The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog

Mark Wimbush; Li Li

doi:10.1007/BF02847832

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The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog

OriginalPaper | Updated：2023-05-16

- The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog
- The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog
- 海洋湖沼学报（英文） 1988年6卷第2期页码：127-134
- Affiliations：
  
  1. Graduate School of Oceanography University of Rhode Island
  2. Third Institute of Oceanography SOA
- Author bio：
- Funds：
- DOI：10.1007/BF02847832
  中图分类号：
- 纸质出版：1988
- Accepted：
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The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog[J]. 海洋湖沼学报（英文）, 1988,6(2):127-134.

Wimbush, M., Li, L. The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog., Chin. J. Ocean. Limnol. 6, 127–134 (1988). https://doi.org/10.1007/BF02847832
The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog[J]. 海洋湖沼学报（英文）, 1988,6(2):127-134. DOI： 10.1007/BF02847832.

Wimbush, M., Li, L. The relationship of current fluctuations on the Southeast United States shelf to fluctuations of the wind and gulf stream and the East China Sea analog., Chin. J. Ocean. Limnol. 6, 127–134 (1988). https://doi.org/10.1007/BF02847832 DOI：

摘要

Abstract

Sub-tidal (1.04–25 day) current fluctuations during winter/spring on the continental shelf off Savannah

Georgia (32°N) and off St. Augustine

Florida (30°N) were compared with records of local wind stress components and GulfStream position. (Acoustic travel time and bottom pressure measurements at stations on the continental slope were combined to determine main

thermocline depth

as an indicator of Gulf Stream displacement). Relative wind influences increased towards the coast. GulfStream influence increased towards the shelf-break and towards the surface. Off Savannah

the Gulf Stream influence was predominately at 12 day period and was negligible at the 45 m isobath. Off St. Augustine

its influence was predominately at 4 day period and was appreciable at the 40 m isobath (but negligeable at the 28 m isobath). Linear predictions of currents from wind and Gulf Stream account for ∼80% of the observed variance. Similar methods of studying and predicting the wind—and Kuroshio-influenced currents on the East China Shelf are proposed.

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references

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