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대표농도경로 (RCP)에 따른 21세기 말 우리나라 극한강수 전망

Projection of Extreme Precipitation at the end of 21st Century over South Korea based on Representative Concentration Pathways (RCP)

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주제분류대기과학

초록

Representative Concentration Pathways (RCP) are the latest emission scenarios recommended to use for the fifth assessment report of Intergovernmental Panel on Climate Change. This study investigates the projection of extreme precipitation in South Korea during the forthcoming 21st Century using the generalized extreme value (GEV) analysis based on two different RCP conditions i.e., RCP 4.5 and 8.5. Maximum daily precipitation required for GEV analysis for RCP 4.5 and 8.5 are obtained from a high-resolution regional climate model forced by the corresponding global climate projections, which are produced within the CMIP5framework. We found overall increase in frequency of extreme precipitation over South Korea in association with climate change. Particularly, daily extreme precipitation that has been occurred every 20 years in current climate (1980~2005) is likely to happen about every 4.3 and 3.4 years by the end of 21st Century (2070~2099) under the RCP 4.5 and 8.5 conditions,respectively.

Abstract

Representative Concentration Pathways (RCP) are the latest emission scenarios recommended to use for the fifth assessment report of Intergovernmental Panel on Climate Change. This study investigates the projection of extreme precipitation in South Korea during the forthcoming 21st Century using the generalized extreme value (GEV) analysis based on two different RCP conditions i.e., RCP 4.5 and 8.5. Maximum daily precipitation required for GEV analysis for RCP 4.5 and 8.5 are obtained from a high-resolution regional climate model forced by the corresponding global climate projections, which are produced within the CMIP5framework. We found overall increase in frequency of extreme precipitation over South Korea in association with climate change. Particularly, daily extreme precipitation that has been occurred every 20 years in current climate (1980~2005) is likely to happen about every 4.3 and 3.4 years by the end of 21st Century (2070~2099) under the RCP 4.5 and 8.5 conditions,respectively.

참고문헌 (27)

  1. IPCC 5차 평가보고서 대응을 위한기후변화 시나리오 보고서 2011, "국립기상연구소", 2~ (2011)
  2. 2011년도 수해복구 현안업무 보고, "서초구", 1~ (2011)
  3. 신진호, "역학적 상세화 기법을 활용한우리나라 극한 강수사상 전망: 일최대강수량 변화 분석", 한국수자원학회 학술발표회 초록집, pp.350~ (2010)
  4. 오태석, "군집분석과 변동핵밀도함수를 이용한 지역빈도해석의 확률강우량 산정", 대한토목학회 논문집B, 28(2B), pp.225~236 (2008), 대한토목학회
  5. 이경미, "한국에서 평균기온 및 극한기온의 변화시점 분석", 대한지리학회지, 46(5), pp.583~596 (2011), 대한지리학회
  6. 이창환, "비정상성 강우빈도해석법에 의한 확률강우량의 평가", 한국수자원학회 논문집, 43(2), pp.187~199 (2010), 한국수자원학회
  7. 정대일, "기후 변화를 고려한 홍수 위험도 평가", 대한토목학회 논문집B, 28(1B), pp.55~64 (2008), 대한토목학회
  8. 허준행, "우리나라 강우자료의 지역빈도해석 적용성 연구(Ⅰ) : 확률강우량 산정", 대한토목학회 논문집B, 27(2B), pp.101~111 (2007), 대한토목학회
  9. Beniston, M., "Future extreme events in European climate: An exploration of regional climate model projections", Climatic Change, 81, pp.71~95 (2007)
  10. Boo, K.-O, "Response of global warming on regional climate change over Korea: an experiment with the MM5 model", Geophys. Res. Lett., 31, pp.L21206~ (2004)[DOI]
  11. Boo, K.-O, "Change of extreme events of temperature and precipitation over Korea using regional projection of future climate change", Geophys. Res. Lett, 33, pp.L01701,~ (2006)[DOI]
  12. Chang, H., "Spatial variation of summer precipitation trends in South Korea, 1973- 2005", Environ. Res. Lett (2005)[DOI]
  13. Evaluation of HadGEM2 model, "Collins, W. J", 44~, pp.Hadley Centre Technical Note, 74 (2008)
  14. Ganguly, A. R, , Climate extremes hydrometeorological extremes and impacts, fall creek Falls 2007 Workshop (2007)
  15. Greenwood, J. A, "Probability weighted moments: definition and relation to parameters of several distributions expressible inverse form", Water Resources Research,, 15, pp.1049~1054 (1979)
  16. Hosking, J. R, "Estimation of the GEV distribution by the method of probabilityweighted moment", Technometrics, 27(3), pp.251~261 (1985)
  17. Hosking, J. R., "Regional frequency analysis: an approach based on L-moments" (1997), Cambridge University Press
  18. Im, E. -S., "Characteristics of extreme climate sequences over Korea using a regional climate change scenario", Sci. Online Lett. Atmos., 3, pp.17~20 (2007), Meteorological Society of Japan
  19. Koo, G.-S, "Projection of temperature over Korea using an MM5 regional climate simulation", Climate Research, 40, pp.241248~ (2009)
  20. Lu, L, "Variance of 2- and 3- paremeter GEV", PWM quantile estimators: formulas, confidence intervals and a comparison, 1992, pp.138, 247~268
  21. Martin, E. S, "Generalized maximum likelihood GEV quantile estimator for hydrologic data", Water Resources Research, 28(1), pp.3001~3010 (2000)
  22. May, W., "Potential future changes in the characteristics of daily precipitation in Europe simulated by the HIRHAM regional climate model", Climate Dyn, 30, pp.581603~ (2008)
  23. Moss, R, "Towards New Scenarios for Analysis of Emissions, Climate Change, Impacts, and Response Strategies", Intergovernmental Panel on Climate Change, pp.132~ (2008)
  24. Park, J.-S, "Changes in the extreme daily rainfall in South Korea", International Journal of Climatology (2010)[DOI]
  25. Stedinger, J. R, "Chapter 18, Frequency analysis of extremeevents, Handbook of Hydrology" (1993), McGraw-Hill
  26. Um, M.-J., "A comparative study of the adaptive choice of thresholds in extreme hydrologic events", Stochastic Environmental Research and Risk Assessment, 24(5), pp.611~623 (2010), Springer New York
  27. Walters, D. N, "The Met office unified model global atmosphere 3.0", 3.1 and JULES global land 3.0, Geosci. Model Dev. Discuss, pp.2011, 4[DOI]

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