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| Asheville, NC, March 14, 1993. Source: NOAA |
As summarized in the now classic paper by Kocin et al. (1995), the Superstorm began as disorganized low over the Gulf of Mexico, but deepened 17 mb in 12 hours to reach 984 mb when it was just south of Louisiana. As it moved up the eastern seaboard, the central pressure dropped to 971 mb over Georgia and 960 mb over Delaware. The storm set record low sea level pressures at locations spanning from Georgia to Maine.
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| Source: Kocin et al. (1995) |
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| Source: Kocin et al. (1995) |
Prior to the Superstorm, forecasts for nor'easters were not known for their reliability. As a budding young skier in the northeast, I recall many surprise storms and great forecast disappointments. Storms such as the 1979 President's Day Cyclone, which produced the largest snowfall accumulation in Washington D.C. in 50 years, were poorly forecast by the numerical models of the day (e.g., Uccellini et al. 1984).
By 1993, however, the resolution and capability of numerical models had reached a point where they were becoming more skillful at predicting nor'easters and forecasters were able to process and take maximum advantage of these forecasts. The forecasts for the Superstorm were especially noteworthy. As summarized by Uccellini et al. (1995), the Superstorm cyclogenesis was predicted up to 5 days in advance, the unusual intensity of the storm 3 days in advance, and the excessive snowfall amounts and coverage two days advance. It was a major forecast victory.
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| Headline from the Boston Herald prior to the Superstorm. Source: Uccellini et al. (1995) |






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