地球科学进展 ›› 2001, Vol. 16 ›› Issue (2): 215 -219. doi: 10.11867/j.issn.1001-8166.2001.02.0215

综述与评述 上一篇    下一篇

  1. 中国科学院南海海洋研究所,广东 广州  510301
  • 收稿日期:2000-05-20 修回日期:2000-08-03 出版日期:2001-04-01
  • 通讯作者: 蔡树群(1968-),男,广东澄海人,副研究员,主要从事海流数值模拟、内波研究. E-mail:caisq@scsio.ac.cn
  • 基金资助:



CAI Shu-qun,GAN Zi-jun   

  1. South China Sea Institute of Oceanology,CAS,Guangzhou  510301,China
  • Received:2000-05-20 Revised:2000-08-03 Online:2001-04-01 Published:2001-04-01


Internal solition is the large amplitude wave existing in the pycnocline induced by internal tide in the condition of special bottom topography. During the propagation process of internal solition,the induced disturbance can bring about strong convergence of sea surface water and sudden strong current(wave-induced current),which can cause severe threat to the ocean engineering, oil drilling platform and sea bottom oil pipeline.The dynamic state of the international study on oceanic internal soliton is introduced,the internal solition phenomena existing in the northern South China Sea(SCS) is described,some problems about internal solition study now in SCS are discussed,and the study thought is put forward.


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