DOI QR코드

DOI QR Code

스펙트럼 분석을 통한 2016년 하계 한국연안의 수온변동 특성에 관한 연구

A Study on the Characteristics of Summer Water Temperature Fluctuations by Spectral Analysis in Coast of Korea in 2016

  • Seo, Ho-San (Research Center for Ocean Industrial Development, Pukyong National University) ;
  • Jeong, Yong-Hyun (Department of Ecological Engineering, Pukyong National University) ;
  • Kim, Dong-Sun (Department of Ecological Engineering, Pukyong National University)
  • 투고 : 2020.01.31
  • 심사 : 2020.04.27
  • 발행 : 2020.04.30

초록

본 연구에서는 한국의 동해, 서해 및 남해안에서 하계 수온의 단기적인 변화에 영향을 주는 환경 요인을 파악하기 위해 국립해양조사원에서 제공하는 2016년 하계 조위관측소의 수온, 기온, 조위 및 바람자료를 이용하여 스펙트럼 분석을 실시하였다. Power spectrum 분석 결과, 평균조차가 100 cm 이상인 서해안(인천, 평택, 군산 및 목포)과 남해안(완도, 고흥, 여수, 통영 및 마산)에서는 수온, 조위가 동일한 주기에서 peak가 나타났다. 반면에 서해안과 남해안에 비해 평균조차가 상대적으로 작은 동해안(묵호, 포항 및 울산)과 부산에서는 수온의 주기성이 나타나지 않았다. Coherence 분석에서 서해안과 남해안의 3개 정점(완도, 고흥, 통영)은 수온과 조위의 상관성이 높게 나타났다. 특히 완도와 통영에서 수온과 조위의 상관성은 반일주기에서 0.96으로 높았다. 여수는 조석과 담수의 유입이 수온에 영향을 주는 것으로 보인다. 한편 마산의 수온은 남풍의 바람 영향이 가장 크지만 조석과 담수의 영향도 받는 것으로 판단된다. 그리고 동해안은 조차가 작고 해류의 영향이 크기 때문에 수온에 대한 조석의 영향이 작은 것으로 사료된다. 환경 요인의 시계열그래프를 비교한 결과, 수온과 조위가 상관성이 높게 나타난 정점은 창조 시 비교적 저수온의 외해수가 유입되고 낙조 시 빠져나가는 것으로 판단된다. 일주기의 수온 변화는 조석의 영향이 크지만 전체적인 수온의 상승과 하강은 기온의 영향이 큰 것으로 보인다.

In this study, spectral analysis was conducted to identify environmental factors af ecting short-term changes in water temperature in the East, West and South coasts of Korea. The data used in the spectrum analysis is the 2016 summer water temperature, air temperature, tide level and wind data provided by Korea Hydrographic & Oceanographic Agency. In power spectrum results, peaks of water temperature and tide level were observed at same periods in West Sea (Incheon, Pyeungteak, Gunsan and Mokpo) and South Sea (Wando, Goheung, Yeosu, Tongyeong and Masan) where mean tidal range was more than 100 cm. On the other hand, periodicity of water temperature did not appear in East Sea and Busan where the mean tidal range was small. Coherence analysis showed that water temperature was highly correlated with tide in West Sea and three stations(Wando, Goheung and Tongyeong) of South Sea. Especially, correlation between water temperature and tide level in Wando and Tongyeong presented 0.96 at semi-diurnal period. Water temperature in Yeosu seems to have influenced by tide and inflow of fresh water. In Masan, water temperature is influenced by south wind, tide and inflow of fresh water. In East Sea, influence of tide on water temperature is small due to current and small tidal range. As a result of comparing the time series graph, stations where the correlation between water temperature and tide is high show that relatively cold water was inputted at flood tide and flow out at ebb tide. short-term variation of water temperature was affected by tide, but long-term variation over a month was affected by air temperature.

