Japan Geoscience Union Meeting 2019

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-HW Hydrology & Water Environment

[A-HW23] Hydrology & Water Environment

Tue. May 28, 2019 3:30 PM - 5:00 PM 103 (1F)

convener:Isao Machida(Geological Survey of Japan), Dai Yamazaki(Institute of Industrial Sciences, The University of Tokyo), Takeshi Hayashi(Faculty of Education and Human Studies, Akita University), Keisuke Fukushi(Institute of Nature & Environmental Technology, Kanazawa University), Chairperson:Megumi Watanabe

4:45 PM - 5:00 PM

[AHW23-11] Seasonality in the extreme precipitation events linked to temperature over Japan

*Sridhara Nayak1, Tetsuya Takemi1 (1.Disaster Prevention Research Institute, Kyoto University)

Keywords:Extreme Precipitation Events, d4PDF, Clausius-Clapeyron Equation

The frequency of extreme precipitation events is expected to increase in future warmer climate according to the Clausius-Clapeyron (CC) equation which states that atmosphere can hold more moisture in warmer air temperature (about 7 percent per increase of 1ºC). In this study, the extreme precipitation intensities linked to temperature are investigated for different seasons over seven sub-regions of Japan by analyzing the d4PDF dataset at 20 km in present (1951-2010) and future climate (2051-2110). To do this we stratified the precipitation intensities of wet days (defined as excess of 1 mm per day) in different temperature bins at 1º intervals and computed the 99-percentile of the precipitation intensities from each temperature bin. We find that the extreme precipitation intensities linked to temperature is strongly influenced by the seasons and regions of Japan. The extreme precipitation intensities increase with temperature up to 21º over northern Japan, while the extreme precipitation intensities over Okinawa increase up to 24º. Intensities of extreme precipitation events over northern parts of Japan including Hokkaido and Tohoku regions are increased by about 10 mm per day in future warming climate, while over western regions of Japan it is increased by about 20 mm per day. Seasonal analysis indicates a super CC relationship in winter season and a sub CC relationship in summer. Overall results suggest that Japanese regions may experience more extreme precipitations in future warming climate.