Tropical Storm Arlene (1959) - Meteorological History

Meteorological History

Tropical Storm Arlene developed out of a tropical wave which was first noted near the Dominican Republic on May 23. The wave slowly developed as it moved westward through the Caribbean Sea and developed into an area of low pressure on May 25. By May 27, the low entered the Gulf of Mexico and a ship report the next day showed that the low had developed a closed low-level circulation. Early the next morning, the low was determined to have intensified into Tropical Storm Arlene, the first storm of the season, while located 300 mi (480 km) south-southeast of New Orleans, Louisiana with winds estimated at 40 mph (65 km/h). Arlene was moving towards the northwest at 10 to 15 mph (16 to 24 km/h). Arlene slowly intensified throughout the day as it continued towards the northwest at 12 to 15 mph (19 to 24 km/h). On May 29, Arlene turned towards the west and its foreword motion slowed before becoming nearly stationary that night.

The storm was located 150 mi (240 km) south of Lafayette, Louisiana as it drifted northward and winds were estimated to have peaked at 50 mph (85 km/h). However, in the post-season, it was determined that Arlene peaked near landfall with winds of 60 mph (95 km/h). As Arlene neared the coast, the storm began to weaken due to the interaction with land. Arlene made landfall about 40 mi (65 km) southeast of Lafayette, Louisiana at 2100 UTC (4 p.m. CST). The operational landfall intensity was 50 mph (85 km/h) but it was lowered to 45 mph (75 km/h) in the post season. Upon making landfall, Arlene became the earliest landfalling tropical cyclone in Louisiana history. Arlene weakened quickly to a tropical depression shortly after landfall. The storm further degenerated to a remnant area of low-pressure on the afternoon of May 31. The remnant of the storm lingered in the Southern United States until June 2, when it dissipated over South Carolina. Although the original low pressure system dissipated, a new, non tropical center formed further north over Virginia. This new low quickly tracked northeast, brushing the southern coast of New England before moving over Nova Scotia and losing its identity on June 3.

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