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Join date : 2011-06-10
|Subject: Tropical Storm Barry Fri Jun 24, 2011 9:29 am|| |
Hurricane Barry originated from a tropical disturbance that left the Northwestern African coast on August 13. Most of the season, the northwestern tropical Atlantic Ocean had upper-level wind shear, which had inhibited development of systems. Due to these conditions, the disturbance was unable to strengthen until August 22 as it was approaching the Bahamas. A weak trough moved the disturbance into an area of low wind shear, and the disturbance intensified into Tropical Depression Four on the evening of August 23. The depression was just to the northeast of the northern Bahamian Islands where it strengthened into Tropical Storm Barry on the morning of August 24.
Tropical Storm Barry turned to the west and with returning wind shear, weakened into a tropical depression. The depression made landfall near Melbourne, Florida on the morning of August 25. After Tropical Depression Barry emerged from central Florida, it was still under pressure from high-level winds. The depression entered the central Gulf of Mexico and returned to tropical storm strength. Barry rapidly intensified, becoming a hurricane on August 28, making landfall near Brownsville, Texas that afternoon. Before landfall, Barry peaked with 80 mph (130 km/h) winds and a pressure of 986 millibars (29.11 inHg). The remnants dissipated over the northern Mexican mountains on August 29.send textgolf argentina