論文ID: 2024-026
The interannual variation in the number of heavy rainfall events in Japan in 1976-2022, extracted from 3-hour accumulated precipitation (P3H) data exceeding 130 mm, showed a relatively large relationship (correlation coefficient 0.45) with sea surface temperature (SST) around the Japanese Islands. In the Kyushu area during the rainy season (June-July), the correlation coefficient with SST became considerably smaller, while a relatively large relationship (correlation coefficient 0.45) was found with the appearance frequency of 500m-height water vapor flux above 250 g m−2 s−1, suggesting that the interannual variation could be considerably influenced by the synoptic scale pressure pattern. Diurnal variations in the number of heavy rainfall events, including long-term increasing trends, were also investigated. Although less significant diurnal variations were observed on the annual basis, the events in the Kyushu area were more frequent in the morning (7-9 JST: JST = UTC + 9 hours) during the rainy season. In the Kyushu area, the 47-year long-term trend of heavy rainfall events in 4-9 JST was a 7.47-fold increase in June and July, while it was only a 1.35-fold increase in the other months.