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Hurricane Waldo (1985) : ウィキペディア英語版
Hurricane Waldo (1985)

Hurricane Waldo was a Pacific hurricane that caused significant flooding in Kansas during October 1985. After developing into a tropical depression on October 7, it steadily intensified, becoming a tropical storm within a day. Waldo reached hurricane intensity on October 8. After peaking as a moderate Category 2 hurricane on the Saffir-Simpson Hurricane Scale, it re-curved to the east, making landfall at peak intensity near Culiacan. Afterword, it rapidly dissipated. In all, Waldo caused moderate damage in Sonora. The remnants of the storm combined with a cold front over the Great Plains. Significant flooding and one death was recorded in Kansas. Many rivers and creeks overflowed its banks.
==Meteorological history==

Waldo originated from a developing disturbance first noted by Eastern Pacific Hurricane Center (EPHC) on October 5 based on data from ship reports. By 0000 UTC October 7, a circulation became evident on satellite imagery. Based on this, the EPHC upgraded the system into a tropical depression about west of the Mexican coast. Upon becoming a tropical cyclone, the depression began to turn to the northwest in response to a strong upper-level trough over Baja California Peninsula. Passing over 86 °F (30 °C) sea surface temperatures, the tropical cyclone intensified into Tropical Storm Waldo about 12 hours after developing. The storm began to intensify rapidly. Meanwhile, the tropical storm passed east of Socorro Island. Tropical Storm Waldo then began to turn to the north and while located south of Baja California Sur, Waldo was upgraded into a Category 1 hurricane on the Saffir-Simpson Hurricane Scale.〔
After reaching hurricane status the strengthening cyclone attained Category 2 hurricane status on October 9. Shortly thereafter, a ship reported a sea level pressure of just outside of the center of circulation. Meanwhile, Hurricane Waldo reached its peak intensity of 105 mph (165 km/h).〔 Four hours after Hurricane Waldo's peak, the storm made landfall near Culiacan. The storm rapidly dissipated during the afternoon of October 9, while the system was located inland over Mexico.〔 The remnants of Waldo merged with a cold front and produced heavy rains across the Great Plains and Mississippi River Valley.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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