The Western Boundary Current of the pacific and its role in the climate

Hu Dunxin; Cui Maochang

doi:10.1007/BF02849784

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The Western Boundary Current of the pacific and its role in the climate

OriginalPaper | Updated：2023-05-16

- The Western Boundary Current of the pacific and its role in the climate
- The Western Boundary Current of the pacific and its role in the climate
- 海洋湖沼学报（英文） 1991年9卷第1期页码：1-14
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 1791 from the Institute of Oceanology, Academia Sinica.
- DOI：10.1007/BF02849784
  中图分类号：
- 纸质出版：1991
- Accepted：
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The Western Boundary Current of the pacific and its role in the climate[J]. 海洋湖沼学报（英文）, 1991,9(1):1-14.

Dunxin, H., Maochang, C. The Western Boundary Current of the pacific and its role in the climate., Chin. J. Ocean. Limnol. 9, 1–14 (1991). https://doi.org/10.1007/BF02849784
The Western Boundary Current of the pacific and its role in the climate[J]. 海洋湖沼学报（英文）, 1991,9(1):1-14. DOI： 10.1007/BF02849784.

Dunxin, H., Maochang, C. The Western Boundary Current of the pacific and its role in the climate., Chin. J. Ocean. Limnol. 9, 1–14 (1991). https://doi.org/10.1007/BF02849784 DOI：

摘要

Abstract

On the basis of the CTD data gathered by the R/VScience I in each Oct. of 1986–1988 and the winter averaged temperature anomaly in southeast China

the interannual variability of the Western Boundary Current (WBC) is examined in terms of volume transport by inverse calculation and its role in the climate is studied by statistical method. The estimated transport is 50

and 33×106 m3/s for the Kuroshio and 24

and 36×106 m3/s for the Mindanao Current (MC) in October of 1986

1987

and 1988

respectively. The WBC is the biggest channel in the ocean for transporting heat poleward and plays an extremely important role in establishing and maintaining the global heat balance. Results showed that meridional heat transport by the Kuroshio northeast of Luzon apparently dominates coldness or warmness in winter in southeast China. Two phenomena observed in the western Pacific but not in the western Atlantic are the warm pool and the equatorward flowing MC which

together with the North Equatorial Counter-current (NECC) may play an important role in preventing the warm water from extending to the north. So in order to understand the dynamics of the warm pool formation and evolution

the MC and NECC must be studied as well as the Equatorial Current.

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references

Cui, M. and D. Hu, 1990. Inversion calculation of the western boundary current in the Pacific during October 1988.Chin. J. Oceanol. Limnol. 8 (2): 177–187.

Guan, B., 1989. Variation of the Mindanao eddy and its relation with El Niño event.Oceanologia et Limnologia 20 (2): 131–138 (in Chinese with Exglish abstract).

Hasunuma, K. and K. Yoshida, 1978. Splitting of the subtropical gyre in the western North Pacific.J. Oceanogr. Soc. Jap. 34: 160–171.

Hu, D., 1989. A thought on the role of western Pacific Ocean circulation in climate change in southeast China.Chin. J. Oceanol. Limnol. 7 (1): 93–94.

Hu, D. and M. Cui, 1989. The western boundary current in the far-western Pacific Ocean. Proceedings of Western International Meeting and Workship on TOGA COARE, May 24–30, 1989, Noumea, New Caledonia, edited by Joel Picaut, Roger Lukas and Thierry Delcroix, pp. 123–134.

Kishindo, S., 1931. On the method of ocean current observation now used by the Hydrographical Department and some results obtained.Part 3 Hydr. Bull. 109: 483–503 (in Japanese).

Nitani, H., 1970. Oceanographic conditions in the sea east of the Philippines and Luzon Strait in summers of 1965 and 1966.In: The Kuroshio—A Symposium on the Japan Current (edited by J. C. Marr), East-West Center Press, Honolulu, pp. 213–232.

Nitani, H., 1972. Beginning of the Kuroshio. In: Kuroshio—Its Physical Aspects. Tokyo Univ. Press, pp 129–163.

Sverdrup, H. U., M. W. Johnson and R. H. Fleming, 1942. The Oceans—Their Physics, Chemistry and General Biology, Prentice-House, New York, 1087 pp.

Uda, M., 1955. On the subtropical convergence and the currents in the northwest Pacific.Rec. Oceanogr. Works Jap. 2 (1): 141–150.

Wunsch, C., 1978. The north Atlantic circulation west of 50°W determined by inverse methods.Space Phys. 16: 582–620.

White, W. B. and A. E. Walker, 1985. The influence of the Hawaiian Archipelago upon the wind-driven Subtropical Gyre in the western North Pacific.J. Geophis. Res. 90 (c4): 7061–7074.

Wyrtki, K., 1961: Physical oceanography of the Southeast Asian Waters. Scientific Results of Marine Investigations of the South China Sea and Gulf of Thailand, 1959–1961.Naga Report 2: 195.

Yamanaka, H., N. Anraku and J. Morita, 1965. Seasonal and long-term variations in oceanographic conditions in the western North Pacific Ocean.Rep. Nankai Reg. Fish. Res. Lab. 22: 35–70 (in Japanese).

Yoshida, K. and T. Kidokoro, 1967a. A subtropical countercurrent in the North Pacific.—An eastward flow near the Subtropical Convergence.J. Oceanogr. Soc. Jap. 23 (2): 88–91.

Yoshida, K. and T. Kidokoro, 1967b. A subtropical countercurrent (II).—A prediction of eastward flow at lower subtropical latitudes.J. Oceanogr. Soc. Jap. 23 (5): 231–246.

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