키워드

참고문헌

  1. Bayne, B. L., D. A. Brown, K. Burns, D. R. Dixon, A. Ivanovici, D. R. Livingstone, D. M. Lowe, M. N. Moore, A. R. D. Stebbing, and J. Widdows(1985), The effects of stress and pollution on marine animals (Praeger special studies), Praeger Scientific, Westport, C.T. p. 9.
  2. Cho, K. D., C. H. Hong, K. H. Lee, J. H. Yoon, S. K. Yang, Y. K. Choi, D. S. Kim, K. W. Cho, H. D. Kim, and S. W. Kim(2005), Descriptive Physical Oceanography, Pukyong National University Press, pp. 119-121.
  3. Choi, H. S., J. I. Myoung, M. A. Park, and M. Y. Choi(2009), A Study on the summer mortality of Korean rockfish Sebastes schlegeli in Korea, J. Fish Pathol., 22(2), pp. 155-162.
  4. Choi, Y. H., Y. J. Ro, and H. K. Jun(2002), Variability of Seawater Temperature in the Coastal Water off the Dangjin Power Plant, Asan Bay, Korea, J. Korean Soc. Oceanography, 7(2), pp. 43-50.
  5. Choo, H. S., G. H. Lee, and Y. H. Yoon(1997), Variations of Temperature and Salinity in Kugum Suro Channel, J. Korean Fish. Soc., 30(2), pp, 252-263.
  6. Emery, W. J. and R. E. Thomson(1998), Data Analysis Methods in Physical Oceanography, Pergamon Press, pp. 468-487.
  7. Hue, H. K., D. H. Kim, S. H. Ahn, and G. W. Park(2000), Characteristics of the Sedimentary Environment in Yoja Bay in the Summer of 1998, Korean J. Environ. Biol. 18(2), pp 227-235.
  8. Ichiye, T.(1984), Ocean hydrodynamics of the Japan and East China Seas, Elsevier Oceanography Series, Amsterdam, Netherlands, 39, p. 423.
  9. Kim, C. H. and K. Kim(1983), Characteristics and origin of the cold water mass along the east coast of Korea, J. Oceanol. Soc. Korea, 18, pp. 73-83.
  10. Kim, C. W., E. O Kim, H. D. Jeong, C. G. Jung, M. W. Park, and S. G. Son(2009), Variation of Body Composition and Survival Rate According to Spawning of Pacific Oyster, (Crassostrea gigas) in Gamak Bay, Kor. J. Fish Aquat. Sci., 42(5), pp. 481-486. https://doi.org/10.5657/kfas.2009.42.5.481
  11. Kim, S. J., S. H. Woo, B. M. Kim, and S. D. Hur(2011), Trends in Sea Surface Temperature (SST) Change Near the Korean Peninsula for the Past 130 Years, Ocean and Polar Research, Vol. 33(3), pp. 281-290. https://doi.org/10.4217/OPR.2011.33.3.281
  12. Lee, C. I., J. H. Lee, and D. S. Kim(2007), Effects of Meteorological Factors on Water Temperature, Salinity in the West Sea of Korea, Journal of the Korean Society of Marine Environment & Safety, 13(1), pp. 29-37.
  13. Lee, J. C., H. S. Choo, K. H. Lee, and K. D. Cho(1995), Tides and Currents of Kamag Bay in July-August 1994, J. Korean Fish. Soc. 28(5), pp. 624-634.
  14. Lee, Y. S.(2002), An Influence of Inflowing Freshwater on the Diatom Blooms in the Eastern Coast of Dolsan, Yosu, Korea. J. of KSSE Vol. 24. No. 3. pp. 477-488.
  15. Miita, T. and Y. Ogawa(1984), Tsushima currents measured with current meters and drifters, Elsevier Oceanography Series, Vol. 39, pp. 67-76. https://doi.org/10.1016/S0422-9894(08)70291-5
  16. Min, H. S. and C. H. Kim(2006), Interannual Variability and Long-term Trend of Coastal Sea Surface Temperature in Korea, Ocean and Polar Research, Vol. 28(4), pp. 415-423. https://doi.org/10.4217/OPR.2006.28.4.415
  17. MLTMA(2009), Ministry of Land, Transport and Maritime Affairs, A Study of Total Amount Management of Coastal Pollution in Masan Bay, pp. 1-977.
  18. Na, G. H., C. S. Lee, and W. J. Choi(1991), The Effect of Dissolved Oxygen on the Estival Mass Mortality of sea quirt, Halocynthia roretzi(Drasche), Bull. Korean Fish, Soc. 42(1), pp. 52-58.
  19. Oh, S. Y., S. W. Jang, and H. J. Yoon(2011), Variations of catch of Anchovy and Saury due to oceanic climate change in the Korean seas, J. of Korea Institute of Information and Communication Engineering, 15(3), pp. 740-746. https://doi.org/10.6109/jkiice.2011.15.3.740
  20. Oh, S. Y., S. W. Jang, D. H. Kim, and H. J. Yoon(2012), Temporal and Spatial Variations of SL/SST in the Korean Peninsula by Remote Sensing, Jour. Fish. Mar. Sci. Edu., 24(2), pp. 333-345. https://doi.org/10.13000/JFMSE.2012.24.2.333
  21. Seong, K. T., J. D. Hwang, I. S. Han, W. J. Go, Y. S. Suh, and J. Y. Lee(2010), Characteristic for Long-term Trends of Temperature in the Korean Waters, J. Korean Society of Marine Environment & Safety, 16(4), pp. 353-360.
  22. Suh, Y. S., L. H. Jang, and J. D. Hwang(2003), Anomalous Variation of the Oceanic Features around Korean Waters Related to the Global Change, J. of the Environmental Sciences, 12(3), pp. 257-263. https://doi.org/10.3321/j.issn:0253-2468.2000.03.001
  23. Vinay, K. I. and G. P. John(1999), Digital signal processing using MATLAB, Thomson-Engineering, pp. 139-190.
  24. Zhang, C. I., J. B. Lee, S. Kim, and J. H. Oh(2000), Climatic regime shifts and their impacts on marine ecosystem and fisheries resources in Korean waters, Progress in Oceanography, 47, pp. 171-190. https://doi.org/10.1016/S0079-6611(00)00035-5

피인용 문헌

  1. Spatial-temporal distributions of the newly described mixotrophic dinoflagellate Gymnodinium smaydae in Korean coastal waters vol.35, pp.3, 2020, https://doi.org/10.4490/algae.2020.35.8.25