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Tropical Storm Carlos (2003)
Tropical Storm Carlos was the first of five tropical cyclones to make landfall during the 2003 Pacific hurricane season. It formed on June 26 from a tropical wave to the south of Mexico. It quickly strengthened as it approached the coast, and early on June 27 Carlos moved ashore in Oaxaca with winds of 65 mph (100 km/h). The storm rapidly deteriorated to a remnant low, which persisted until dissipating on June 29. Carlos brought heavy rainfall to portions of southern Mexico, peaking at 337 mm (13.3 in) in two locations in Guerrero. Throughout its path, the storm damaged about 30,000 houses, with a monetary damage total of 86.7 million pesos (2003 MXN, $8 million 2003 USD). At least nine people were killed throughout the country, seven due to mudslides and two from river flooding; there was also a report of two missing fishermen.
== Meteorological history ==
The origins of Carlos were from a tropical wave that exited the west coast of Africa on June 14. The wave moved westward across the Atlantic Ocean and Caribbean Sea, with little evidence of its existence on satellite imagery. By June 20 it crossed Central America into the eastern Pacific Ocean, later spawning an area of convection, or thunderstorms, south of the Gulf of Tehuantepec. The National Hurricane Center (NHC) first mentioned the system in its tropical weather outlook on June 24, by which time a low pressure center developed. Gradually, the system continued to develop due to light wind shear, with rainbands and convection located near the broad center. By early on June 26, the disturbance had organized enough for the NHC to initiate advisories on Tropical Depression Three-E, about 130 miles (210 km) south-southwest of Puerto Escondido, Oaxaca.
Upon first being classified as a tropical cyclone, the depression had a slightly elongated circulation. An anticyclone to its north was forecast to track westward, which would allow the depression to track west-northwestward and remain offshore; however, the NHC noted uncertainty in its motion.〔 The cloud pattern gradually organized, with warm water temperatures and lessening wind shear. At 1200 UTC on June 26, it is estimated the depression attained tropical storm status; upon doing so, the NHC named the storm Carlos.〔 As it reached tropical storm intensity, Carlos began an erratic northward track toward the Mexican coast, under the influence of a trough. It quickly strengthened, developing a well-defined eye feature in the center of the convection. Based on the eye, it is estimated Carlos made landfall early on June 27 with peak winds of 65 mph (100 km/h), about 60 miles (95 km) west of Puerto Escondido, Oaxaca, or about 150 miles (245 km/h) east-southeast of Acapulco, Guerrero.〔
As Carlos moved inland, it turned to the northwest in response to the anticyclone over Mexico, and it quickly weakened to tropical depression status.〔 By 12 hours after landfall, there was little evidence of a circulation on satellite imagery. Late on June 27, Carlos degenerated into a non-convective remnant low pressure area near Acapulco. The circulation turned to the southwest and emerged into the Pacific Ocean; by 0000 UTC on June 29, the system dissipated completely.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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