Upwelling and sedimentation dynamics III: Coincidence of upwelling areas with mud patches in north hemisphere shelf seas

Pang Chong-guang; Hu Dun-xin

doi:10.1007/BF02849645

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Upwelling and sedimentation dynamics III: Coincidence of upwelling areas with mud patches in north hemisphere shelf seas

Updated：2023-05-16

- Upwelling and sedimentation dynamics III: Coincidence of upwelling areas with mud patches in north hemisphere shelf seas
- Journal of Oceanology and Limnology Vol. 20, Issue 2, Pages: 101-106(2002)
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/BF02849645
  CLC：
- Published：2002
- Accepted：
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Chong-guang, P., Dun-xin, H. Upwelling and sedimentation dynamics III: Coincidence of upwelling areas with mud patches in north hemisphere shelf seas., Chin. J. Ocean. Limnol. 20, 101–106 (2002). https://doi.org/10.1007/BF02849645
DOI：

Chong-guang, P., Dun-xin, H. Upwelling and sedimentation dynamics III: Coincidence of upwelling areas with mud patches in north hemisphere shelf seas., Chin. J. Ocean. Limnol. 20, 101–106 (2002). https://doi.org/10.1007/BF02849645 DOI：

摘要

Abstract

The determinant role of upwelling in fine sediment patches is examined from the viewpoints of physical process and biological process respectively. It is pointed out that physical and biological processes are usually coexistent and interact with each other during the sedimentation of suspended matters. This study used available figures showing the circulation pattern and surface sediment distribution in the whole China Seas

the Gulf of Maine

the Irish Sea and the North Sea

and additional data to verify that wherever upwelling exists on the continental shelf

mud must occur; and that wherever downwelling occurs

coarse sediment substitutes for mud.

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references

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