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2005-070
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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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1993 ) . Humid conditions , which add to the discomfort of high temperatures , o N.cur when an <br /> area of high atmospheric pressure traps hazy , damp air near the ground . <br /> Human bodies dissipate heat in one of three ways : by varying the rate and depth <br /> of blood circulation ; by losing water through the skin and sweat glands ; and by panting . As <br /> the blood is heated to above 98 . 60 , the heart begins to pump more blood , blood vessels <br /> dilate to accommodate the increased flow , and the bundles of tiny capillaries penetrating <br /> through the upper layers of skin are put into operation . The body' s blood is circulated closer <br /> to the surface , and excess heat is released into the cooler atmosphere . At the same time , <br /> water diffuses through the skin as perspiration . The skin handles about 90 % of the body's <br /> heat dissipating function . <br /> Heat disorders generally have to do with a reduction or collapse of the body' s <br /> ability to cool itself by circulatory changes and sweating , or a chemical (salt) imbalance <br /> caused by too much sweating . When the body cannot cool itself, or when it cannot <br /> compensate for fluids and salt lost through perspiration , the temperature of the body's inner <br /> core begins to rise and heat- related illness may develop . Studies indicate that, other things <br /> being equal , the severity of heat disorders tend to increase with age . Heat cramps in a <br /> 17-year old may be heat exhaustion in a 40-year old , and heat stroke in a person over 60 . <br /> When the temperature gets extremely high , the NWS has increased its efforts to <br /> alert the general public as well as the appropriate authorities by issuing speci I weather <br /> statements . Residents should heed these warnings to prevent heat- related medical <br /> complications . As a result of the latest research findings , the NWS has devised the " Heat <br /> Index" ( HI ) . The HI , given in degrees Fahrenheit, is an accurate measure of t ow hot it really <br /> feels when relative humidity is added to the actual air temperature . The NW will initiate <br /> alert procedures when the HI is expected to exceed 105 ° F for at least two cor secutive days . <br /> Possible heat disorders related to the corresponding HI are listed below . <br /> • Heat Index of 130 ° F or higher — Heatstroke/sunstroke with exposure for <br /> people in higher risk groups ; <br /> • Heat Index of 105 ° F- 130 ° F — Sunstroke , heat cramps , and heat exhaustion <br /> likely and heatstroke possible with prolonged physical activity; <br /> • Heat Index of 90 ° F- 105 ° F — Sunstroke , heat cramps with prolonged exposure ; <br /> and <br /> • Heat Index of 80 ° F-90 ° F — Fatigue possible with prolonged exposure and <br /> physical activity ( NWS , 1999b ) . <br /> Historic Events. The highest temperature ever recorded in the state was on <br /> 29 June 1931 at 103 ° F in Monticello at an elevation of 207 feet ( NCDC , 1999 :) ) . In a normal <br /> year, approximately 175 Americans die from extreme heat . However, in 199 .5 , the death toll <br /> was 1 , 021 ( NWS , 1997 ) . There were no data available to document previous occurrences of <br /> extreme heat by jurisdiction . <br /> Because temperature extremes are hazards that are not bounded by geographic <br /> or topographic characteristics , there are no definite means to determine whetrier or not the <br /> extent of this hazard differs from jurisdiction to jurisdiction within Indian River County . <br /> *400 <br /> 4-42 <br />
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