Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea

Bai Hong; Hu Dunxin; Pang Chongguang

doi:10.1007/BF02860428

Your Location：

Home >

Browse articles >

Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea

OriginalPaper | Updated：2023-05-16

- Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea
- Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea
- 海洋湖沼学报（英文） 2003年21卷第4期页码：329-334
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
  
  This work was supported by CAS Innovation Project (No. KZCX2-207), National Key Programme for Developing Basic Sciences (No: G1999043803) and CAS Major Project (KZ951-B1-403).
- DOI：10.1007/BF02860428
  中图分类号：
- 网络首发：2013-01-31，
  
  纸质出版：2003
- Accepted：
Scan QR Code
Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea[J]. 海洋湖沼学报（英文）, 2003,21(4):329-334.

Hong, B., Dunxin, H. & Chongguang, P. Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea., Chin. J. Ocean. Limnol. 21, 329–334 (2003). https://doi.org/10.1007/BF02860428
Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea[J]. 海洋湖沼学报（英文）, 2003,21(4):329-334. DOI： 10.1007/BF02860428.

Hong, B., Dunxin, H. & Chongguang, P. Characteristics of light transmission in summer and winter and its relation to sediment transport in the East China Sea., Chin. J. Ocean. Limnol. 21, 329–334 (2003). https://doi.org/10.1007/BF02860428 DOI：

摘要

Abstract

Light transmission data collected from June to July 1987 and from February to March 1997 by theR/V Kexue 1 in the East China Sea were used to analyze its distribution characteristics and its relation to the sediment transport in this sea. Some results obtained were: (1) The Taiwan Warm Current flowing northwards seemed to be a barrier preventing suspended matter discharged from the Changjiang River Estuary from continuously moving southeastward and causing the suspended matter to flow along a path near 123°30′E in summer and 123°00′E in winter. (2) Suspended matter in the area adjacent to the Changjiang River Estuary could not be transported southward along the coast in summer due to opposing offshore currents including the Taiwan Warm Current flowing northward and the Changjiang Diluted Water turning northeastward. (3) The thermocline and temperature front bar suspended matter from crossing through.

关键词

Keywords

references

Drake, D. E. 1971. Suspended sediment and thermal stratification in Santa Barbara Channel, California.Deep Sea Research 18 (7): 763–769.

Guo, Z., Yang, Z., Hu, D. et al., 1997. Suspended matter of the northern East Chian Sea in the spring: its distribution structure and effect on sedimentation.Oceanologia et Limnologia Sinica 28 (supplement): 66–72. (in Chinese with English abstract)

Lei, K., Bai, H., 1997. Comparison and analysis of suspended matter concentration and light transmission in the East China Sea Cold Eddy region. Abstract in: Symposium on “The study of key processes in the material flux in the East China Sea” (in Chinese), Qingdao, December 14–15, 1997, p: 34–35.

Lei, K., Yang, Z., Guo, Z. et al., 2001. Suspended sediment flux in spring on the East China Sea shelf with different surface sediment types.Oceanologia et Limnologia Sinica 32 (1): 50–57. (in Chinese with English abstract)

Milliman, J., Hsueh, Y., Hu, D. 1984. Tidal phase control of sediment discharge from the Yangtze River.Estuarine, Coastal and Shelf Science 19 (1): 119–128.

Qin, Y., Li, F., Xu, S. et al., 1989a. Study on suspended matter in seawater in the south Huanghai SeaOceanologia et Limnologia Sinica 20 (2): 101–111. (in Chinese)

Qin, Y., Zhao, Y., Chen, L. et al., 1989b. Sediment on the bottom in the Yellow Sea.In: Geology of the Yellow Sea, China Ocean Press, Beijing, p: 71–74 (in Chinese).

Yang, Z., Milliman, J., Fitzgerald, M. 1982. Transfer of water and sediment from the Changjiang River to the East China Sea in June 1980.Can. J. Fish. Aquatic Sci. 40 (suppl. 1): 72–82.

Yang, Z., Guo, Z., Wang, S. et al., 1991. Suspended matter in the Huanghai Sea and East China Sea: its contents, relation to the water masses and factors of influence.Journal of Ocean University of Qingdao 21 (3): 55–69. (in Chinese)

Yang Z., Guo, Z., Wang, Z. et al., 1992. Basic pattern of transportation of suspended matter from the Yellow Sea and East China Sea to the east deep sea.Acta Oceanologica Sinica 14 (2): 81–90. (in Chinese)

Zhao, B. Hu, D., Xiong, Q. 1986. Distribution of transmission and its relation to circulation in the southern Yellow Sea in late autumn.Studia Marina Sinica 27: 97–105 (in Chinese with English abstract)

Su, Y., 1989. A Survey of Geographical Environment Circulation System in, the Huanghai Sea and East China Sea.Journal of Ocean University of Qingdao 19 (1) (II): 145–158. (in Chinese with English abstract)

浏览量

Downloads

CSCD

文章被引用时，请邮件提醒。

Submit

工具集

关联资源

Effect of sea surface temperature during critical early life history stages of Portunustrituberculatus on later yield

Spatio-temporal variability of surface chlorophyll a in the Yellow Sea and the East China Sea based on reconstructions of satellite data of 2001–2020

Physical processes determining the distribution patterns of Nemopilemanomurai in the East China Sea

A two-year (2020–2021) observation of marine phycotoxins in phytoplankton in typical mariculture areas of East China Sea

Two new species of Leodamas Kinberg, 1866 (Annelida, Orbiniidae) from China seas