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1940 Nova Scotia hurricane : ウィキペディア英語版 | 1940 Nova Scotia hurricane
The 1940 Nova Scotia hurricane swept through areas of Atlantic Canada in mid-September 1940. The fifth tropical cyclone and fourth hurricane of the year, it formed as a tropical depression east of the Lesser Antilles on September 7, though at the time weather observations in the area were sparse, so its formation was inferred. The disturbance gradually intensified throughout much of its early formative stages, attaining tropical storm strength on September 10; further strengthening into a hurricane north of Puerto Rico occurred two days later. Shortly thereafter, the hurricane recurved northward, and reached peak intensity the following day as a Category 2 hurricane with maximum sustained winds of 100 mph (160 km/h) and a minimum barometric pressure of at least 988 mbar (hPa; 29.18 inHg). The cyclone steadily weakened thereafter before making landfall on Nova Scotia on September 17 with winds of 85 mph (135 km/h). Moving into the Gulf of Saint Lawrence later that day, the storm transitioned into an extratropical cyclone. The remnant system curved eastward and passed over Newfoundland before dissipating over the Atlantic on September 19. While off of the United States East Coast, the hurricane caused numerous shipping incidents, most notably the stranding of the Swedish freighter ''Laponia'' off of Cape Hatteras, North Carolina on September 16. Two other boat incidents resulted in two deaths. The hurricane also brought strong winds of tropical storm-force and snow over areas of New England. In Atlantic Canada, a strong storm surge peaking at 4 ft (1.3 m) above average sunk or damaged several ships and inundated cities. In New Brunswick, the waves hurt the lobster fishing industry. In Nova Scotia, strong winds disrupted telecommunication and power services. The winds also severely damaged crops. Roughly half of apple production in Annapolis Valley was lost during the storm, resulting in around $1.49 million in economic losses. Strong winds in New Brunswick caused moderate to severe infrastructural damage, and additional damages to crops occurred there. Overall, the hurricane caused three fatalities, with two off of the United States and one in New Brunswick. ==Meteorological history==
The origins of the system can be traced to a tropical depression roughly midway between the Lesser Antilles and the west coast of Africa at 1800 UTC on September 7. Though initially believed to have developed on September 11, the disturbance was found to have formed earlier in post-season reanalysis, based on data from the International Comprehensive Ocean-Atmosphere Data Set. In its early developmental stages, the disturbance remained a tropical depression with little change in intensity. At 0600 UTC on September 10, it intensified into a tropical storm while still east of the Lesser Antilles. Closer to the islands, ships reported a quickly intensifying tropical cyclone with low barometric pressures, strong winds and heavy thunderstorms, although most of the activity occurred to the east of its center.〔〔 At 1800 UTC on September 12, the storm intensified into the equivalent of a modern-day Category 1 hurricane to the north of Puerto Rico. The following day, the hurricane began to recurve northward, attaining Category 2 intensity at 1200 UTC.〔 Numerous vessels in its vicinity reported hurricane-force winds; the ''S.S. Borinquen'' observed a minimum peripheral pressure of 988 mbar (hPa; 29.18 inHg), the lowest observed pressure associated with the hurricane.〔〔 At the time, the storm had maximum sustained winds of 100 mph (160 km/h), which it maintained throughout its duration as a Category 2 system. Progressing rapidly into more northerly latitudes, the storm weakened to a Category 1 hurricane by 1800 UTC on September 15. By the next day, two warm fronts began extending eastward from the cyclone as the wind field expanded in size, indicating the start of an extratropical transition. At 0200 UTC, the hurricane made landfall near Lockeport, Nova Scotia, with winds of 85 mph (135 km/h).〔 The storm fully transitioned into an extratropical cyclone over the Gulf of Saint Lawrence by 1200 UTC on September 17. In the gulf, the system turned eastward, causing it to move ashore Newfoundland just north of Cape Race during the evening of September 18.〔 After passing over the island, the extratropical storm reentered the Atlantic Ocean, where it gradually weakened before dissipating on September 19.
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