"By only focusing on the 2004 and 2005 seasons, it is easy to forget that every hurricane season is unique and actual landfall activity is a function of complex interactions between a range of environmental factors such as genesis location, sea surface temperatures and the depth of warm ocean waters, wind shear, and atmospheric steering," said Dr. Peter Dailey, director of research in atmospheric science at AIR Worldwide. "A higher number of tropical storms in the Atlantic basin does not translate to an equivalent increase in hurricanes or landfalling hurricanes."
AIR researchers found that a storm's genesis location, or starting point, greatly influences its probability of making landfall along the North American coastline. The pattern of hurricane genesis locations changes from year to year and by comparing the pattern for a particular season to long-term climatological patterns, one can better understand why in some years the proportion of storms making landfall is high, while in other years it is low.
AIR's research can be used to analyze the landfall probabilities of the two strongest storms of the 2007 season—Category 5 hurricanes Dean and Felix—based on their genesis locations. Dean and Felix, which were the only storms this year to achieve greater than Category 1 status, both took southerly tracks across the Caribbean and eventually made landfall along the coasts of
"Contrary to popular belief, the
Sea surface temperatures in the Atlantic basin have been warmer than average every year since 1995. However, the percentage of Atlantic basin storms that make
"The seasonal forecasters correctly projected that a higher-than average number of tropical storms would form in the basin in 2007," continued Dr. Dailey. "But it's much more difficult to predict not only how many of these storms will become hurricanes, but more importantly how many will make landfall as hurricanes. Like many past seasons, the 2007 season showed that an elevated number of tropical storms does not always translate to more hurricanes or more landfalling hurricanes. In 2007, sea surface temperatures were not as warm as some scientists expected and significant wind shear suppression by La Niña did not materialize as they had anticipated. Clearly there's a danger in assuming that one or two single seasons are indicative of a paradigm shift in hurricane risk. While 2004 and 2005 were both very active seasons, they were not good predictors of activity in 2006 and 2007."