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Tropical Storm Larry was the twelfth tropical storm in the 2003 Atlantic hurricane season. It was one of eight storms to impact Mexico from either the Pacific or Atlantic Oceans in the season, a near-record. Larry formed in early October from an extratropical storm in the Bay of Campeche, and reached a peak intensity of 65 mph (100 km/h). Due to weak steering currents, the storm moved southward, which resulted in the storm hitting the Tabasco coastline. The storm was the first Tabascan landfall since Tropical Storm Brenda in 1973. Larry drifted across the Isthmus of Tehuantepec, dropping heavy rainfall of over 9 in (229 mm) in places. The rainfall led to flooding and mudslides, causing damage to thousands of houses. The flooding killed five people and resulted in $53.6 million (2003 USD) in damage. Larry was one of three tropical cyclones to hit Mexico in a short period of time, including Tropical Depression Nora and Tropical Storm Olaf in the eastern Pacific Ocean. ==Meteorological history== A tropical wave moved off the coast of Africa on September 17. It moved across the shear-ridden Atlantic Ocean without development, and remained disorganized until reaching the western Caribbean Sea on September 26. There, the wave situated itself beneath an upper-level anticyclone, allowing for favorable upper-level outflow and for deep convection to develop. On the September 27, a low pressure area developed while the system was located a few hundred miles to the east of the Yucatán Peninsula. The system continued to organize, and nearly developed into a tropical depression before moving ashore on the Yucatán Peninsula on September 29. Dry air and land weakened the tropical wave, and when it entered the area of the Bay of Campeche, it merged with a stationary frontal boundary. Cool, dry air around the system caused the system to develop a cold core, and the area organized into an extratropical low on September 30. A large high pressure system over the northern Gulf of Mexico forced the system southward, where it developed significant convection. The system developed a warm core, and on October 1 the storm organized into Tropical Storm Larry while located 300 mi (483 km) east-southeast of Tampico, Mexico.〔 Weak steering currents allowed for Larry to drift westward at about two mph (3 km/h) while marginally favorable conditions allowed the storm to strengthen to a peak of 65 mph (105 km/h) on October 3. A mid-level ridge forced the storm more to the south-southeast, where after remaining a 60 mph (97 km/h) storm for three days, Larry made landfall on Paraíso in the Mexican state of Tabasco on October 5. It steadily weakened over land, and degenerated into a remnant low on October 6 while mid-way through the Isthmus of Tehuantepec. The remnant low turned to the southwest, and reached the eastern Pacific Ocean on the October 7.〔 The remnants of Larry re-organized in the eastern Pacific, with the National Hurricane Center indicating for the possibility of redevelopment into a tropical depression on October 9. However, the convection diminished, and further development was no longer anticipated. 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 Larry (2003)」の詳細全文を読む スポンサード リンク
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