Physical and geographical origins of the South China Sea Warm Current

Tzu Ling Chiang, Chau Ron Wu, Shenn Yu Chao

Research output: Contribution to journalArticle

15 Citations (Scopus)

Abstract

We examine the formation mechanism of the South China Sea Warm Current in winter, using a high-resolution, numerical model. The current, noted for its ability to flow against the prevailing northeast monsoon in winter, has received considerable attentions in recent years. The collective wisdom from previous models points to two likely generation scenarios: occasional wind relaxation or the Kuroshio intrusion. The present model consistently points to the wind relaxation as the dominant mechanism. When comparing differences between previous models and ours, we also conclude that the Kuroshio intrusion helps, but is not chiefly responsible. Tracing the current to the source, we identify the elevated sea level in the Gulf of Tonkin, induced by the northeast monsoon, as the ultimate driving force. The presence of Hainan Island bears little importance in generating the current.

Original languageEnglish
Article numberC08028
JournalJournal of Geophysical Research: Oceans
Volume113
Issue number8
DOIs
Publication statusPublished - 2008 Aug 8

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South China Sea
China
monsoons
monsoon
intrusion
winter
Sea level
formation mechanism
gulfs
Numerical models
tracing
bears
sea level
sea
high resolution

ASJC Scopus subject areas

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Physical and geographical origins of the South China Sea Warm Current. / Chiang, Tzu Ling; Wu, Chau Ron; Chao, Shenn Yu.

In: Journal of Geophysical Research: Oceans, Vol. 113, No. 8, C08028, 08.08.2008.

Research output: Contribution to journalArticle

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