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By early on October 6, a low pressure area and circulation persisted over eastern Cuba in the middle levels of the atmosphere. The low drifted westward, and interacted with Hurricane Klausto its east.[1] Initially cold-core in nature, the system gradually built downward to the surface, and on October 9, the low developed a low-level circulation; at 1200 UTC the National Hurricane Center classified it as Tropical Depression Fifteen while located near the Cuban city of Caibarién,[2] though the cyclone was initially subtropical in character.[3] To its east, Tropical Storm Klaus continued to weaken; the depression absorbed most of Klaus and became the dominant system.[1] The storm tracked parallel to the coast of Cuba before veering northward and crossing the Florida Keys, where it intensified into Tropical Storm Marco about 35 mi (55 km) south-southeast of Key West, Florida.[2]
After passing midway between Key West and the Dry Tortugas, Tropical Storm Marco adopted a steady northward track and quickly intensified, reaching peak winds of 65 mph (100 km/h) on October 11, while still southwest of Englewood, Florida. The center of the storm continued on its off-shore parallel for another six hours after reaching its peak intensity, until it reached a position about six mi (10 km) west of Bradenton Beach; although the center of the storm remained offshore, much of its circulation was over land.[2] Initially the storm still was forecast to move ashore between Fort Myers and Sarasota.[4] However, the cyclone continued its northward trajectory, the center remaining offshore, and it weakened to a tropical depression prior to making landfall near Cedar Key early on October 12.
