DOI QR코드

DOI QR Code

Estimation of Effective Range of HFR Data and Analysis of M2 Tidal Current Characteristics in the Jeju Strait

제주해협 HFR 자료의 유효 범위 산정과 M2 조류 특성 분석

  • Oh, Kyung-Hee (Ocean Circulation and Climate Research Center, Korea Institute of Ocean Science & Technology) ;
  • Lee, Seok (Ocean Circulation and Climate Research Center, Korea Institute of Ocean Science & Technology) ;
  • Park, Joonseong (Instrumental Development and Management Center, Korea Institute of Ocean Science & Technology) ;
  • Song, Kyu-Min (Ocean Circulation and Climate Research Center, Korea Institute of Ocean Science & Technology) ;
  • Jung, Dawoon (Ocean Circulation and Climate Research Center, Korea Institute of Ocean Science & Technology)
  • 오경희 (한국해양과학기술원 해양순환.기후연구센터) ;
  • 이석 (한국해양과학기술원 해양순환.기후연구센터) ;
  • 박준성 (한국해양과학기술원 해양기기개발.운영센터) ;
  • 송규민 (한국해양과학기술원 해양순환.기후연구센터) ;
  • 정다운 (한국해양과학기술원 해양순환.기후연구센터)
  • Received : 2020.02.03
  • Accepted : 2020.05.25
  • Published : 2020.06.30

Abstract

The effective range of surface current data observed by high-frequency radar (HFR) operated in the northern coastal area of Jeju Island by Korea Institute of Ocean Science and Technology was estimated and the distribution and variability of the M2 tidal current of the Jeju Strait was analyzed. To evaluate the HFR data, the M2 tidal current corrected from 25 hours current data observed by the Korea Hydrographic and Oceanographic Agency (KHOA) was compared with the M2 tidal current in the Jeju Strait analyzed from the surface currents of HFR. The reliability of HFR data was confirmed by analyzing the characteristics of the tide components of these two data sets, and the effective range of HFR data was estimated through temporal and spatial analysis. The observation periods of HFR used in the analysis were from 2012 to 2014, and it was confirmed that there is a difference in the effective range of HFR data according to the observation time. During the analysis periods, the difference between the M2 current ellipses from the data of KHOA and the HFR was greater in the eastern than in the western part of the Jeju Strait, and represented a high reliability in the western and central parts of the Jeju Strait. The tidal current of the Jeju Strait analyzed using the HFR data revealed a seasonal variability a relatively weak in summer and a strong in winter, about a 17% fluctuations between the summer and winter based on the length of the semi-major axis of tidal ellipse. Appraisals and results of regarding the characteristics and seasonal variability of the M2 tidal current in the Jeju Strait using HFR data have not been previously reported, so the results of this study are considered meaningful.

Keywords

References

  1. Kim C-S, Lee S-H, Son Y-T, Kwon H-K, Lee K-H, Kim Y-B, Jeong O-J (2006) Changes of surface $M_2$ currents as onserved by HF radar before and after Saemangeum fourth tidal dyke closing. J Kor Soc Oceanog 11(2):37-48
  2. Kim C-S, Lee S-H, Son Y-T, Kwon H-K, Lee K-H, Choi B-J (2008) Variations in subtidal surface currents observed with HF radar in the costal waters off the Saemangeum areas. J Kor Soc Oceanog 13(1):56-66
  3. Song K-M, Cho C-H (2012) Effective installation and operating of high frequency ocean surface radars in Korea - part 1: hardware. Ocean Polar Res 34(4):453-462 https://doi.org/10.4217/OPR.2012.34.4.453
  4. Lee SH, Moon HB, Baek HY, KIM CS, Son YT, Kwon HK, Choi BJ (2008) Accuracy of HF radar-derived surface current data in the coastal waters off the Keum river estuary. J Kor Soc Oceanog 13(1):42-55
  5. Choi BH, Chung HW, Cho Y-K (1995) Tidal computations for the southwestern sea of Korea. J Korean Soc Coast Ocean Eng 7(2):163-169
  6. Choi YG, Kim H-K, Lee D-H, Song K-M, Kim D-H (2016) Short-Term variavility analysis of the HF-Radar data and its classification scheme. J Korean Soc Coast Ocean Eng 28(6):319-331 https://doi.org/10.9765/KSCOE.2016.28.6.319
  7. Bell C, Vassie JM, Woodworth PL (1999) POL/PSMSL tidal analysis software kit 2000 (Task-2000). Permanent service for mean sea level, Birkenhead, 21 p
  8. Chapman RD, Shay LK, Graber HC, Edaon JB, Karachintsev A, Trump CL, Ross DB (1997) On the accuracy of HFR surface current measurements: Inter-comparisons with shipbased sensors. J Geophys Res 102(C8):18737-18748 https://doi.org/10.1029/97JC00049
  9. Choi J-W, Song K-M, Choi J-Y (2019) Accuracy improvement of particle tracking model using 2-D current measurement (HF-radar) data. J Coastal Res 91:251-255 https://doi.org/10.2112/SI91-051.1
  10. Crombie DD (1955) Doppler spectrum of sea echo at 13.56 Mc/s. Nature 175:681-682 https://doi.org/10.1038/175681a0
  11. Harlan J, Terrill E, Hazard L, Keen C, Barrick D, Whelan C, Howden S, Kohut J (2010) The integrated ocean observing system high-frequency radar network: Status and local, regional, and national applications. Mar Technol Soc J 44(6):122-132 https://doi.org/10.4031/MTSJ.44.6.6
  12. Kang SK, Foeman MGG, Lie H-J, Lee J-H, Cherniawsky J, Yum K-D (2002) Two-layer tidal modeling of the Yellow and East China Seas with application to seasonal variability of the $M_2$ tide. J Geophys Res 107(C3):1-19
  13. Lee S, Lie H-J, Cho C-H, Kang SK, Teague WJ, Chang K-I, Song K-M, Oh K-H (2011) Vertical structure of the $M_2$ tidal current in the Yellow Sea. Ocean Sci J 46(2):73-84 https://doi.org/10.1007/s12601-011-0007-x
  14. Lee S, Oh K-H, Jang S-T, You HY, Park J, Song K-M (2019) $M_2$ tidal current estimation from one-day observation data off the western and southern coasts of Korea. Ocean Sci J 54(1):39-50 https://doi.org/10.1007/s12601-018-0062-7
  15. Seasonde (2009) Seasonde information. http://www.support.seasonde.com/index.php Accessed 2 Nov 2012
  16. Son Y-T, Lee S-H, Kim C-S, Lee JC, Lee G-H (2007) Surface current variability in the Keum River Esturay (South Korea) during summer 2002 as observed by high-frequency radar and coastal monitoring buoy. Cont Shelf Res 27:43-63 https://doi.org/10.1016/j.csr.2006.08.008