H and O isotopic differences in typhon and urban-induced heavy rain in Tokyo

Stable isotope ratios of hydrogen and oxygen of water are useful tracers of the hydrological cycle. For example, isotopes monitor the evapotranspiration in vegetated areas, local snow ice processes and stream water flow processes. δ 18 O and δD in rainwater reflect the processes of evaporation, condensation and precipitation. Heavy rains thus modify the stable isotope ratio of ground water, stream water and transpiration water vapor. However, the controlling factors of δ 18 O and δD are not clear. Here we analyzed the inorganic ion concentration and stable isotope ratio in 38 normal rainwater and 15 heavy rainwater samples were collected in Shinjuku, Tokyo, Japan, during four years from October 2012 to December 2015. Results show a decrease in δ 18 O and δD values with the total rainfall amount, thus highlighting the amount effect. δ 18 O and δD volume-weighted mean values in typhoon heavy rain were higher than the values estimated from amount effect, whereas δ 18 O and δD volume-weighted mean values in urban-induced heavy rain were lower. Typhoon heavy rain has high Na + ratio and stable isotope ratios, while urban-induced heavy rain has low Na + ratio and stable isotope ratio.