Continuing to weaken, the cyclone resumed a northward track after the high weakened and persisted through November 17, by which time it had moved over Atlantic Canada. On November 14, a brief secondary low developed within the system, off the coast of Delaware. Gradual weakening took place during this period, though heavy rains continued to fall across much of the Chesapeake Bay area. Due to the high pressure system situated over Vermont, the low turned southeastward, bringing its center back over water. Tracking parallel to the North Carolina coastline, the system eventually moved onshore near Cape Hatteras by November 13. In combination with a large area of high pressure, a long stretch of easterly, onshore winds impacted areas from Virginia to southern New England. By November 12, the system attained a minimum pressure of 992 mbar (hPa 29.29 inHg) along with winds of 65 mph (100 km/h). Due to the rapid succession of these systems, United States media referred to the nor'easter as 'Nor'Ida'. This new low quickly intensified and became a powerful nor'easter that caused substantial damage throughout the Mid-Atlantic States. However, Ida's mid-level circulation led to the formation of a new low over southeastern Georgia, which eventually moved off the coast of North Carolina. Ida eventually dissipated over the Florida Panhandle. The system eventually moved over the southeastern United States on November 10 before transitioning into an extratropical cyclone. Once in the Gulf of Mexico, the combination of increasing wind shear and cooler waters caused Ida to weaken. After tracking through Nicaragua as a Category 1 hurricane, the system attained Category 2 status over the Yucatán Channel. The origins of the nor'easter originated from with the remnants of Hurricane Ida, a storm that formed on November 4 over the southern Caribbean Sea.
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