DOI QR코드

DOI QR Code

Bias-Aware Numerical Surface Temperature Prediction System in Cheonsu Bay during Summer and Sensitivity Experiments

편향보정을 고려한 수치모델 기반 여름철 천수만 수온예측시스템과 예측성능 개선을 위한 민감도 실험

  • Young-Joo Jung (Department of Oceanography, Chonnam National University) ;
  • Byoung-Ju Choi (Department of Oceanography, Chonnam National University) ;
  • Jae-Sung Choi (Department of Oceanography, Chonnam National University) ;
  • Sung-Gwan Myoung (Tropical and Subtropical Research Center, Korea Institute of Ocean Science & Technology) ;
  • Joon-Young Yang (Ocean Climate and Ecology Research Division, National Institute of Fisheries Science) ;
  • Chang-Hoon Han (Ocean Climate and Ecology Research Division, National Institute of Fisheries Science)
  • 정영주 (전남대학교 지구환경과학부 해양환경전공) ;
  • 최병주 (전남대학교 지구환경과학부 해양환경전공) ;
  • 최재성 (전남대학교 지구환경과학부 해양환경전공) ;
  • 명성관 (한국해양과학기술원 제주연구소 열대.아열대연구센터) ;
  • 양준용 (국립수산과학원 기후환경연구과) ;
  • 한창훈 (국립수산과학원 기후환경연구과)
  • Received : 2023.12.27
  • Accepted : 2024.02.22
  • Published : 2024.03.30

Abstract

A real-time numerical prediction system was developed to predict sea surface temperature (SST) in Cheonsu Bay to minimize damages caused by marine heatwaves. This system assimilated observation data using an ensemble Kalman filter and produced 7-day forecasts. Bias in the temperature forecasts were corrected based on observed data, and the bias-corrected predictions were evaluated against observations. Using this real-time numerical prediction system, daily SSTs were predicted in real-time for 7 days from July to August 2021. The forecasted SSTs from the numerical model were adjusted using observational data for bias correction. To assess the accuracy of the numerical prediction system, real-time hourly surface temperature observations as well as temperature and salinity profiles observed along two meridional sections within Cheonsu Bay were compared with the numerical model results. The root mean square error (RMSE) of the forecasted temperatures was 0.58℃, reducing to 0.36℃ after bias-correction. This emphasizes the crucial role of bias correction using observational data. Sensitivity experiments revealed the importance of accurate input of freshwater influx information such as discharge time, discharge volume, freshwater temperature in predicting real-time temperatures in coastal ocean heavily influenced by freshwater discharge. This study demonstrated that assimilating observational data into coastal ocean numerical models and correcting biases in forecasted SSTs can improve the accuracy of temperature prediction. The prediction methods used in this study can be applied to temperature predictions in other coastal areas.

Keywords

Acknowledgement

이 연구는 국립수산과학원 한반도 주변해역 해양변동 특성연구사업의 연구비(R2024013)와 과학기술정보통신부의 재원으로 한국연구재단의 지원(No. 2020R1A2C1014678)을 받아 수행되었습니다.

