See NHC's new Storm Surge web page (launched September 2010)
Learn about Probabilistic Storm Surge Products
One
tool used to evaluate the threat from storm surge is the SLOSH
model. Emergency managers use this data from SLOSH to determine which areas
must be evacuated for storm surge. The links below provide some altered photos
that show how the intensity of the storm (as given by the Saffir-Simpson
Hurricane Scale) affects the possibility of flooding from storm surge at
two locations. Storm surge also affects rivers and inland lakes, potentially
increasing the area that must be evacuated. You can see some of these effects
by looking at simulated storm surge pictures for Brunswick,
GA, New Orleans, LA, Brooklyn,
NY, Wrightsville Beach, NC and Manteo,
NC. In
general, the more intense the storm, and the closer a community is to the right-front
quadrant, the larger the area that must be evacuated. The problem is always
the uncertainty about how intense the storm will be when it finally makes landfall.
Emergency managers and local officials balance that uncertainty with the human
and economic risks to their community. This is why a rule of thumb for emergency
managers is to plan for a storm one category higher than what is forecast. This
is a reasonable precaution to help minimize the loss of life from hurricanes. Wave
and current action associated with the tide also causes extensive damage. Water
weighs approximately 1,700 pounds per cubic yard; extended pounding by frequent
waves can demolish any structure not specifically designed to withstand such
forces.
RELATED
INFORMATION RELATED
MULTIMEDIA ADDITIONAL
SAFETY INFORMATION STORM SURGE
SAFETY ACTIONS HISTORIC
STORM SURGE EVENTS
Storm
surge is simply water that is pushed toward the shore by the force of the winds
swirling around the storm. This advancing surge combines with the normal tides
to create the hurricane storm tide, which can increase the mean water level
15 feet or more. In addition, wind driven waves are superimposed on the storm
tide. This rise in water level can cause severe flooding in coastal areas, particularly
when the storm tide coincides with the normal high tides. Because much of the
United States' densely populated Atlantic and Gulf Coast coastlines lie less
than 10 feet above mean sea level, the danger from storm tides is tremendous.
The
level of surge in a particular area is also determined by the slope of the
continental shelf. A shallow slope off the coast (right, top picture) will
allow a greater surge to inundate coastal communities. Communities with
a steeper continental shelf (right, bottom picture) will not see as much
surge inundation, although large breaking waves can still present major
problems. Storm tides, waves, and currents in confined harbors severely
damage ships, marinas, and pleasure boats.


The
currents created by the tide combine with the action of the waves to severely
erode beaches and coastal highways. Many buildings withstand hurricane force
winds until their foundations, undermined by erosion, are weakened and fail.
STORM
SURGE SAFETY ACTIONS
SLOSH
MODEL
SAFFIR
SIMPSON HURRICANE SCALE
HISTORIC
STORM SURGE EVENTS
MAX
MAYFIELD DISCUSSES - STORM
SURGE (0.3mb MP3
)
Hurricane Opal made landfall near Pensacola Beach, Florida as a Category 3
hurricane. The storm caused extensive storm surge damage from Pensacola Beach
to Mexico Beach (a span of 120 miles) with a maximum storm tide of 24 feet,
recorded near Fort Walton Beach. Damage estimates for Opal were near $3 billion.
More...
Devastated the West Indies and the Southeastern United States, including South
Carolina cities Charleston and Myrtle Beach. Hugo was responsible for sixty
deaths and $7 billion in damages, with a storm surge estimated at 19.8 feet
at Romain Retreat, South Carolina. More...
A Category 5 hurricane, the most powerful on the Saffir/Simpson Scale with
maximum winds of more than 200mph devastated the Mississippi coast. The final
death count for the U.S. is listed at 256. This includes 143 on the Gulf coast
and another 113 from the Virginia floods. More...
There were 390 deaths as the result of a storm surge
in excess of 12 feet, which inundated the flat coast of southwestern Louisiana
as far as 25 miles inland in some places. More...
A fast-moving Category 3 hurricane (the Long Island Express) that struck
Long Island and New England with little warning on September 21. A storm surge
of 10 to 12 ft inundated the coasts of Rhode Island, Connecticut, southeastern
Massachusetts, and Long Island, NY, especially in Narragansett Bay and Buzzards
Bay. Six hundred people died due to the storm. More...
A Category 4 hurricane that made landfall near Palm Beach on September 16
with a central pressure of 929 mb. The center passed near Lake Okeechobee,
causing the lake to overflow its banks and inundate the surrounding area to
a depth of 6 to 9 ft. 1,836 people died in Florida, primarily due to the lake
surge. More...
More than
6,000 people died when hurricane storm tides (the surge plus the astronomical
tide) of 8-15 feet inundated the entire island city of Galveston, TX. More...