Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea

Liu Qin-yu; Yang Hai-jun; Wang Qi

doi:10.1007/BF02842568

Your Location：

Home >

Browse articles >

Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea

OriginalPaper | Updated：2023-05-16

- Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea
- Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea
- 海洋湖沼学报（英文） 2000年18卷第2期页码：104-109
- Affiliations：
  
  Institute of Physical Oceanography Ocean University of Qingdao
- Author bio：
- Funds：
  
  Project 49636230 supported by NSFC and National Special Research Program (No. 97-926-05-02).
- DOI：10.1007/BF02842568
  中图分类号：
- 纸质出版：2000
- Accepted：
Scan QR Code
Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea[J]. 海洋湖沼学报（英文）, 2000,18(2):104-109.

Qin-yu, L., Hai-jun, Y. & Qi, W. Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea., Chin. J. Ocean. Limnol. 18, 104–109 (2000). https://doi.org/10.1007/BF02842568
Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea[J]. 海洋湖沼学报（英文）, 2000,18(2):104-109. DOI： 10.1007/BF02842568.

Qin-yu, L., Hai-jun, Y. & Qi, W. Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea., Chin. J. Ocean. Limnol. 18, 104–109 (2000). https://doi.org/10.1007/BF02842568 DOI：

摘要

Abstract

The dynamic characteristics of the seasonal thermocline in the deep sea region of the South China Sea were analyzed by using seasonal mean temperature climatology. The thermocline undergoes remarkably seasonal variation throughout a year

is thinnest and weakest in winter

and thickest in spring

strongest in summer and fall. Due to the upper Ekman transport caused by monsoon over the SCS

the thermocline slopes upward (downward) in winter (summer) from northwest to southeast

but there is no pileup of upper warm water along the monsoon direction. In addition

the intrusion of the Kuroshio loop through the Luzon Strait

and some local eddies in the SCS

can notably affect the depth

thickness and strength of the thermocline in the deep sea region of the SCS.

关键词

Keywords

references

Chao, S. Y., Shaw, P. T., Wang, J., 1995. Wind relaxation as a possible cause of the South China Sea warm current.J. Oceanogra. 51: 111–132.

Chu, P. C., Chang, C. P., 1997. South China Sea warm pool in Boreal Spring.Advances in Atmospheric Sciences 14(2): 193–206.

Levitus, S., 1982. Climatological Altas of the World Ocean. NOAA Prof. Pap. No. 13, U. S. Government Printing Office, Washington, DC, 173 p.

Li, R. F., Huang, Q. Z., Wang, W. Z., 1994. Numerical simulation of the upper circulation in the South China Sea.Acta Oceanologica Sinica 16(4): 13–22. (in Chinese with English abstract)

Liu, Q. Y., Liu, C. T., Liu, S. P. et al., 1996. The deformation of the Kuroshio in Luzon Strait and its dynamics.J. Ocean University of Qingdao 26(4): 413–419. (in Chinese with English abstract)

Qiu, Z., Xu, X. Z., Long, X. M., 1996. The characteristics of the thermocline in the Nansha Islands in September 1994.Tropic Oceanology 15(2): 61–66. (in Chinese with English abstract)

Shaw, P. T., 1996. Winter upwelling off Luzon in the northeastern South China Sea.J. Geophys. Res. 101(C7): 16435–16448.

Xu, X. Z., Qiu, Z., Long, X. M., 1993. The radical characteristics and the one—dimensional calculated pattern of the South China Sea thermocline.Oceanol. Limnol. Sin. 24(5): 494–502. (in Chinese with English abstract)

Yang, H. J., Liu, Q. Y., 1998. The seasonal features of temperature distributions in the upper layer of the South China Sea.Oceanol. Limnol. Sin. 29(5): 501–507. (in Chinese with English abstract)

Zeng, Q. C., Li, R. F., Ji, F. F., 1989. Calculation of the monthly mean circulation in the South China Sea.Scientia Atmospherica Sinica 13(2): 127–138. (in Chinese with English abstract)

浏览量

Downloads

CSCD

文章被引用时，请邮件提醒。

Submit

工具集

关联资源

Environmental influence on transparent exopolymer particles and the associated carbon distribution across northern South China Sea

An ENSO-like oscillation system

3-D baroclinic numerical simulation of the South China Sea I. Upper circulation

Three-dimensional baroclinic numerical simulation of the South China sea circulation's seasonal characteristics II. Middle and deep circulation

Spatio-temporal variations in the siphonophore community of the northern South China Sea