Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea

Pang Chongguang; Bai Xuezhi; Hu Dunxin

doi:10.1007/BF02842837

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Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea

OriginalPaper | Updated：2023-05-16

- Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea
- Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea
- 海洋湖沼学报（英文） 2003年21卷第3期页码：214-221
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
  
  Project No. KZCX2-207 supported by Chinese Academy of Sciences and No. 496-36210 supported by NSFC.
- DOI：10.1007/BF02842837
  中图分类号：
- 网络首发：2013-01-31，
  
  纸质出版：2003
- Accepted：
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Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea[J]. 海洋湖沼学报（英文）, 2003,21(3):214-221.

Chongguang, P., Xuezhi, B. & Dunxin, H. Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea., Chin. J. Ocean. Limnol. 21, 214–221 (2003). https://doi.org/10.1007/BF02842837
Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea[J]. 海洋湖沼学报（英文）, 2003,21(3):214-221. DOI： 10.1007/BF02842837.

Chongguang, P., Xuezhi, B. & Dunxin, H. Numerical study of water and suspended matter exchange between the Yellow Sea and the East China Sea., Chin. J. Ocean. Limnol. 21, 214–221 (2003). https://doi.org/10.1007/BF02842837 DOI：

摘要

Abstract

POM was used to study the monthly mean circulation in the Yellow Sea and East China Sea. The calculated results showed almost all major characteristics of the circulation system. The calculated circulation system and observational data were used to determine the sediment concentration

volume transport

heat flux and suspended matter flux between the Yellow Sea and the East China Sea. The conclusions obtained were that the volume and heat are transported northward through the 32°N section during each season; that in winter and autumn

total suspended matter is transported southward

and is larger in winter than in autumn. The reason is that the Yellow Sea Coastal Current is strong and always contains more suspend matter in winter and autumn. The seasonal suspended matter exchange between the Yellow Sea and the East China Sea are 0.58×107 tons in spring

2.81×107 tons in summer

−2.60×107 tons in autumn and −3.40×107 tons in winter. Net flux of suspended matter from the Yellow Sea to the East China Sea is 2.61×107 tons every year.

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references

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