The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River

M. F. Gerstell

doi:10.1007/BF02850522

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The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River

OriginalPaper | Updated：2023-05-16

- The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River
- The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River
- 海洋湖沼学报（英文） 1995年13卷第3期页码：223-225
- Affiliations：
  
  Dept. of Planetary Sciences
- Author bio：
- Funds：
- DOI：10.1007/BF02850522
  中图分类号：
- 纸质出版：1995
- Accepted：
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The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River[J]. 海洋湖沼学报（英文）, 1995,13(3):223-225.

Gerstell, M.F. The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River., Chin. J. Ocean. Limnol. 13, 223–225 (1995). https://doi.org/10.1007/BF02850522
The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River[J]. 海洋湖沼学报（英文）, 1995,13(3):223-225. DOI： 10.1007/BF02850522.

Gerstell, M.F. The Kuroshio Meander/Southern Oscillation connection and drought/flood cycles in the Changjiang River., Chin. J. Ocean. Limnol. 13, 223–225 (1995). https://doi.org/10.1007/BF02850522 DOI：

摘要

Abstract

In response to a suggestion that the large meander of the Kuroshio is a good predictor of droughts in the Changjiang River Valley

it is argued that more recent inceptions of the meander lend statistical weight to the belief that the large meander is itself a consequence of E1 Niño

and hence of the Southern Oscillation. The meander usually lags. Thus

if the meander reliably predicts droughts

the Tahiti component of the Southern Oscillation will usually give six months' extra warning.

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Keywords

references

Cayan, D. R. and Webb, E. H., 1992. El Niño/Southern Oscillation and streamflow in the western United States.In: El Niño: Historical and Paleoclimatic Aspects of the Southern Oscillation, H. F. Diaz and V. Markgraf, eds. Cambridge Univ. Press, New York.

Diaz, H. F. and Kiladis, G. N., 1992. Atmospheric teleconnections associated with extreme phases of the Southern Oscillation.In: El Niño: Historical and Paleoclimatic Aspects of the Southern Oscillation, H. F. Diaz and V. Markgraf, eds., Cambridge Univ. Press, New York.

He, Y. and White, W. B., 1987. Interannual variability of the Kuroshio frontal structure along its western boundary in the North Pacific Oceean, associated with the 1982 ENSO event.J. Phys. Oceanog. 17: 1494–1506.

Qiu, B. and Joyce, T. M., 1992. Interannual variability in the middle and low-latitude western North Pacific.J. Phys. Oceanog. 22: 1062–1079.

Shi Maochong, Wang Xiaoqing, and Jing Zhenhua, 1989. Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region. Chin.J. Oceanol. Limnol. 7: 312–317.

Shoji, D., 1972. Time variation of the Kuroshio South of Japan.In: Kuroshio: Physical Aspects of the Japan Current, H. Stommel and K. Yoshida, eds. Univ. of Washington Press, Seattle.

Uda, M., 1962. Cyclic, correlated occurrence of worldwide anomalous oceanographic phenomena and fisheries conditions.J. Oceanogr. Soc. jap. 20th Anniv, pp. 368–376.

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