Typhoon Kezia
Typhoon Kezia was an intense tropical cyclone which struck the southern part of Japan in September 1950. The eighth named storm of the 1950 Pacific typhoon season, Kezia formed north of Guam on September 4. The system's wind speed increased steadily as it moved northwest. The peak wind speed according to the China Meteorological Administration gave a peak wind speed of. Kezia retained its peak intensity until it weakened rapidly near the coast of Japan. The storm made landfall in Kagoshima Prefecture in Kyushu on September 13 and made two more landfalls after in Hokkaido on September 14 and Kamchatka Krai on September 15 as an extratropical. It dissipated the next day. Numerous military vehicles were warned and grounded. Floods were recorded in Iwakuni and Hiroshima. The overall deaths nationally were 25.
Meteorological history
Kezia formed north of Guam on September 4 with a wind speed from the CMA of as a tropical depression. Shifting northwest, the depression steadily increased its wind speed and was a tropical storm on September 6. The next day, it was officially a typhoon as the Joint Typhoon Warning Center started monitoring the cyclone. The storm steadily grew as it started traversing more west. As September 10 started, the CMA gave a peak wind speed of. The storm had a sharp curve more western while still moving north.Over the following days, Kezia retained its peak intensity while traversing northwest. On September 12, the cyclone was in close proximity to the coast of extreme south Japan, weakening rapidly. The storm made landfall in Kagoshima Prefecture in Kyushu on September 13 at 06:00 UTC as it continued straight north. Researcher Atsushi Kimpara commented in the Journal of Geomagnetism & Geoelectricity that the storm changed its character after it passed the island, elaborating that origins of atmospherics moved to the coast of Shikoku. He also noticed the weakening of the cyclone. It continued weakening and eventually made a second landfall on the island of Hokkaido at 21:00 UTC, September 14. It continued weakening until the CMA stopped tracking it the next day; it had conflicting classifications from different agencies. In the middle of September 15, the JTWC concluded its tracking of the cyclone when it became extratropical. It made landfall in Kamchatka Krai at 18:00 UTC that same day before dissipating on September 16 at 06:00 UTC.