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1934 Muroto typhoon

Pacific typhoon hitting Japan

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Through Atmospheric pressure

Regarded at the time as the "second-greatest catastrophe of modern Japan" after the 1923 Great Kantō earthquake, the storm left parts of Osaka in ruins. Tens of thousands of structures were damaged or destroyed, leaving approximately 200,000 people homeless. Among the 3,066 people killed were 421 children and teachers who perished when their flimsy schools were destroyed. That ranked it, at the time, as the deadliest typhoon in Japanese history. In addition to the fatalities, 13,184 people were injured. Total damage exceeded $300 million (1934 USD).

Meteorological history

On September 13, 1934, a tropical cyclone developed over the western Caroline Islands. The storm traveled generally northwest, executing a brief cyclonic loop on September 14–15. After a brief stint traveling nearly due north on September 17, the cyclone began recurving to the northeast. It brushed the Ryukyu Islands to the southeast on September 20 as it accelerated northeast. On the morning of September 21, the typhoon struck Shikoku and southern Honshu. According to the Central Meteorological Observatory (now called the Japan Meteorological Agency), maximum sustained winds reached 150 km/h (90 mph), with gusts exceeding 215 km/h (130 mph).

The typhoon first made landfall over Muroto, Kōchi Prefecture, resulting in it later being dubbed the "Muroto typhoon". A then-world record low barometric pressure for a land station of 911.9 hPa (26.93 inHg) was observed in Muroto. Though surpassed less than a year later during the 1935 Labor Day hurricane in the Florida Keys, it remains the lowest value ever observed in mainland Japan and the third-lowest throughout the country. It briefly emerged over the Kii Channel before striking the Kaifu District in Tokushima Prefecture. The system then crossed the Kii Channel again and traversed Awaji Island. After another brief stint over water, the storm made its next landfall directly over Kobe, Hyōgo Prefecture, just 30 km (19 mi) west of Osaka City. A barometric pressure of 954.3 hPa (28.18 inHg) was observed in Osaka. Crossing mainland Japan, the storm briefly emerged over the Sea of Japan before traversing northern Honshu.

Pronounced frontal features, a characteristic of extratropical cyclones, developed late on September 21, with a cold front extending south toward the Philippines. The system continued on an easterly course and was last noted in the International Best Track Archive on September 22 moving away from Hokkaido. Surface weather analyses depict the system continuing east, crossing the International Date Line (180°) by September 23. During this time, its central pressure rose to roughly 985–990 mbar (hPa; 29.09–29.34 inHg). On September 24, the storm turned north toward the Aleutian Islands of the then Territory of Alaska and deepened. Winds up to Force 10—89 to 102 km/h (55 to 63 mph)—on the Beaufort scale affected parts of the Aleutians and a pressure of 964 mbar (hPa; 28.47 inHg) was observed near 48°00′N 160°30′W / 48°N 160.5°W. Traversing the Bering Sea, the system was last identifiable on September 25 over western Alaska.

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