Fred was the second hurricane and sixth named storm of the 2015 Atlantic hurricane season. Fred originated from a well-defined tropical wave over West Africa in late August 2015. It became easternmost tropical cyclone ever in the tropical Atlantic, with a minimum pressure of 986mbar and a maximum sustained winds of 90mph.
About Hurricane Fred (2015) in brief

It was also among the four easternmost locations for a tropical Storm to form since modern record-keeping began in 1851. The storm developed a thick, circular central dense overcast with good outflow and the eye feature became well established at all levels of the circulation. Fred moved through a region with ample tropical moisture, light upper winds, and above-average sea surface temperatures. It then turned to the west-northwest, enduring increasingly hostile wind shear, but maintained its status as a tropical Cyclone despite repeated forecasts of imminent dissipation. The hurricane traversed the Barlavento Islands, barely skirting the southern coast of Boa Verde, skirting southern air-norter over the next 12 hours. Fred dissipated on September 7, with winds decreasing gradually in definition, decreasing in definition and decreasing in intensity. It became a tropical depression on September 8, with sustained winds of 35 mph and a low-level circulation center near Guinea’s coastline. On September 9, the depression was upgraded to Tropical Storm Fred while 390 mi east-southeast of Praia, Cape Verde. It later weakened to tropical Storm Fred, centered 165mi east-east-1, east-southwest of Sal, and then upgraded again to a tropical Cyclone. The cyclone was the fourth named storm in the Atlantic Ocean this year.
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This page is based on the article Hurricane Fred (2015) published in Wikipedia (as of Dec. 05, 2020) and was automatically summarized using artificial intelligence.






