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JIA Yongjun,ZHANG Youguang,LIN Mingsen.The numerical simulation of the Kuroshio frontal eddies in the East China Sea using a hybrid coordinate ocean mode[J].Acta Oceanologica Sinica,2013,32(5):31-41
The numerical simulation of the Kuroshio frontal eddies in the East China Sea using a hybrid coordinate ocean mode
The numerical simulation of the Kuroshio frontal eddies in the East China Sea using a hybrid coordinate ocean mode
投稿时间:2011-08-24  修订日期:2012-05-22
DOI:10.1007/s13131-013-0311-7
中文关键词:  Kuroshio frontal eddies  hybrid coordinate ocean model  East China Sea
英文关键词:Kuroshio frontal eddies  hybrid coordinate ocean model  East China Sea
基金项目:The State Oceanic Administration Youth Funds of China under contract No. 2012403; the Public Science and Technology Research Funds Projects of Ocean of China under contract No. 201005030; the Special Funds for Basic Scientific Research Project of the First Institute of Oceanography, the State Ocean Administration of China under contract No. 2010G12; Water Marine Remote Sensing Survey and Research of China under contract No. 908-01-ST10(II); China's Coastal Marine Optics and Remote Sensing Research under contract No. 908-ZC-I-04.
作者单位E-mail
JIA Yongjun National Satellite Ocean Application Service, State Oceanic Administion, Beijing 100081, China jiayongjun@mail.nsoas.gov.cn 
ZHANG Youguang National Satellite Ocean Application Service, State Oceanic Administion, Beijing 100081, China  
LIN Mingsen National Satellite Ocean Application Service, State Oceanic Administion, Beijing 100081, China  
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中文摘要:
      A hybrid coordinate ocean model (HYCOM) is used to simulate the Kuroshio frontal eddies in the East China Sea (ECS). The research area is located (20°-32°N, 120°-132°E). Using the simulating data, it is figured out that the Kuroshio frontal eddies occur in summer as well as in the other season in this area. The life cycle of the Kuroshio and its frontal eddies is different with the position. The life-cycle of the Kuroshio frontal eddies of the northwest Diaoyu Islands is about 14 d; and the life cycle of the Kuroshio frontal eddies of southwest Yakushima about 20 d. This result extends the in situ researching results greatly. In addition, the vertical impact depth of the Kuroshio frontal eddies is also changing with the position. On the whole, in the ECS, the maximum impact depth of the Kuroshio frontal eddies of the northwest Taiwan Islands is about 75 m; the maximum impact depth of the Kuroshio frontal eddies of the northwest Diaoyu Islands is more than 125 m, but no more than 200 m; and the maximum impact depth of the Kuroshio frontal eddies of southwest Yakushima is up to 100 m.
英文摘要:
      A hybrid coordinate ocean model (HYCOM) is used to simulate the Kuroshio frontal eddies in the East China Sea (ECS). The research area is located (20°-32°N, 120°-132°E). Using the simulating data, it is figured out that the Kuroshio frontal eddies occur in summer as well as in the other season in this area. The life cycle of the Kuroshio and its frontal eddies is different with the position. The life-cycle of the Kuroshio frontal eddies of the northwest Diaoyu Islands is about 14 d; and the life cycle of the Kuroshio frontal eddies of southwest Yakushima about 20 d. This result extends the in situ researching results greatly. In addition, the vertical impact depth of the Kuroshio frontal eddies is also changing with the position. On the whole, in the ECS, the maximum impact depth of the Kuroshio frontal eddies of the northwest Taiwan Islands is about 75 m; the maximum impact depth of the Kuroshio frontal eddies of the northwest Diaoyu Islands is more than 125 m, but no more than 200 m; and the maximum impact depth of the Kuroshio frontal eddies of southwest Yakushima is up to 100 m.
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