Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea

Feng Ming; Bai Hong; Hu Dun-xin; Wang Fan

doi:10.1007/BF02842567

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Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea

OriginalPaper | Updated：2023-05-16

- Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea
- Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea
- 海洋湖沼学报（英文） 2000年18卷第2期页码：97-103
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
  
  Contribution No. 3868 from the Institute of Oceanology, Chinese Academy of Sciences.;Project 49636210 supported by NSFC.
- DOI：10.1007/BF02842567
  中图分类号：
- 纸质出版：2000
- Accepted：
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Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea[J]. 海洋湖沼学报（英文）, 2000,18(2):97-103.

Ming, F., Hong, B., Dun-xin, H. et al. Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea., Chin. J. Ocean. Limnol. 18, 97–103 (2000). https://doi.org/10.1007/BF02842567
Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea[J]. 海洋湖沼学报（英文）, 2000,18(2):97-103. DOI： 10.1007/BF02842567.

Ming, F., Hong, B., Dun-xin, H. et al. Temporal variations of hydrology and light transmission at two fixed observation stations in the East China Sea., Chin. J. Ocean. Limnol. 18, 97–103 (2000). https://doi.org/10.1007/BF02842567 DOI：

摘要

Abstract

The temporal variations of the hydrology and light transmission at two fixed position observation stations in the East China Sea (ECS) during February to March 1997 were analyzed. The fixed position observations were conducted at 29°28'N

124°45'E (Station 409)

the center of the PN section

and at 32°N

126°E (Station 111)

the center of the ECS Cold Eddy. The results indicate: the semidiurnal tide generated semidiurnal variations of temperature

salinity and light transmission due to horizontal advection

but the resuspension effect of the semidiurnal tide still need to be analyzed; the sea surface diurnal temperature range was as large as 0.2°C during low wind period; the resuspension due to wind disturbance at the two stations (with water depth of more than 80 m) seemed to be small; from late February to early March

the near bottom water temperature as well as light transmission at Station 111 sharply decreased.

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references

Bai, H., Wang, F., Jin, Z., 1999. Light light transmission and its relation to sediment transportation along 32°N-and PN-sections in East China Sea in winter 1997. Proceedings of an international workshop on sediment transport and storage in coastal sea-ocean system, Tsukuba, Japan, March 15–19, 1999, p. 91–95.

Guo, Z., Yang, Z., Fan, D. et al., 1997. The Study of sedimentation dynamics in the East China Sea Cold Eddy region. I: seasonal variability. Abstract in: Symposium on “The study of key processes in the material flux in the East China Sea”, Qingdao, December 14, 1997, p. 28–29. (in Chinese)

Hu, D., 1984. Upwelling and sedimentation dynamics. I: The role of upwelling in sedimentation in the Huanghe Sea and East China Sea--a description of general features.Chin. J. Oceanol. Limnol. 2(1): 12–19.

Hu, D., 1995. The role of vertical circulation in sediment dynamics.In: Ye D., Lin H. et al. ed., China Contribution to Global Change Studies. Science Press, Beijing, p. 168–170.

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”, Qingdao, December 14, 1997, p. 34–35. (in Chinese)

Li, F., Li, P., Zhang, X. et al., 1997. Transport of suspended matter from the Changjiang River to the East China Sea shelf.Chin. J. Oceanol. Limnol. 15(3): 264–270.

Peng, M., Hu, D., 1997. Outflow of suspended materials from the Changjiang River mouth.Chin. J. Oceanol. Limnol. 15(3): 258–263.

Qu, T., Hu, D., 1993. Upwelling and sedimentation dynamics II: A simple model.Chin. J. Oceanol. Limnol. 11(4): 289–295.

Yang, Z., Saito, Y., Guo, Z. et al., 1995. Distal mud area as a material sink in the East China Sea.In: Tsunogai et al. ed., Global fluxes of carbon and its related substances in the coastal sea-ocean-atmosphere system. M & J International Press, Japan, 1995: p. 1–6.

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