본 연구는 GIS 기반의 SWAT (Soil and Water Assessment Tools) 모형을 이용하여 탁수발생 잠재가능성 평가지표를 개발하고 수계별 탁수 관리방안 대책을 지원하기 위해 기후변화에 따른 안동호와 임하호 유역의 유출량과 부유사량의 변화특성을 분석하였다. 장래 기후변화자료는 IPCC (Intergovernmental Panel on Climate Change)에서 제공하는 A1B 기후변화시나리오의 MIROC3.2 hires 모델의 결과값을 이용하여 생성하였다. 과거의 기후자료(1977~2006)를 기반으로 20C3M (20th Century Climate Coupled Model) 모의값을 이용하여 강수와 온도를 보정한 뒤 CF (Change Factor) 기법으로 downscaling 하였다. 미래 기후변화 시나리오는 세 기간(2020s, 2050s, 2080s)으로 나누어 분석하였고, SWAT 모형과 연계하여 기후변화에 따른 유출량 및 부유사량의 변화를 산출하였다. 2020s, 2050s, 2080s 기간동안의 안동호와 임하호 유역의 유출량과 부유사량은 기준년도(2006)에 비해 증가하였고, 계절적인 분석에서도 봄, 가을, 겨울철 안동호와 임하호 유역의 유출량과 부유사량이 기준년도에 비해 증가하는 것으로 모의되었다. 단, 여름철 유량과 부유사량은 2020s에만 증가하고 2080s에는 감소하는 것으로 분석되었다.
This study analyzed the change of flowout and suspend solid in Andong and Imha basin according to the climate change to develop evaluation index about turbid water occurrence possibility and to support the countermeasures for turbid water management using GIS-based Soil and Water Assessment Tools (SWAT). MIROC3.2 hires model values of A1B climate change scenario that were supplied by Intergovernmental Panel on Climate Change (IPCC) were applied to future climage change data. Precipitation and temperature were corrected by applying the output value of 20th Century Climate Coupled Model (20C3M) based on past climate data during 1977 and 2006 and downscaled with Change Factor (CF) method. And future climate change scenarios were classified as three periods (2020s, 2050s, 2080s) and the change of flowout and suspended solid according to the climate change were estimated by coupling modeled value with SWAT model. Flowout and suspended solid of Andong and Imha basin in 2020s, 2050s, and 2080s were simulated as increasing compared with standard year (2006). Also, as the result of seasonal change, flowout and suspended solid of Andong and Imha basin in spring, autumn, and winter showed as increasing compared with standard year. And them of Andong and Imha basin in summer were analyzed as decreasing compared with standard year.
