伊勢湾台風擬似温暖化実験による淀川流域における洪水規模の変化予測

抄録

This paper deals with a methodology to estimate the variations of flood hazard and risk due to a climate change. A pseudo global warming (pgw) experiment result of the Isewan Typhoon in 1959 is used as the rainfall input with a climate change effect to a distributed rainfall-runoff/flood inundation (DRR/FI) model. The simulated rainfalls of the control run (ctl) for the reproduction of the Isewan Typhoon as well as pgw experiment by JMA-NHM exhibit that, though the 48-hrs rainfall of ctl underestimates the observation, the maximum hourly rainfall of pgw becomes much higher than the observation. As the result, the simulated water level/discharge and inundation depth with pgw rainfall becomes all worse than those of the Isewan Typhoon.