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What Made the Halloween Nor'easter of '91 the 'Perfect Storm'?

This Halloween marks the 22nd anniversary of the "Perfect Storm," also known as the Halloween Nor'easter of 1991.

In 1997, a book based on the storm was written, which was then made in to an Oscar-nominated movie in 2000. They told the tale of the six Gloucester, Mass., fishermen who died at sea when the storm's massive waves, some of which reached 39 feet, capsized their boat. These pieces of pop culture have helped the notoriety of the storm, but what exactly was it that made the storm "perfect"?

According to AccuWeather Senior Expert Meteorologist Dan Kottlowski it was the combination of a tropical system, the remnants of Hurricane Grace, and a non-tropical system that created such a massive storm.

The conditions had to come together just right to allow these systems to feed off of one another the way that they did. Grace had weakened enough so that it could be pulled in by the non-tropical system, but still contained enough deep moisture for it to feed into the cold. When tropical moisture is added to cold air in such a way it creates enormous amounts of energy, which leads to increased rain and wind.

While these conditions are rare, this was not a one-time occurrence. The storm's iconic name and its popularity in film and literature have greatly helped make this storm stand out the most, but according to Kottlowski, storms from such conditions have occurred since then.

Satellite image of the Perfect Storm. Photo courtesy of Wikimedia Commons.

"It's rare for a tropical and a non-tropical system to join," he said. "But these conditions are favored this time of year. Late October to early November southern Atlantic waters are still warm enough for a tropical system, but cold air is already coming down from Canada. It's the right time for these systems to meet."

The Gale of 1878, for example, was created with similar conditions. In late October a tropical system moved out of the Keys northward along the East Coast, bringing 4.5 inches of rain to Cape Hatteras, N.C. By the time the storm reached Philadelphia, it met with a cold air system. The result was hurricane-force winds on Oct. 23 in the city and its surrounding areas, up to 72 mph. Estimates gauge that from 500-700 buildings were destroyed.

Superstorm Sandy was another similar storm, since it was part tropical and part nor'easter.

The technology for forecasting storms today is not that much different than it was in 1991. According to Kottlowski, the big difference now is what people know about utilizing the data that satellites bring in. While this same data was available in 1991, forecasters and researchers have made breakthroughs in their diagnostic formats so that storms can be detected and tracked better.