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The environmental stability for afternoon rain events over the Kanto Plain in summer was investigated. The AMeDAS data were used to extract the hot, sunny days under synoptically undisturbed conditions, and the gridded mesoscale analysis data that cover the southern Kanto Plain were used to examine the difference of the characteristics of environmental stability among no-rain, rain, and strong-rain events in the afternoon by calculating commonly used stability indices and parameters. A statistical analysis by t-test statistic was conducted to determine the significance of the different features of the stability parameters among the events. Among the parameters, K-index indicated the highest significance level. The analyses on the difference of temperature and humidity at each height among the events indicated that the temperatures and moistures at low to middle levels clearly distinguish the stability conditions for the afternoon rain events. It is strongly suggested that colder temperature at middle levels and higher humidity at low to middle levels are favorable conditions for the development of stronger rains in the afternoon.

Environmental Stability for Afternoon Rain Events in the Kanto Plain in Summer