![]() ![]() 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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