Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region

Shi Maochong; Wang Xiaoqing; Jing Zhenhua

doi:10.1007/BF02846262

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Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region

OriginalPaper | Updated：2023-05-16

- Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region
- Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region
- 海洋湖沼学报（英文） 1989年7卷第4期页码：312-317
- Affiliations：
  
  Ocean University of Qingdao
- Author bio：
- Funds：
  
  This paper was presented at the Conference on Western Pacific Circulation Influence on the China Seas in Qingdao, 1987, and approved for publishing as a monograph.
- DOI：10.1007/BF02846262
  中图分类号：
- 纸质出版：1989
- Accepted：
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Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region[J]. 海洋湖沼学报（英文）, 1989,7(4):312-317.

Maochong, S., Xiaoqing, W. & Zhenhua, J. Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region., Chin. J. Ocean. Limnol. 7, 312–317 (1989). https://doi.org/10.1007/BF02846262
Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region[J]. 海洋湖沼学报（英文）, 1989,7(4):312-317. DOI： 10.1007/BF02846262.

Maochong, S., Xiaoqing, W. & Zhenhua, J. Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region., Chin. J. Ocean. Limnol. 7, 312–317 (1989). https://doi.org/10.1007/BF02846262 DOI：

摘要

Abstract

The aim of the study was 1)to determine the relation between the Kuroshio meander and the intensity of the subtropic high pressure over the Pacific Ocean

and then to obtain statistical validity for the observational conclusion that the occurrence time of the Kuroshio meander leads the time of strengthened C-circulation of Europe by one or more years; 2) to develop a method to predict the occurrence time of flood or drought periods in the Changjiang River Valley from the occurrence time of the Kuroshio meander

since there is a close relation between the occurrence time of the drought or flood periods in the Changjiang River Valley and the occurrence time of the strong or weak periods of C-circulation of Europe; and 3) to develop a logical explanation verifiable by remote sensing technique and other means that the warm species phytoplanktons collected recently in the Jiaozhou Bay of Shandong Peninsula in China were carried there by a new warm current branch of the Kuroshio in the East China Sea.

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references

Botalin, A. M. 1961. Problems of Kuroshio meander.Oceanology,6: 961–975. (in Russian with English abstract)

Chen Juyin, 1986. The analysis and forecast about relation between the moon-sun and the drought and flood periods in the Changjiang River Valley. The collected works on medium to long period hydrographic forecasts. Proceedings of Astronomy and Meteorology Symposium, Chinese Meteorogic Press. pp. 121–129(in Chinese)

Liaoning Institute of Meteorology Science, 1974. Historical Records of Drought and Flood in Liaoning. pp. 329–383. (in Chinese)

Yasuo Matsukawa, 1969. The relation between wind variation over the north Pacific Ocean and the large Kuroshio meander.Marine Sciences.9: 67–69. (in Japanese)

Peng Chengji, 1986. Winter current pattern of the East China Sea and the Yellow Sea from remote sensing data.Journal of Shandong College of Oceanology.3: 41–45. (in Chinese with English abstract)

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