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Tropical Storm Trudy was a short-lived tropical cyclone in October 2014 that caused significant flooding in southern Mexico. The storm originated from an area of low pressure associated with a monsoon trough near Central America in early October. A slow-moving system, the low eventually consolidated into a tropical depression on October 17 near the Mexican coastline. Favorable environmental conditions aided rapid development of Trudy. Within 15 hours of its designation, an eye formed over the storm's center. Trudy ultimately achieved its peak as a strong tropical storm with 65 mph (100 km/h) winds as it made landfall just southeast of Marquelia, Mexico. The region's mountainous terrain quickly weakened Trudy and the cyclone dissipated early on October 19. Though the cyclone dissipated, its remnant energy later contributed to the formation of Tropical Storm Hanna in the Atlantic. Prior to Trudy's landfall, the Government of Mexico issued multiple watches and warnings for the threatened region. Forecasters highlighted the threat of heavy rains and mudslides. Guerrero experienced the greatest effects from Trudy, with landslides and flooding claiming eight lives in the state. Over 4,000 people were evacuated in the region. A ninth fatality took place in Campeche. ==Meteorological history== On October 8, a weak area of low pressure developed within a monsoon trough over the extreme eastern edge of the Pacific basin. Environmental conditions ahead of the system were forecast to become gradually favorable for tropical cyclogenesis. Situated near Costa Rica, scattered convection accompanied the well-defined system. This low became less defined over the following days while remaining in the same general area. The National Hurricane Center (NHC) began monitoring the system for long-term cyclogenesis on October 13, at which time the low was situated 150 mi (240 km) south of Guatemala. Organization was prolonged and slow; however, the convergence of a Kelvin wave and a Gulf of Tehuantepec gap wind event on October 15 spurred a significant increase in convection.〔 Marked structural improvements took place on October 17 and the NHC assessed a high probability of the system becoming a tropical cyclone within 48 hours. That evening, corroborating data from ships, satellite imagery, and scatterometer estimates indicated the formation of a tropical depression by 12:00 UTC.〔 With the cyclone located over warm waters of 86 °F (30 °C) and within a very moist region with low wind shear, intensification was a certainty as the depression approached Mexico. Uncertainties existed as to how fast the system would move. Some forecast models depicting the system as stalling just offshore for several days, though forecasters indicated that a steady northward movement would lead to dissipation within 48 hours. Owing to the aforementioned environmental conditions, the depression intensified to a tropical storm by 18:00 UTC on October 17;〔 it was subsequently assigned the name ''Trudy'' by the NHC. Very deep convection blossomed over both the center and accompanying banding features. During the morning of October 18, a central dense overcast became increasingly defined; microwave satellite imagery and coastal radars depicted the formation of a 12 to 17 mi (19 to 27 km) wide eye by 03:00 UTC.〔 It is estimated that Trudy reached its peak intensity around 09:15 UTC on October 18 with maximum sustained winds of 65 mph (100 km/h) and a barometric pressure of 998 mbar (hPa; 29.47 inHg). Simultaneously the storm made landfall just southeast of Marquelia, or roughly 70 mi (110 km) east of Acapulco. Interaction with the mountainous terrain of Mexico quickly took its toll on Trudy, with the system degrading to a tropical depression by 18:00 UTC. The low-level circulation of the depression dissipated early on October 19, with its mid-level remnants continuing northeastward over Mexico. The remnant system emerged over the Bay of Campeche on October 20 and subsequently developed into Atlantic Tropical Depression Nine—which later became Tropical Storm Hanna—on October 22. Due to the dissipation of its surface low, Trudy and Hanna are considered separate tropical cyclones by the NHC.〔 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 Trudy (2014)」の詳細全文を読む スポンサード リンク
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