Meteorological History
On June 24 a vigorous tropical wave moved off the African coast and quickly west across the Atlantic without developing. The wave gradually became more organized as it crossed the Caribbean and late on July 3 it strengthened into Tropical Depression Three about 80 miles (130 km) east of Chetumal, Mexico. The models initially had difficulty predicting the track of the depression and the forecasts from the National Hurricane Center reflected this, indicating that the depression would move towards Texas. The depression developed quickly before making landfall on Yucatán Peninsula early on July 4 with 35 mph (55 km/h) winds and began to lose its circulation overland.
A new center of circulation began forming later on July 4, over the Gulf of Mexico, to the north of the original center. This reformation caused a significant alteration in the forecast models, which now indicated a landfall in Louisiana. The depression moved northwards into the Gulf of Mexico and became a Tropical Storm Cindy early on July 5. Weakened shear allowed Cindy to strengthen further as it approached Louisiana and the storm was a minimal hurricane with 75 mph (120 km/h) winds when it made landfall near Grand Isle late on July 5. Initially it was felt that Cindy did not reach hurricane strength, but post-season reanalysis confirmed the upgrade.
Hurricane Cindy weakened back into a tropical storm as it crossed over extreme southeastern Louisiana and Breton Sound before making a second landfall near Waveland, Mississippi with 50 mph (85 km/h) winds on July 6. Cindy moved to the northeast over Mississippi and Alabama, weakening to a tropical depression that day. The depression became extratropical over the Carolinas on July 7 and moved to the northeast dissipating in the Gulf of St Lawrence on July 9.
Read more about this topic: Hurricane Cindy (2005)
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