(Tenki is the bulletin journal of the Meteorological Society of Japan in Japanese.)
TENKI, Vol. 72, No. 4, pp. 167-181, 2025
The number of heatstroke patients in Kyoto city during the warm season (May-September) over the past 13 years (2011-2023) was estimated using the number of people transported to hospital by ambulance. Daily, seasonal and interannual variations of these numbers were analyzed in relation to changes in meteorological factors and the number of tourists visiting Kyoto. The number of people transported during the midsummer period under the Ogasawara anticyclone increases rapidly: more than 5 persons/day at mean daily temperatures above 28ßC, more than 10 persons/day above 30ßC and more than 20 persons/day above 31ßC. The seasonal trends in the number of people transported to hospital show, in most of the years, two peaks of number in mid-July and early August. The peak in July well corresponds with the Gion Festival (of 17 July), which is held several days after the end of the rainy season in most years, and the peak in August corresponds with the period of seasonal maximum temperature. A machine-learning analysis (by XGBoost method) quantitatively confirmed that the July-peak becomes remarkably large when a very large number of tourists visited the Gion Festival under conditions of insufficient heat acclimatization due to the rapid rise of temperature immediately after the end of the rainy (Baiu/Meiyu) season.
TENKI, Vol. 72, No. 7, pp. 325-335, 2025
An observational case study of a polar mesoscale cyclone (PMC) formed over the NW Pacific in 16-20 February 1975 is made. A synoptic-scale low, which formed nearby Formosa in 13 February, moved northeastward in the baroclinic zone over the Kuroshio Current. The low developed rapidly over the Northeastern Pacific in 15-16, under the influence of an upper cold vortex, and caused the southward shift of the cold vortex. The PMC formed in 16 February, within the circulation of the synoptic-scale (parent) low, and nearby the cold vortex. While the parent low developed rapidly over the warmer sea area, where heat energy supply from the sea surface is large, the PMC formed and developed over the cooler sea area, where heat energy supply is relatively small. The rapid development of the parent low is important for the PMC generation of the present case.