. Beginning of the Kuroshio[M]// Stommel H, Yoshida K. Kuroshio: Physical Aspects of the Japan Current. Washington: University of Washington Press, 1972: 129-163.

Qu T. Evidence for water exchange between the South China Sea and the Pacific Ocean through the Luzon Strait[J]. Acta Oceanologica Sinica, 2002, 21(2): 175-185.

Tian J W, Yang Q X, Liang X F, et al. Observation of Luzon Strait transport[J]. Geophysical Research Letters, 2006, 33(19):L19607.

Yang Q X, Tian J W, Zhao W. Observation of Luzon Strait transport in summer 2007[J]. Deep Sea Research Part I: Oceanographic Research Papers, 2010, 57(5): 670-676.

Lan J, Zhang N N, Wang C X. The destiny of the North Pacific Intermediate Water in the South China Sea[J]. Acta Oceanologica Sinica, 2012, 31(5): 41-45.

刘长建, 杜岩, 张庆荣, 等. 南海次表层和中层水团年平均和季节变化特征[J]. 海洋与湖沼, 2008, 39(1): 55-64.

刘增宏, 许建平, 孙朝辉, 等. 吕宋海峡附近海域水团分布及季节变化特征[J]. 热带海洋学报, 2011, 30(1): 11-19.

杨春辉. 南海中层水的年际变化研究. 青岛: 中国海洋大学, 2011.

Liu C J, Wang D X, Chen J, et al. Freshening of the intermediate water of the South China Sea between the 1960s and the 1980s[J]. Chinese Journal of Oceanology and Limnology, 2012, 30(6): 1010-1015.

刘增宏, 李磊, 许建平, 等. 1998年夏季南海水团分析[J]. 东海海洋, 2001, 19(3): 1-10.

田天, 魏皓. 南海北部及巴士海峡附近的水团分析[J]. 中国海洋大学学报, 2005, 35(1): 9-12.

施引文献

资源附件(0)

访问统计