Monitoring the diffusion of suspended sediments and stability of tidal radial sand ridges area using multi-satellite remote sensing data

Huang Hai-jun; He Yi-jun

doi:10.1007/BF02850741

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Monitoring the diffusion of suspended sediments and stability of tidal radial sand ridges area using multi-satellite remote sensing data

Updated：2023-05-16

- Monitoring the diffusion of suspended sediments and stability of tidal radial sand ridges area using multi-satellite remote sensing data
- Journal of Oceanology and Limnology Vol. 19, Issue 4, Pages: 361-367(2001)
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/BF02850741
  CLC：
- Published：2001
- Accepted：
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Hai-jun, H., Yi-jun, H. Monitoring the diffusion of suspended sediments and stability of tidal radial sand ridges area using multi-satellite remote sensing data., Chin. J. Ocean. Limnol. 19, 361–367 (2001). https://doi.org/10.1007/BF02850741
DOI：

Hai-jun, H., Yi-jun, H. Monitoring the diffusion of suspended sediments and stability of tidal radial sand ridges area using multi-satellite remote sensing data., Chin. J. Ocean. Limnol. 19, 361–367 (2001). https://doi.org/10.1007/BF02850741 DOI：

摘要

Abstract

Nine Landsat TM tapes and images and MSS images

10 NOAA tapes and images and 1 SAR image from 1973 to 1997 were used to analyze the diffusion of suspended sediments and the change of tidal radial sand ridges in the northern part of the Changjiang River delta

the South Yellow Sea. The results showed that the diffusion of suspended sediments was controlled by the tide

net current

and submarine topography in this area. The distribution of suspended sediments had close relationship with the submarine topography. The old Huanghe River delta and the Changjiang River comprise the main sediment supply for the formation of radial sand ridges

whose evolution can be divided into three stages since the Huanghe River changed its course and flowed northward into the Bohai Sea.

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references

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