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A spatial multi-risk hazard assessment and vulnerability study of ...

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worth <strong>of</strong> property are at <strong>risk</strong> <strong>of</strong> flooding in the United States. Thous<strong>and</strong>s <strong>of</strong> floods occur<br />

worldwide each year, making it one <strong>of</strong> the most common <strong>and</strong> damaging <strong>of</strong> all <strong>hazard</strong>s<br />

(Federal Emergency Management Agency, 1997).<br />

A flood is a normal event for any river or stream that could occur over a period <strong>of</strong> time<br />

varying from several times a year to once every few hundred years. Floods are caused<br />

when excess water from heavy rainfall, snowmelt or storm surge accumulates <strong>and</strong><br />

overflows the river or stream’s normal path onto its banks <strong>and</strong> adjacent floodplains<br />

(Miller, 1997).<br />

Floodplains are lowl<strong>and</strong>s adjacent to rivers, streams, lakes <strong>and</strong> oceans that are subject to<br />

recurring floods. Floods can occur anywhere in a country, any time <strong>of</strong> the year, day or<br />

night. The potential volume <strong>of</strong> water that could reach the floodplain is a function <strong>of</strong> the<br />

size <strong>of</strong> the contributing watershed <strong>and</strong> topographic characteristics such as watershed<br />

slope <strong>and</strong> shape, <strong>and</strong> climatic <strong>and</strong> l<strong>and</strong> use characteristics (Coch, 1992).<br />

Several factors determine the severity <strong>of</strong> floods, including rainfall intensity <strong>and</strong> duration.<br />

A large amount <strong>of</strong> rainfall in a short time span can cause flash flooding. A small amount<br />

<strong>of</strong> rain can also cause flooding if the soil is saturated from a previous wet period, or if the<br />

rain is concentrated in areas where the surface is impermeable, such as in developed areas<br />

where most <strong>of</strong> the surface is covered with concrete, tar <strong>and</strong> other building materials<br />

(Federal Emergency Management Agency, 1997).<br />

Topography <strong>and</strong> groundcover are also contributing factors for floods. Water run<strong>of</strong>f is<br />

higher in areas with a steep slope <strong>and</strong> low vegetation density. Urbanization <strong>of</strong> floodplains<br />

<strong>and</strong> manipulation <strong>of</strong> stream channels have increased both the frequency <strong>and</strong> magnitude<br />

<strong>of</strong> floods in many areas. Floods are most common in the season <strong>of</strong> highest precipitation<br />

(Miller, 1997).<br />

The intensity <strong>of</strong> floods in South Africa is measured in cubic metres per second, <strong>and</strong> the<br />

<strong>risk</strong> <strong>of</strong> flooding is defined as the probability <strong>of</strong> occurrence in a year in percentage or<br />

return period (years). Therefore a 50 year flood has a 2% (1/50x100) chance <strong>of</strong> occurring<br />

in any specific year. The probability <strong>of</strong> a 50 year flood occurring once in a 50 year time<br />

span is thus calculated at 66% (RAVA, 2002).<br />

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