An analysis of characteristics of variation of the Taiwan Warm Current Deep Water

Weng Xuechuan; Wang Congmin

doi:10.1007/BF02852907

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An analysis of characteristics of variation of the Taiwan Warm Current Deep Water

OriginalPaper | Updated：2023-05-16

- An analysis of characteristics of variation of the Taiwan Warm Current Deep Water
- An analysis of characteristics of variation of the Taiwan Warm Current Deep Water
- 海洋湖沼学报（英文） 1985年3卷第1期页码：96-108
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 861 from the Institute of Oceanology, Academia Sinica.;This paper was published in Chinese in;Oceanologia et Limnologia, Sinica;14;(4): 357–366.
- DOI：10.1007/BF02852907
  中图分类号：
- 纸质出版：1985
- Accepted：
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An analysis of characteristics of variation of the Taiwan Warm Current Deep Water[J]. 海洋湖沼学报（英文）, 1985,3(1):96-108.

Xuechuan, W., Congmin, W. An analysis of characteristics of variation of the Taiwan Warm Current Deep Water., Chin. J. Ocean. Limnol. 3, 96–108 (1985). https://doi.org/10.1007/BF02852907
An analysis of characteristics of variation of the Taiwan Warm Current Deep Water[J]. 海洋湖沼学报（英文）, 1985,3(1):96-108. DOI： 10.1007/BF02852907.

Xuechuan, W., Congmin, W. An analysis of characteristics of variation of the Taiwan Warm Current Deep Water., Chin. J. Ocean. Limnol. 3, 96–108 (1985). https://doi.org/10.1007/BF02852907 DOI：

摘要

Abstract

The Taiwan Warm Current Deep Water (or the East China Sea Upper Layer Water

or the East China Sea Subsurface Water) lying in the deep and bottom layers off the coast of Fujian-Zhejiang is one of the main watermasses in the continental shelf region of the western East China Sea. The hydrographical conditions and the fishery productions in this region are affected remarkably by the decline and growth of the Taiwan Warm Current Deep Water. Although the temperature

salinity and origin of the Taiwan Warm Current Deep Water have been investigated[3] by oceanographers the world over

there are up to now few papers published on its characteristics of ariations (seasonal and multiyear variations). Understanding of this problem will be helpful to further characterize this watermass. For this reason

in this paper

section 28°N representing the middle Taiwan Warm Current Deep Water and section 30°N representing the northern Taiwan Warm Current Deep Water are taken for examples

and the method of similar coefficient is used for analysis of this problem.

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references

Miller, A. R., 1950. A study of mixing processes over the edge of the continental shelf.Jour. Mar. Res. 9 (2): 145–160.

Weng Xuechuan and Wang Congmin, 1982. Determination of the boundary and T-S bounds of the Huanghai Sea Cold Water Mass. Proceedings of the 1980 Symposium on Hydrometeorology of the Chinese Society of Oceanology and Limnology. 61–70.

Weng Xuechuan and Wang Congmin, 1984. A preliminary study on the T-S characteristics and the origin of Taiwan Warm Current Water in summer.Studia Marina Sinica 21: 113–133.

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