Characteristics of the transition layer in the South China Sea in 1998

Li Peiliang; Zuo Juncheng; Li Lei; Du Ling

doi:10.1007/BF02842758

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Characteristics of the transition layer in the South China Sea in 1998

OriginalPaper | Updated：2023-05-16

- Characteristics of the transition layer in the South China Sea in 1998
- Characteristics of the transition layer in the South China Sea in 1998
- 海洋湖沼学报（英文） 2003年21卷第1期页码：27-33
- Affiliations：
  
  Department of Oceanography Ocean University of Qingdao
- Author bio：
- Funds：
  
  Project No. 49906001 supported by the NSFC;the CTD data were provided by ‘Monsoon Experiments in South China Sea’ Project (G1999043805).
- DOI：10.1007/BF02842758
  中图分类号：
- 纸质出版：2003
- Accepted：
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Characteristics of the transition layer in the South China Sea in 1998[J]. 海洋湖沼学报（英文）, 2003,21(1):27-33.

Peiliang, L., Juncheng, Z., Lei, L. et al. Characteristics of the transition layer in the South China Sea in 1998., Chin. J. Ocean. Limnol. 21, 27–33 (2003). https://doi.org/10.1007/BF02842758
Characteristics of the transition layer in the South China Sea in 1998[J]. 海洋湖沼学报（英文）, 2003,21(1):27-33. DOI： 10.1007/BF02842758.

Peiliang, L., Juncheng, Z., Lei, L. et al. Characteristics of the transition layer in the South China Sea in 1998., Chin. J. Ocean. Limnol. 21, 27–33 (2003). https://doi.org/10.1007/BF02842758 DOI：

摘要

Abstract

CTD data on standard levels collected during July and December in 1998 and the cubic spline interpolating method were used to study the characteristics of the transition layer temperature and salinity. The thermocline undergoes remarkable seasonal variation in the South China Sea (SCS)

and especially in the region of the north shelf where the thermocline disappears in December. The thermocline is stronger and thicker in July than in December. There is no obvious seasonal variation in the halocline. Due to the upper Ekman transport caused by monsoon over the SCS

the thermocline slopes upward in July and downward in December from east to west in the northern SCS. The characteristics of the thermocline and halocline are influenced by local eddies in the SCS. The Zhujiang diluted flow influences significantly the SCS shelf's halocline.

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references

Huang Qizhou, Wang Wenzhi, Li, Y.S., 1992. General situations of the current and eddy in the South China Sea.Advance in Earth Sciences 7(5): 1–9 (in Chinese with English abstract)

Li Peiliang, Qi Jianhua, Fang Xinhua, 2000. The characteristics of the seawater transition layer in the investigated ara of Nansha Islands in Nov. 1997.Transactions of Oceanology and Limnology 1: 1–7. (in Chinese with English abstract)

Liu Qinyu, Yang Haijun, Wang Qi, 2000. Dynamic characteristics of seasonal thermocline in the deep sea region of the South China Sea.Chin. J. Oceanol. Limnol. 18(2): 104–109.

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