Early on the following day, the system had developed into Tropical Depression Three while nearly halfway between the west coast of Africa and the Windward Islands. However, in post-analysis, it was revealed that the previous tropical depression had actually developed before Bonnie. Thus, those two depressions were operationally numbered incorrectly. Two reports of gale-force winds were received from ships later that day. As a result, the depression was re-classified as Tropical Storm Bonnie about twelve hours after developing. Bonnie turned in a general northward direction, possibly due to interaction with nearby Tropical Depression Four. Based on satellite estimates, Bonnie was upgraded to a hurricane at 0000 UTC on August 16. The storm strengthened slightly further and attained its peak intensity with winds of 100 mph (155 km/h) and a minimum pressure of . After attaining peak intensity on August 16, Bonnie slowly weakened as it continued in an unusual northward direction. On the following day, Bonnie weakened slightly to a minimal Category 1 hurricane. The storm remained at that intensity for 72 hours as it accelerated northward across the open Atlantic. By 1800 UTC on August 19, Bonnie transitioned into an extratropical cyclone while almost halfway between the southern tip of Greenland and the Azores. Hurricane Charley An extratropical low pressure system was centered over the Mid-Atlantic United States, though it tracked southeastward and emerged into the Atlantic on August 20. Later that day, satellite imagery indicated that a well-defined low-level circulation. As a result, it was determine that the system developed into a subtropical depression at 1200 UTC, while located about east-northeast of Hatteras, North Carolina. Initially, the depression tracked east-southeastward, though it curved east-northeastward by August 21. Shortly thereafter, the depression strengthened into a subtropical storm. By early on August 23, the storm had intensified and acquired enough tropical characteristics to be re-classified as Hurricane Charley. At 1200 UTC on August 23, Charley attained its peak intensity with winds of 80 mph (130 km/h) and a minimum pressure of . Following peak intensity, Charley completed a cyclonic loop and began weakening as it headed almost due-east. Charley was downgraded to a tropical storm early on August 24. The storm continued eastward and by August 26, Charley became unidentifiable as it merged with an intense extratropical cyclone, while located about southeast of Cape Race, Newfoundland. While a tropical cyclone, Charley produced rip currents along the Outer Banks of North