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2023 Vol.56, Issue 11 Preview Page

Research Article

Future hydrological changes in Jeju Island based on CMIP6 climate change scenarios

CMIP6 기후변화 시나리오에 따른 제주도 지역의 미래 수문변화 전망

Chul-Gyum Kima*
,
Jaepil Chob
,
Jeong Eun Leec
,
Sunwoo Changd
김 철겸a*
,
조 재필b
,
이 정은c
,
장 선우d
aResearch Fellow, Department of Hydro Science and Engineering Research, Korea Institute of Civil Engineering and Building Technology, Goyang, Korea
bDirector, Integrated Watershed Management Institute, Seoul, Korea
cSenior Researcher, Department of Hydro Science and Engineering Research, Korea Institute of Civil Engineering and Building Technology, Goyang, Korea
dResearch Fellow, Department of Hydro Science and Engineering Research, Korea Institute of Civil Engineering and Building Technology, Goyang, Korea
a한국건설기술연구원 수자원하천연구본부 연구위원
b유역통합관리연구원 유역관리융합연구소 소장
c한국건설기술연구원 수자원하천연구본부 수석연구원
d한국건설기술연구원 수자원하천연구본부 연구위원
*Corresponding Author
30 November 2023. pp. 737-749
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Abstract

In this study, we analyzed the hydrological impacts of future climate change on Jeju Island using SSP-based climate change scenarios from 18 climate models and watershed modeling (SWAT-K). Despite discrepancies among climate models, we generally observed an increase in evapotranspiration due to rising future temperatures. Furthermore, a significant increase in runoff and recharge was noted due to increased precipitation. These increasing trends were particularly pronounced in the SSP5-8.5 scenario, and differences among GCM models became more significant in the late 21 century. When compared to the historical period (1981-2010), the projected changes for the far-future period (2071-2100) in the SSP5-8.5 scenario showed a 21.4% increase in precipitation, a 19.2% increase in evapotranspiration, a 40.9% increase in runoff, and a 16.6% increase in recharge on an annual average basis. On a monthly basis in the SSP5-8.5 scenario, precipitation was expected to increase by 24.5% in September, evapotranspiration by 34.1% in April, runoff by 58.1% in October, and recharge by 33.8% in September. To further assess projections based on extreme climate scenarios, we selected two models, CanESM5 and ACCESS-ESM1-5, which represented the maximum and minimum future precipitation forecasts, and compared the hydrological changes in the future scenarios. The results indicated that runoff and recharge rates were relatively higher in the CanESM5 model with the highest precipitation forecast, while evapotranspiration rates were higher in the ACCESS-ESM1-5 model with the lowest precipitation forecast. Based on the climate change scenarios used in this study, the overall available water resources on Jeju Island are more likely to increase. However, since results vary by season and region depending on the climate model and scenario, it is considered necessary to conduct a comprehensive analysis and develop response measures using various scenarios.

Keywords
Climate change
SSP scenario
GCM
Jeju Island
SWAT-K

본 연구에서는 18개 기후모형으로부터 도출된 SSP 기반의 미래 기후변화 시나리오와 유역모델링(SWAT-K)을 연계하여 제주도 지역의 미래 기후변화에 따른 수문학적 영향을 분석하였다. 기후모형에 따른 편차가 있으나 대체로 미래 기온의 증가에 따라 증발산량이 증가하고, 강수량의 증가로 인해 유출량과 함양량 또한 크게 증가할 것으로 전망되었다. 특히 SSP5-8.5 시나리오에서 이러한 증가가 더욱 뚜렷하게 나타났으며, 미래 후반기로 갈수록 GCM 모형 간의 차이가 크게 나타났다. 연평균 값에 대한 과거기간(1981~2010년) 대비 증감률로는 미래 후반기(2071~2100년)에 SSP5-8.5 시나리오에서 강수량 +21.4%, 증발산량 +19.2%, 유출량 +40.9%, 함양량 +16.6%의 전망을 나타내었다. 월별로 변화율을 보면 SSP5-8.5 시나리오에서 강수량은 9월에 24.5%, 증발산량은 4월에 34.1%, 유출량은 10월에 58.1%, 함양량은 9월에 33.8%까지 증가할 것으로 전망되었다. 또한 극한 기후 시나리오에 따른 전망을 위해, 미래에 최다 강수량을 예측한 CanESM5 모형과 최소 강수량을 예측한 ACCESS-ESM1-5 모형의 미래 기후자료를 사용하여 연평균 수문학적 변화를 비교하였다. 그 결과 강수량이 최대로 나타난 CanESM5 모형에서는 유출률과 함양률이 상대적으로 높게 나타난 반면, 강수량이 최저로 전망된 ACCESS-ESM1-5의 경우에는 증발산 비율이 높게 나타났다. 본 연구에서 적용한 기후변화 시나리오 기준으로 제주도 전체의 가용수자원은 증가한다고 전망할 수 있으나, 기후모형에 따라 계절별 지역별로 상이한 결과를 도출할 수 있기 때문에 가능한 다양한 시나리오를 활용한 종합적 분석과 대응방안이 필요하다고 생각된다.

키워드
기후변화
SSP 시나리오
GCM
제주도
SWAT-K
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Information
  • Publisher :KOREA WATER RESOURECES ASSOCIATION
  • Publisher(Ko) :한국수자원학회
  • Journal Title :Journal of Korea Water Resources Association
  • Journal Title(Ko) :한국수자원학회 논문집
  • Volume : 56
  • No :11
  • Pages :737-749
  • Received Date : 2023-09-18
  • Revised Date : 2023-10-12
  • Accepted Date : 2023-10-23
  • DOI :https://doi.org/10.3741/JKWRA.2023.56.11.737
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