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Saffir-Simpson
Hurricane Scale
| Scale
Number (Category) |
Sustained Winds (MPH) |
Damage | Examples (States Affected) |
|
1
|
74-95
|
Minimal
|
Florence 1988
(LA) |
|
2
|
96-110
|
Moderate
|
Kate 1985 (FL
Panhandle) |
|
3
|
111-130
|
Extensive
|
Alicia 1983 (N
TX) |
|
4
|
131-155
|
Extreme
|
Andrew 1992 (S FL) |
|
5
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>
155
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Catastrophic
|
Camille
1969 (LA/MS)
Labor Day Hurricane 1935 (FL Keys) |
Timely warnings have greatly diminished hurricane fatalities in the United States.
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Breeding Grounds
In the eastern
Pacific, hurricanes start forming by mid-May. In the Atlantic, Caribbean, and
Gulf of Mexico, hurricanes season starts in June. For the United States, peak
hurricane threat exists from mid-August to late October although the official
hurricane season extends through November. Over other parts of the world, such
as the western Pacific, hurricanes can occur year-round. Developing
hurricanes gather heat and energy through contact with warm ocean waters. The
addition of moisture by evaporation from the sea surface powers them like giant
heat engines. Storm Structure
The process by which a disturbance forms and subsequently strengthens into a hurricane depends on at least three conditions. Warm waters and moisture are mentioned above. The third condition is a wind pattern near the ocean surface that spirals air inward. Bands of thunderstorms form, allowing the air to warm further and rise higher into the atmosphere. If the winds at these higher levels are relatively light, this structure can remain intact and allow for additional strengthening. The center, or eye, of a hurricane is relatively calm. The most violent activity takes place in the area immediately around the eye, called the eyewall. At the top of the eyewall (about 50,000 feet), most of the air is propelled outward, increasing the air's upward motion. Some of the air, however, moves inward and sinks into the eye, creating a cloud-free area. |
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Storm FuryStorm SurgeStorm surge is a
large dome of water often 50 to 100 miles wide that sweeps across the coastline
near where a hurricane makes landfall. The surge of high water topped by waves
is devastating. The stronger the hurricane and the shallower the offshore water,
the higher the surge will be. Along the immediate coast, storm surge is the
greatest threat to life and property. |
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Storm Tide
If the storm
surge arrives at the same time as the high tide, the water height will be even
greater. The storm tide is the combination of the storm surge and the normal
astronomical tide. For example as hurricane
moves ashore, a 15-foot surge added to the normal 2-foot tide creates a storm
tide of 17 feet. This mound of water, topped by battering waves, moves ashore
along an area of the coastline as much as 100 miles wide. The combination of the
storm surge, battering waves, and high winds is deadly. Storm Tide Facts
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Winds
Hurricane-force
winds, 74 mph or more, can destroy poorly constructed buildings and mobile
homes. Debris, such as signs, roofing material, siding, and small items left
outside, become flying missiles in hurricanes. Winds often stay above hurricane
strength well inland. Hurricane Hugo (1989) battered Charlotte, North Carolina
(which is about 175 miles inland), with gusts to near 100 mph, downing trees and
power lines and causing massive disruption. |
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Heavy Rains/Floods
Widespread torrential
rains often in excess of 6 inches can produce deadly and destructive floods.
This is the major threat to areas well inland.
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Tornadoes
Hurricanes also produce tornadoes, which add to the hurricane's destructive power. These tornadoes most often occur in thunderstorms embedded in rain bands well away from the center of the hurricane. However, they can also occur near the eyewall. |
Click here to find out more about watches and warnings and what to do if a hurricane threatens your area.
Click here for a list of hurricane and cyclone names.
Source: http://www.nws.noaa.gov
Graphics Source: AP