The surface cold water off Subei (Northern Jiangsu) in late spring and summer

Pu Yongxiu

doi:10.1007/BF02845002

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The surface cold water off Subei (Northern Jiangsu) in late spring and summer

OriginalPaper | Updated：2023-05-16

- The surface cold water off Subei (Northern Jiangsu) in late spring and summer
- The surface cold water off Subei (Northern Jiangsu) in late spring and summer
- 海洋湖沼学报（英文） 1987年5卷第2期页码：186-193
- Affiliations：
  
  Second Institute of Oceanography
- Author bio：
- Funds：
- DOI：10.1007/BF02845002
  中图分类号：
- 纸质出版：1987
- Accepted：
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The surface cold water off Subei (Northern Jiangsu) in late spring and summer[J]. 海洋湖沼学报（英文）, 1987,5(2):186-193.

Yongxiu, P. The surface cold water off Subei (Northern Jiangsu) in late spring and summer., Chin. J. Ocean. Limnol. 5, 186–193 (1987). https://doi.org/10.1007/BF02845002
The surface cold water off Subei (Northern Jiangsu) in late spring and summer[J]. 海洋湖沼学报（英文）, 1987,5(2):186-193. DOI： 10.1007/BF02845002.

Yongxiu, P. The surface cold water off Subei (Northern Jiangsu) in late spring and summer., Chin. J. Ocean. Limnol. 5, 186–193 (1987). https://doi.org/10.1007/BF02845002 DOI：

摘要

Abstract

Every year during late spring and summer

a patch of surface cold water exists near the eastern side of the Subei shoal patch. The main cause of the cold water is the monthly southward migration and climbing up of the deep cold water from the western part of the southern Huanghai Sea. The existence of the deep ditches on the north side of the underwater delta off Subei controls the position of this cold water. Another patch of cold water is commonly observed southwest of Jizhou Island on the surface in the region 32oN and 124o–124.5oE during late spring and summer. Based on analysis

this water comes mainly from the deep layers of the northwest area; its upwelling is related to the northward “impulsive” extension of the Taiwan Warm Current in the previous period

and its position is probably related to the underwater reef chain there.

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references

Ding Zongxin. 1985. Description of hydrological structure in cyclonic eddy region of northern East China Sea in Summer.Oceanologia et Limnologia Sinica 16(2): 138–146 (in Chinese with English abstract).

Zhao Jinshan, Qiao Rongzhen et al., 1983. An Analysis of Current Conditions in the Investigation Area of the East china Sea.In “Proceedings of International Symposium on Sedimentation on the Continental Shelf, with Special Reference to the East China Sea. April 12–16. 1983. Hangzhou, China.” China Ocean Press, Beijing, pp. 314–327.

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