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Sea Surface Cooling in the East Sea with the Passage of Typhoons

태풍통과시 동해에서의 해수면 냉각현상

  • HONG Chul-Hoon (Department of Marine Production Management, Pukyong National University) ;
  • SOHN Ik-Sung (Department of Marine Production Management, Pukyong National University)
  • 홍철훈 (부경대학교 해양생산관리학과) ;
  • 손익성 (부경대학교 해양생산관리학과)
  • Published : 2004.04.01

Abstract

Sea surface cooling (SSC) with the passage of typhoons is examined in the East Sea using the Japan Meteorological Agency buoy data $(37^{\circ}45'N,\;134^{\circ}23'E)$ during 1983-2000 and a three-dimensional primitive equation model (the Princeton Ocean Model). Forty typhoons in this period induced the SST decrease ranging from about $-0.5^{\circ}C\;to\;-4.3^{\circ}C.$ Intense SSC $(<-2^{\circ}C)$ occurs with typhoons that passed mainly through the left-hand side of the buoy station. The model is implemented to examine a physical process of SSC with a typical-track typhoon in the northwestern Pacific $(24^{\circ}N\;to\;52^{\circ}N).$ The model well reproduces prominent features in the observation and addresses how it happens; SSC is induced mainly by momentum mixing effect stirred with the typhoon rather than upwelling.

Keywords

References

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