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Evaluation of Temperature and Salinity Fields of HYCOM Reanalysis Data in the East Sea

HYCOM 재분석 자료가 재현한 동해 수온 및 염분 평가

  • Hong, JinSil (Department of Marine Sciences and Convergent Technology, College of Science and Technology Hanyang University) ;
  • Seo, Seongbong (Ocean Circulation and Climate Research Division, KIOST) ;
  • Jeon, Chanhyung (Department of Marine Science and Biological Engineering, Graduate School Inha University) ;
  • Park, Jae-Hun (Department of Ocean Sciences, College of Natural Science, Inha University) ;
  • Park, Young-Gyu (Ocean Circulation and Climate Research Division, KIOST) ;
  • Min, Hong Sik (Ocean Circulation and Climate Research Division, KIOST)
  • 홍진실 (한양대학교 과학기술대학 해양융합과학과) ;
  • 서성봉 (한국해양과학기술원 해양순환기후연구센터) ;
  • 전찬형 (인하대학교 일반대학원 해양과학.생물공학과) ;
  • 박재훈 (인하대학교 자연과학대학 해양과학과) ;
  • 박영규 (한국해양과학기술원 해양순환기후연구센터) ;
  • 민홍식 (한국해양과학기술원 해양순환기후연구센터)
  • Received : 2016.06.27
  • Accepted : 2016.12.19
  • Published : 2016.12.30

Abstract

We evaluate the temperature and salinity fields in the East Sea reproduced by the global ocean reanalysis data using HYbrid Coordinate Ocean Model (HYCOM for short). Temporal correlation of Sea Surface Temperature (SST) change between HYCOM and the Group for High Resolution Sea Surface Temperature (GHRSST) are higher in summer than winter. Though distributions of temperature and salinity in the HYCOM are similar to those from historical data (World Ocean Atlas 2013 V2), salinity in the HYCOM is lower (highter) in the region where the salinity is high (low). Temperature fields in the Ulleung basin of HYCOM are quite similar to those derived from Pressure-recording Inverted Echo Sounder (PIES), such as the correlation coefficient is higher than 0.7. This indicates that the HYCOM represents well the circulation and meso-scale phenomena in the Ulleung basin.

Keywords

References

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