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1887 Halloween tropical storm : ウィキペディア英語版 | 1887 Halloween tropical storm
The 1887 Halloween tropical storm was a late-season tropical cyclone that caused significant damage along the East Coast of the United States during Halloween of 1887. The sixteenth tropical storm of the annual hurricane season, it formed from an area of disturbed weather over the Gulf of Mexico on October 29. The storm later came ashore along the west coast of Florida. After crossing the state, it produced severe thunderstorms along the North Carolina–Virginia coastline before becoming extratropical on November 1. The extratropical system intensified into the equivalent of a Category 1 hurricane on the modern-day Saffir–Simpson Hurricane Scale. It eventually dissipated on November 6, shortly after hitting northwest France. The storm affected the town of Norfolk, where it became the most damaging storm since 1879. Despite the damage inland, the storm is best known for the unusually high amount of shipwrecks and maritime incidents it caused. One ship, a schooner called the ''Manantico'', capsized, killing the captain and one of its crew members. Three other ships were driven ashore on Virginia beaches from Dam Rock to Cape Henry, and numerous others were put in danger. ==Meteorological history== The storm originated from an area of disturbed weather that had persisted in the Gulf of Mexico during late October 1887, outside the area of coastal stations. On October 29, the disturbance completed tropical cyclogenesis and became the sixteenth tropical storm of the season. After forming, the storm was located 200 miles (320 km) northwest of Key West and began moving east-northeastward, making landfall on the Florida Peninsula. It crossed land and emerged over water within the next eight hours while weakening. During its passage near Fort Meade, the storm had an estimated barometric pressure of , supporting minimal tropical storm strength. Upon crossing the state, it paralleled the East Coast for two days while restrengthening. It passed closest to land near the North Carolina coastline on October 31 at its peak intensity, with sustained winds of and a pressure of . Shortly after moving away from land, it became extratropical.〔〔 The extratropical cyclone moved away from the coast and strengthened to the equivalent of a Category 1 hurricane on the modern-day Saffir-Simpson Hurricane Scale on November 1. It began a weakening trend on November 2 while taking a wavering path across the north Atlantic Ocean.〔 On November 4, the cyclone started a general east-southeast motion, passing near the southwest coasts of Ireland and Great Britain. It made landfall on the Cotentin Peninsula of France on November 6 and dissipated, although one proposed track, which is a modified track that differs from the official record due to new evidence or theory, was given by Charles Mitchell that showed the cyclone executing a counter-clockwise loop over northwest France until dissipating the storm on November 8.〔
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