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Heat Budget at Gampo in the Eastern Coast of Korea in 2006

2006년 동해안 감포의 열수지

  • Choi, Yong-Kyu (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Han, In-Seong (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Suh, Young-Sang (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Go, Woo-Jin (Ocean Research Team, National Fisheries Research and Development Institute) ;
  • Kim, Sang-Woo (Ocean Research Team, National Fisheries Research and Development Institute)
  • 최용규 (국립수산과학원 해양연구과) ;
  • 한인성 (국립수산과학원 해양연구과) ;
  • 서영상 (국립수산과학원 해양연구과) ;
  • 고우진 (국립수산과학원 해양연구과) ;
  • 김상우 (국립수산과학원 해양연구과)
  • Published : 2009.01.31

Abstract

Based on the monthly weather report of Korea Meteorological Administration (KMA) and daily sea surface temperature (SST) data from National Fisheries Research and Development Institute (NFRDI) in 2006, heat budget was estimated at Gampo in the eastern coast of Korea, the region occuring the cold water known as upwelling in summer. Net heat flux was transported from the air to the sea surface during February to November, and it amounts to $345Wm^{-2}$ in monthly mean value. During December to January, the transfer of net heat flux was conversed from the sea surface to the air with $-56Wm^{-2}$ in minimum of monthly mean value in January. Long wave radiation was ranged from $6Wm^{-2}\;to\;106Wm^{-2}$. Sensible heat was varied from $-36Wm^{-2}$(June) to $61Wm^{-2}$(February) and showed negative values from April to August. Latent heat showed $20Wm^{-2}$(July) with its minimum in July and $49Wm^{-2}$ with its maximum in March in monthly mean value. The annual mean of net heat flux is $129Wm^{-2}$, giving an annual heat surplus of $22Wm^{-2}$. Thus, during summer, the upwelled cold water at Gampo, appears to compensate the heat gain. However the ways in which these compensations are accomplished remains to be clarified.

Keywords

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