A subsurface intensity index of the cold eddy in the East China Sea

Jian Lan; Yi Wang; Gang Wang

doi:10.1007/s00343-010-9015-4

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A subsurface intensity index of the cold eddy in the East China Sea

Updated：2023-05-16

- A subsurface intensity index of the cold eddy in the East China Sea
- Journal of Oceanology and Limnology Vol. 28, Issue 6, Pages: 1275-1280(2010)
- Affiliations：
  
  College of Physical and Environmental Oceanography Ocean University of China
- Author bio：
- Funds：
- DOI：10.1007/s00343-010-9015-4
  CLC：
- Online First：10 November 2010，
  
  Published：2010
- Accepted：
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Lan, J., Wang, Y. & Wang, G. A subsurface intensity index of the cold eddy in the East China Sea., Chin. J. Ocean. Limnol. 28, 1275–1280 (2010). https://doi.org/10.1007/s00343-010-9015-4
DOI：

Lan, J., Wang, Y. & Wang, G. A subsurface intensity index of the cold eddy in the East China Sea., Chin. J. Ocean. Limnol. 28, 1275–1280 (2010). https://doi.org/10.1007/s00343-010-9015-4 DOI：

摘要

Abstract

The Cold Eddy in the East China Sea (CEECS) is located about 150 km southwest of Cheju Island. This region experiences a complex current system under the influences of the Yellow Sea Warm Current (YSWC)

the Yellow Sea Coastal Current (YSCC)

and the northward Kuroshio residual. To identify the strength of the CEECS

a simple subsurface intensity index is developed. Because the CEECS can be traced by temperature minimum

the intensity index is determined by the difference in sea temperature averaged across cores within and surrounding the region. Based on SODA

the CEECS subsurface intensity index time series can be calculated

with which the inter-annual variation of the CEECS is analyzed.

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references

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