Korean Journal of Fisheries and Aquatic Sciences (한국수산과학회지)

The Korean Society of Fisheries and Aquatic Science (한국수산과학회)
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Short-term Variation of Sea Surface Temperature Caused by Typhoon Nabi in the Eastern Sea of Korean Peninsula Derived from Satellite Data

위성영상에서 관측한 태풍 Nabi 통과시의 한반도 동부해역 수온의 단기변동

  • Kim, Sang-Woo (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Yamada, Keiko (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Jang, Lee-Hyun (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Hong, Chul-Hoon (Department of Marine Production Management, Pukyong National University) ;
  • Go, Woo-Jin (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Suh, Young-Sang (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Lee, Chu (Aquaculture Research Team, East Sea Fisheries Research Institute, NFRDI) ;
  • Lee, Gyu-Hyong (Ocean Environmental System Program, Chonnam National University)
  • 김상우 (국립수산과학원 해양연구팀) ;
  • 야마다게이꼬 (국립수산과학원 해양연구팀) ;
  • 장이현 (국립수산과학원 해양연구팀) ;
  • 홍철훈 (부경대학교 해양생산관리학과) ;
  • 고우진 (국립수산과학원 해양연구팀) ;
  • 서영상 (국립수산과학원 해양연구팀) ;
  • 이주 (동해수산연구소 증식연구팀) ;
  • 이규형 (전남대학교 해양시스템보전)
  • Published : 2007.04.30
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Abstract

A remarkable sea surface cooling (SSC) event was observed in the eastern sea of Korean peninsula based on new generation sea surface temperature (NGSST) satellite images in September 2005, when typhoon Nabi passed over the East Sea. The degree of SSC ranged from $1^{\circ}C\;to\;4^{\circ}C$, and its maximum was observed in the southeastern sea area. Daily variations in sea surface temperature at a longitudinal line $(35^{\circ}-41^{\circ}N,\;132^{\circ}E)$, derived from satellite data for September 1-13, 2005, showed that the SSC lasted about 3 days after the typhoon passed in the south of $39^{\circ}N$, whereas it was unclear in the north of$39^{\circ}N$. Water temperature measured by a mooring buoy suggested that the SSC was caused mainly by a vertical mixing of the water column driven by the typhoon, rather than by coastal upwelling.

Keywords

References

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