References

  1. Gang DW, Cho HO, Son SW, Lee JH, Hyun YK, Boo KO (2021) Evaluation of sea surface temperature prediction skill around the Korean Peninsula in GloSea5 hindcast: improvement with bias correction. Atmos 31(2):215-227 
  2. NIFS (2020) Research on high water temperature damage response of aquafarm in Cheonsu Bay. Aquaculture Industry Division, West Sea Fisheries Research Institute, TR-2021-AQ-001, 78
  3. Kwon KM, Choi BJ, Lee SH, Cho YK, Jang CJ (2011) Coastal current along the eastern boundary of the Yellow Sea in summer: numerical simulations. The Sea 16(4):155-168 
  4. Kim YH, Choi BJ, Lee JS, Byun DS, Kang KR, Kim YG, Cho YK (2013) Korean ocean forecasting system: present and future. The Sea 18:89-103 
  5. Byun DS, Seo GH, Park SY, Jeong KY, Lee JY, Choi WJ, Shin JA, Choi BJ (2017) A technical guide to operational regional ocean forecasting systems in the Korea hydrographic and oceanographic agency (I): continuous operation strategy, downloading external data, and error notification. The Sea 22:130-117 
  6. Son DW, Yoo JS, Shin HH (2018) A study of applicability of ERA5 dataset for nearshore wave simulation. J Coast Disaster Prev 5:81-92 
  7. Yoo SH, Mun JY, Park W, Seo GH, Gwon SJ, Heo R (2019) Development of bathymetric data for ocean numerical model using sea-floor topography data: BADA Ver.1. J Korean Soc Coast Ocean Eng 31:146-157 
  8. Jung MI, Son SW, Choi J, Kang HS (2015) Assessment of 6-Month lead prediction skill of the GloSea5 hindcast experiment. Atmos 25(2):323-337 
  9. Jung SH, Le XH, Kim YS, Choi HG, Lee GH (2021) Application of deep learning method for decision making support of dam release operation. J Korea Water Resour Assoc 54(12):1095-1105 
  10. Choo HS (2021) Spatiotemporal fluctuation of water temperature in Cheonsu Bay, Yellow Sea. Fish Aquat Sci 54:90-100 
  11. KMI (2017) A study on disaster risk management of the aquaculture industry. Korea Maritime Institute, KMI Report 2017-09, 152 p
  12. Haidvogel DB, Arango HG, Hedstrom K, Beckmann A, Malanotte-Rizzoli P, Shchepetkin AF (2000) Model evaluation experiments in the North Atlantic Basin: simulations in nonlinear terrain-following coordinates. Dynam Atmos Oceans 32:239-281 
  13. Jung YJ, Choi BJ, Kwon KM, Lee SH (2022) Modeling surface low-salinity pools formed by heavy precipitation in the Yellow Sea. Estuar Coast Shelf S 275(2):107987 
  14. Kleist DT, Ide K (2015) An OSSE-based evaluation of hybrid variational-ensemble data assimilation for the NCEP GFS. Part II: 4DEnVar and hybrid variants. Mon Weather Rev 143(2):452-470 
  15. Kourafalou VH, De Mey P, Le Henaff M, Charria G, Edwards CA, He R, Herzfeld M, Pascual A, Stanev EV, Tintore J (2015) Coastal ocean forecasting: system integration and evaluation. J Oper Oceanogr 8(sup1):127-146 
  16. Kwon KM Choi BJ, Kim SD, Lee SH, Park KA (2020) Assessment and improvement of global gridded sea surface temperature datasets in the Yellow Sea using in situ ocean buoy and research vessel observations. Remote Sens 12(5):759 
  17. Kwon KM, Choi BJ, Lee SH, Kim YH, Seo GH, Cho YK (2016) Effect of model error representation in the Yellow and East China Sea modeling system based on the ensemble Kalman filter. Ocean Dyn 66:263-283 
  18. Park TW, Jang CJ, Jungclaus JH, Haak H, Park WS, Oh IS (2011) Effects of the Changjiang river discharge on sea surface warming in the Yellow and East China Seas in summer. Cont Shelf Res 31(1):15-22 
  19. Saha S, Moorthi S, Pan H-L, Wu X, Wang J, Nadiga S, Tripp P, Kistler R, Woollen J, Behringer D (2010) The NCEP climate forecast system reanalysis. Bull Am Met Soc 91: 1015-1057 
  20. Schiller A, Brassington GB, Oke P, Cahill M, Divakaran P, Entel M, Freeman J, Griffin D, Herzfeld M, Hoeke R (2019) Bluelink ocean forecasting Australia: 15 years of operational ocean service delivery with societal, economic and environmental benefits. J Oper Oceanogr 13(1):1-18 
  21. Shchepetkin AF, Mcwilliams JC (2005) The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model. Ocean Model 9(4):347-404 
  22. WMO (2020) Rtofs-da: Real time ocean-sea ice coupled three dimensional variational global data assimilative ocean forecast system. World Meteorological Organization, Geneva, Research Activities in Earth System Modelling Report 6:1-2