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Tropical Storm Barry was a strong tropical storm that made landfall on the Florida Panhandle during August 2001. The third tropical cyclone and second named storm of the 2001 Atlantic hurricane season, Barry developed from a tropical wave that moved off the coast of Africa on July 24. The wave entered the Caribbean on July 29 and spawned a low-pressure area, which organized into Tropical Storm Barry on August 3. After fluctuations in intensity and track, the storm attained peak winds of over the Gulf of Mexico. Barry headed northward and moved ashore along the Gulf Coast before dissipating on August 7. Unlike the devastating Tropical Storm Allison earlier in the season, Barry's effects were moderate. Nine deaths occurred: six in Cuba and three in Florida. As a tropical cyclone, Barry produced heavy rainfall that peaked at at Tallahassee. Gusts in the area reached , which was the highest wind speed recording for the storm. The precursor tropical wave to Barry dropped large amounts of rain on southern Florida, leading to significant flooding and structural damage. Moderate flooding and wind damage occurred throughout the Florida Panhandle. As the storm's remnants tracked inland, parts of the Mississippi Valley received light precipitation. Barry caused an estimated $30 million (2001 USD) in damage. == Meteorological history == On July 24, 2001, a tropical wave emerged off the west coast of Africa, and tracked westward across the Atlantic Ocean. Little cyclonic development occurred until July 28, when convection began to increase along the wave. The wave moved into the eastern Caribbean on July 29, and its convection continued to increase while it tracked west-northwest over the subsequent few days. The disturbance emerged into the Gulf of Mexico on August 1, with rainfall noted over southern Florida and the western tip of Cuba. That same day, a broad low-pressure system developed along the wave near the Dry Tortugas at the end of the Florida Keys, which began to intensify as it moved northwestward. At around 1800 UTC on August 2, an Air Force Reserve Hurricane Hunter aircraft investigating the system discovered that the low had organized into a tropical storm, which received the name ''Barry''. Post-hurricane season reanalysis, however, revealed that the low had become a tropical depression six hours earlier. There is uncertainty as to whether Barry actually held tropical characteristics at the time of designation, because of an upper-level low that was situated over the cyclone's surface center. When Barry became a tropical cyclone, its convection wrapped around roughly half of the center. Outflow in the eastern semicircle was good, although due to upper-level wind shear, it was restricted to southeast of the circulation. The cyclone became embedded within a mid- to-upper-level trough between the ridge over the central U.S. and the ridge over the northwestern Caribbean. A strong, upper-level cyclonic shear axis extended from just south of Cape Hatteras to near Brownsville, Texas, which prevented Barry from accelerating in forward speed. The ridge over the United States weakened, thus collapsing the steering pattern; this resulted in a west-southwestward drifting motion of the tropical storm by around August 3.〔 Early on August 3, strong westerly winds prevailed, and separated the center of circulation from what limited convection remained. The storm quickly regained some convection, although maximum sustained winds remained weak, at about 40 mph (60 km/h). Despite a slight drop in barometric pressure, post-season analysis revealed Barry weakened into a tropical depression early on August 4 due to the persistent wind shear and falling external pressure.〔 At 1800 UTC on August 4, the cyclone re-intensified slightly, and was upgraded to a tropical storm〔 as the shear decreased. Early on August 5, a strengthening period began as deep convection ignited over and near the low-level center. Prior to landfall, banding features developed on the eastern half of the circulation, despite some residual westerly shear. Within seven hours, the barometric pressure dropped from 1004 mb to 990 mb and overall satellite presentation had begun to improve. Barry reached its peak intensity at 1800 UTC on August 5 with winds of , just shy of hurricane status.〔 An eye formed at around the same time. At 0500 UTC on August 6, Barry increased in forward speed and made landfall at Santa Rosa Beach, Florida with winds of . Moving inland, the system weakened rapidly to a tropical depression; the National Hurricane Center issued its last advisory on the storm early on August 6. By the evening hours, maximum sustained winds near the center were around to as the system slowed significantly and drifted northwest at about . The depression turned northwestward, and steadily weakened to a remnant low near Memphis, Tennessee on August 7, and the low dissipated on August 8 over southeastern Missouri.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Tropical Storm Barry (2001)」の詳細全文を読む スポンサード リンク
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