My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2016-069V
CBCC
>
Official Documents
>
2010's
>
2016
>
2016-069V
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
10/9/2016 1:13:21 AM
Creation date
7/25/2016 12:18:14 PM
Metadata
Fields
Template:
Official Documents
Official Document Type
Plan
Approved Date
05/17/2016
Control Number
2016-069V
Agenda Item Number
8.B.
Entity Name
Emergency Services
Subject
Basic Plan 2016-2020 Comprehensive Emergency Management Plan
Document Relationships
2016-044
(Attachments)
Path:
\Resolutions\2010's\2016
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
186
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
more intense the hurricane is, the sooner the surge arrives. <br /> Water rise can be very rapid, posing a serious threat to those <br /> who have waited to evacuate flood prone areas. A storm <br /> surge is a wave that has outrun its generating source and <br /> become a long period swell. The surge is always highest in <br /> the right-front quadrant of the direction the hurricane is moving <br /> in. As the storm approaches shore, the greatest storm surge <br /> will be to the north of the hurricane eye. <br /> Such a surge of high water topped by waves driven by <br /> hurricane force winds can be devastating to coastal regions. <br /> The stronger the hurricane and the shallower the offshore <br /> water, the higher the surge will be. In addition, if the storm <br /> surge arrives at the same time as the high tide, the water <br /> height will be even greater. The storm tide is the combination <br /> of the storm surge and the normal astronomical tide. <br /> Damage during hurricanes also may result from possible <br /> spawned tornadoes, and inland flooding associated with heavy <br /> rainfall that usually accompany these storms. Hurricane <br /> Andrew, a relatively "dry" hurricane, dumped 10 inches of rain <br /> on south Florida and left many buildings extensively water <br /> damaged. Rainwater may seep into gaps in roof sheathing <br /> and saturate insulation and ceiling drywall, in some cases <br /> causing ceilings to collapse. <br /> Crop damage is another powerful effect of hurricanes and <br /> tropical storms. Tropical Storm Mitch in 1998 dropped as much <br /> as 10 inches of rain in some south Florida areas, which <br /> resulted in approximately $20 million in crop damage in Palm <br /> Beach County alone (Associated Press, 1998). According to <br /> the University of Florida (2001), of Indian River County's <br /> 322,112 acres, 168,399 acres are farmland. With 52% of its <br /> land area being farmed, Indian River County is particularly <br /> vulnerable to crop damage resulting from the wind and rain <br /> from hurricanes and tropical storms. Hurricanes Charley, <br /> Frances, and Jeanne crossed citrus-producing counties in <br /> Florida in 2004, followed by Hurricane Wilma in 2005. <br /> Hurricanes Frances and Jeanne affected the Treasure Coast <br /> directly, making landfall three weeks apart in Martin County. A <br /> special census to measure the losses was conducted in mid- <br /> 2005 in the four counties of Indian River, Martin, Palm Beach, <br /> and St. Lucie. Because of these hurricanes, Indian River and <br /> St. Lucie Counties only produced 36% of the state's grapefruit <br /> Indian River County Comprehensive Emergency Management Plan Basic Page 16 <br />
The URL can be used to link to this page
Your browser does not support the video tag.