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Last modified
7/11/2016 10:40:07 AM
Creation date
9/30/2015 8:40:38 PM
Metadata
Fields
Template:
Official Documents
Official Document Type
Report
Approved Date
02/22/2005
Control Number
2005-070
Agenda Item Number
7.F.
Entity Name
Department of Emergency Services
Subject
Unified Local Mitigation Strategy 2005
Archived Roll/Disk#
4000
Supplemental fields
SmeadsoftID
4892
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occurred to residential construction . Fully engineered construction usually performs well in <br /> high winds due to the attention given to connections and load paths . <br /> Hurricane winds generate massive quantities of debris that can easily exceed a <br /> community' s entire solid waste capacity by three times or more . Debris removal is an <br /> integral first step toward recovery , and as such , must be a critical concern of call those tasked <br /> with emergency management and the restoration of community services . <br /> A storm surge is a large dome of water often 50 to 100 miles wide and rising <br /> anywhere from 4 to 5 feet in a Category 1 hurricane and up to 20 feet in a Category 5 storm . <br /> The storm surge arrives ahead of the storm ' s actual landfall , and the more intense the <br /> hurricane is , the sooner the surge arrives . Water rise can be very rapid , posing a serious <br /> threat to those who have waited to evacuate flood prone areas . A storm surg is a wave <br /> that has outrun its generating source and become a long period swell . The SL rge is always <br /> highest in the right-front quadrant of the direction the hurricane is moving in . As the storm <br /> approaches shore , the greatest storm surge will be to the north of the hurrica a eye . <br /> Such a surge of high water topped by waves driven by hurricane force winds can <br /> be devastating to coastal regions . The stronger the hurricane and the shallower the <br /> offshore water, the higher the surge will be . In addition , if the storm surge arrives at the <br /> same time as the high tide , the water height will be even greater. The storm tide is the <br /> combination of the storm surge and the normal astronomical tide . <br /> Damage during hurricanes also may result from possible spawned tornadoes , <br /> and inland flooding associated with heavy rainfall that usually accompany these storms . <br /> Hurricane Andrew, a relatively "dry" hurricane , dumped 10 inches of rain onsouth Florida <br /> and left many buildings extensively water damaged . Rainwater may seep into gaps in roof <br /> sheathing and saturate insulation and ceiling drywall , in some cases causing ceilings to <br /> collapse . <br /> Crop damage is another powerful effect of hurricanes and tropical storms , <br /> Recently , Tropical Storm Mitch dropped as much as 10 inches of rain in some south Florida <br /> areas , which resulted in approximately $20 million in crop damage in Palm Beach County <br /> alone (Associated Press , 1998 ) . According to the University of Florida (2001 ) of Indian <br /> River County's 322 , 112 acres , 168 , 399 acres are farmland . With 52 % of its land area being <br /> farmed , Indian River County is particularly vulnerable to crop damage resulting from the <br /> wind and rain from hurricanes and tropical storms . <br /> Historic Events. Specific information on previous occurrences of hurricanes and <br /> tropical storms is located in the flooding section . From 1930 through 1959 , a otal of <br /> 58 hurricanes struck the U . S . mainland ; 25 of which were Category 3 or higher ( major <br /> storms ) . Between 1960 and 1989 , 43 hurricanes struck the U . S . ; 16 of which were <br /> Category 3 or stronger. Most hurricane experts feel we are entering a period of increased <br /> hurricane formation similar to the levels seen in the 1930 ' s and 1940 ' s . Current hurricane <br /> risk calculations are complicated by climatic factors suggesting the potential for even greater <br /> hurricane frequency and severity in all of the world ' s hurricane spawning grou ids . Since <br /> 1995 , there have been 33 Atlantic hurricanes , and there were 10 in 1998 alone . Global <br /> warming may cause changes in storm frequency and the precipitation rates associated with <br /> storms . A modest 0 . 9 ° F (0 . 5 ° C ) increase in the mean global temperature will add 20 days to <br /> the annual hurricane season and increase the chances of a storm making landfall on the <br /> U . S . mainland by 33 % . The warmer ocean surface also will allow storms to increase in <br /> 4-22 <br />
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