ImpactsThe simplest characterization of hurricane intensity is embodied in the Saffir-Simpson scale: from Category 1 ---barely a hurricane--- to Category 5 ---the worst imaginable. "Major Hurricanes" are those in Categories 3, 4, and 5 with winds stronger than 110 miles per hour equivalent to 100 kt or 50 m s-1. Category 5 hurricanes are the most extreme and also the most rare. Only two, the 1935 Labor Day Storm and Camille in 1969 are recorded to have struck the United States. Andrew, at the very top of Category 4 was the third strongest U.S. landfall, and the second strongest on the mainland, given that the 1935 storm hit the Florida Keys. The 1995 through 1999 seasons inclusive have been the five most
active in the > 100-year quantitative climatology. Historically,
hurricane landfalls on the U.S. east coast were common during
the 1940s through the mid 1960s. In the 1970s and 1980s, landfalls
were few. Now activity appears to have returned to the high level
that characterized the immediate post-World War II period. These
fluctuations in activity are most pronounced for major hurricanes.
They also correlate with the observed "North Atlantic Mode", a
coherent, multidecadal fluctuation of global sea-surface temperatures.
During the active portion of the long-term record, Atlantic Sea-Surface
Temperature (SST) anomalies in tropics and high latitudes were
warm, and conversely.
In terms of hurricane-related mortality,
the 20th Century started badly. In Galveston Texas,
on a single windy Saturday night, 9 September 1900, the "Great
Hurricane" washed > 6,000 souls to their deaths. The total mortality
for the century was just a bit more than twice this figure, 13,306
U.S. residents. During the first three decades of the century,
the average annual loss of life was 329, or discounting the Galveston
tragedy, 129. In the forty years from 1930 through 1969, it was
70. The reason for the dramatic reduction has been effective warnings
and timely evacuation from coastal areas inundated by storm surge.
Invariably, large loss of life in hurricanes before 1970 stemmed
from wind-driven flooding. Since 1970 drowning from inland flooding
caused by torrential hurricane rains has come to predominate.
Experience shows that when storm surge (or wind for that matter)
completely flattens buildings, about 10% of the people present
die. Evacuation insures that virtually nobody is present. On the
other hand, extreme ( > 30 cm in 6 hr) rainfall places a much
larger population at individually smaller risk.
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