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Hurricanes are the most powerful tropical storms to reach the
New York area with wind speeds in excess of 74 mph. Records are
available for 24 hurricanes that have affected the New York area
in the past century. The heaviest storm damage usually occurs
when high astronomical tides and storm surge coincide.
Extratropical storms also affect the study area. While extratropical
storms or northeasters are usually less intense than hurricanes,
they tend to have a much longer duration and cover larger areas.
Often lasting for a period of days, these storms persist through
several periods of high astronomical tide. The long duration of
extratropical storms greatly enhances their ability to cause damage.
During the passage of a major extratropical or tropical storm,
a temporary rise in water level is often generated, creating a
storm surge. Rising water levels are also evident as propagating
waves break near the coast in a process called wave setup. Historically,
the combined effects of storm surge and wave setup with astronomical
tides have caused extreme water levels in the study area which,
in turn, have lead to severe property damage on both barrier island
and mainland areas.
One example of a major storm is the hurricane of September 21,
1938, which caused severe damage on both the barrier island and
mainland areas. Between Fire Island Inlet and Montauk Point, large
areas were inundated, causing extensive damage. Over 700 homes
on Fire Island were damaged, while nearly 300 were destroyed.
Twelve new inlets, including Shinnecock Inlet, were formed along
the south shore barrier beaches. Twenty square miles of the mainland
were inundated as storm tides overtopped Fire Island. The low
density of mainland development at that time resulted in minimal
damages. However, a recurrence of these flood stages under today's
level of development would flood approximately 8,500 mainland
structures up to 6 feet in depth.
Another example of the storm damage problem is the extratropical
storm of March 6, 1962. A total of 50 washovers occurred, and
one new inlet at Westhampton Beach was formed. On Fire Island,
a total of 47 homes were destroyed and 75 were damaged. Twelve
square miles of the mainland were inundated; under current development
conditions, a recurrence of these flood stages would mean that
approximately 4,500 structures would be inundated up to 6 feet
in depth. As a result of this storm, the New York District of
the Army Corps constructed emergency protective works throughout
the study area ("Operation Five-High"). Assistance was
provided to the local communities in the removal of debris, and
in the rebuilding of beaches and dunes. One of the first response
actions of the Corps was to assist in the closure of the breach
at Westhampton. In total, over 2 million cubic yards of material
were used to rebuild over 23 miles of beaches and dunes in the
study area.
Many severe storm events have impacted the study area in just
the last decade. Events in September 1991, December 1992, November
1996, September 1999 have led to federal disaster declarations
for Suffolk County. These four storms caused over $14 million
dollars in damages to public infrastructure alone. The historic
trends of increasing coastal development and sea-level rise have
contributed to Suffolk County's current storm damage problem.
Over the next 50 years, sea levels are forecast to continue rising,
resulting in more frequent and severe storm damage. Given this
combination of factors, the storm damage problem in Suffolk County
is expected to intensify.
For more information please read the Fire
Island Inlet to Montauk Point Project Fact Sheet or email the
Project Manager.
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