DOI QR코드

DOI QR Code

해양기상부이와 표류부이에서 관측된 유의파고 및 파주기 비교 분석

Comparative Analysis of Significant Wave Height and Wave Period Observed from Ocean Data and Drifting Buoys

  • 조형준 (국립기상과학원 관측연구부) ;
  • 김백조 (국립기상과학원 관측연구부) ;
  • 최규용 (국립기상과학원 관측연구부) ;
  • 노민 (한국해양과학기술원 해양공간개발.에너지연구부) ;
  • 강기룡 (기상청 지진화산국 지진화산기술팀) ;
  • 이철규 (국립기상과학원 관측연구부)
  • Hyeong-Jun Jo (Observation Research Department, National Institute of Meteorological Sciences) ;
  • Baek-Jo Kim (Observation Research Department, National Institute of Meteorological Sciences) ;
  • Reno Kyu-Young Choi (Observation Research Department, National Institute of Meteorological Sciences) ;
  • Min Roh (Ocean Space Development and Energy Research Department, Korea Institute of Ocean Science & Technology) ;
  • KiRyong Kang (Earthquake and Volcano Technology Team, Earthquake and Volcano Bureau, Korea Meteorological Administration) ;
  • Chul-Kyu Lee (Observation Research Department, National Institute of Meteorological Sciences)
  • 투고 : 2023.11.14
  • 심사 : 2023.11.23
  • 발행 : 2023.11.30

초록

In this study, the significant wave height and wave period of a specially designed observation system that connected two drifting buoys to an ocean data buoy was observed for 23 days from February 7 to 29, 2020, and the results were compared and analyzed. The results indicated that, in comparison to the ocean data buoy, the drifting buoy exhibited greater variability in significant wave height over shorter time intervals. The wave period of the ocean data buoy also appeared longer than that of the drifting buoy. The greater the observed significant wave height and wave period from both the ocean data and drifting buoys, the more pronounced the differences between the two observation instruments become. Moreover, the study revealed that the disparity in observation methods between the ocean data and drifting buoys did not significantly affect the significant wave height characteristics, as long as the period remained unchanged for up to half of the observation time.

키워드

과제정보

이 연구는 기상청 국립기상과학원 「해양기상 감시 및 차세대 혜양예측시스템 개발」(KMA2018-00420)의 지원으로 수행되었습니다. 해양기상부이 및 표류부이 관측 업무를 수행한 국립기상과학원 기상관측선 기상1호 관계자 분들에게 감사의 말씀을 드립니다.

참고문헌

  1. Doble, M. J., Bidlot, J. R., 2013, Wave buoy measurements at the Antarctic sea ice edge compared with an enhanced ECMWF WAM: Progress towards global waves-in-ice modelling, Ocean Model, 70, 166-173. https://doi.org/10.1016/j.ocemod.2013.05.012
  2. Hisaki, Y., 2021, Validation of drifting buoy data for ocean wave observation, J. of Mar. Sci. Eng., 729, 1-13. https://doi.org/10.3390/jmse9070729
  3. Hisaki, Y., 2018, Wave hindcast in the North Pacific area considering the propagation of surface disturbance, Prog. Oceanogr., 165, 332-347. https://doi.org/10.1016/j.pocean.2018.06.003
  4. Huh, Y., Hwang, C. S., Kim, D. H., Heo, S., Kim, J. Y., Lee, K. W., Hong, S. D., 2012, Performance evaluation of wave observation system using GPS, J. Korea Soc. Mar. Environ. Eng., 15, 357-362. https://doi.org/10.7846/JKOSMEE.2012.15.4.357
  5. Jeong, W. M., Oh, S. H., Cho, H. Y, Baek, W. D., 2019, Characteristics of wave continuously observed over six years at offshore central east coast of Korea, J. Korean Soc. of Coast. Ocean Eng., 31, 88-99. https://doi.org/10.9765/KSCOE.2019.31.2.88
  6. Kang, Y. H, Seuk, H. B., Bang, J. H., 2015, Seasonal characteristics of sea surface winds and significant wave heights observed marine meteorological buoys and lighthouse AWSs near the Korean peninsula, J. Environ. Sci. Int., Vol.24, 291-302. https://doi.org/10.5322/JESI.2015.24.3.291
  7. Melville, W. K., 1996, The role of surface-wave breaking in air-sea interaction, Annu. Rev. Fluid Mech., 28, 279-321. https://doi.org/10.1146/annurev.fl.28.010196.001431
  8. Tolman, H., 2002, User manual and system documentation of WAVEWATCH-III version 2.22, Technical Note 222, NOAA/NWS/NCEP/OMB, 133.
  9. Tolman, H. L., Balasubramaniyan, B., Burroughs, L. D., Chalikov, D. V., Chao, Y. Y., Chen, H. S., Gerald, V. M., 2002, Development and implementation of wind generated ocean surface wave models at NCEP, Wea. Forecasting, 17, 311-333. https://doi.org/10.1175/1520-0434(2002)017<0311:DAIOWG>2.0.CO;2
  10. Waseda, T., Sinchi, M., Kiyomatsu, K., Nishida, T., Takahashi, S., Asaumi, S., Kawai, Y., Tamura, H., Miyazawa, Y., 2014, Deep water observations of extreme waves with moored and free GPS buoy, Ocean dyn., 64, 1269-1280. https://doi.org/10.1007/s10236-014-0751-4
  11. Woo, H. J., Park, K. A., Byun, D. S., Lee, J., Lee, E., 2018, Characteristics of the differences between significant wave height at Ieodo ocean research station and satellite altimeter-measured data over a decade (2004~2016), J. Korean Soc. Oceanogr., 23, 1-19.