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Comprehensive Risk Assessment for Natural Hazards - Planat

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30<br />

(b) the public;and<br />

(c) those who may be in a position to implement mitigation<br />

measures.<br />

Ideally, the key organizations involved in disaster-relief<br />

ef<strong>for</strong>ts will have the maps displayed permanently on a wall,<br />

and will have studied the maps and instituted disaster planning.<br />

Ideally, the public, community leaders and<br />

government bodies will also study the maps and appreciate<br />

that prevention is worthwhile, and implement appropriate<br />

mitigation measures. Also, near full-scale disaster exercises<br />

may be conducted periodically to maintain the readiness of<br />

disaster relief and management organizations, and to keep<br />

the public aware of the potential hazard.<br />

3.11 RELATED PREPAREDNESS SCHEMES<br />

Three main ways are available to reduce future flood damage<br />

to buildings and their contents:<br />

(a) reduce the flood through physical means (dams, levees,<br />

re<strong>for</strong>estation);<br />

(b) build buildings to withstand flooding with minimal<br />

damage, <strong>for</strong> example, elevation of buildings above the<br />

flood level; and<br />

(c) restrict or prohibit development on flood-prone land.<br />

Realistic consideration of the costs and benefits of these<br />

options requires hazard assessment and at least a rough<br />

assessment of the risks. Lack of data <strong>for</strong> quantitative hazard<br />

and risk assessment,however,should not preclude taking<br />

steps to reduce future damages or disasters. Unconstrained<br />

growth in a flood-prone area can be a costly mistake.<br />

Certain types of advanced planning have the potential<br />

to reduce social, and in some cases, physical damage in the<br />

event of a flood:<br />

(a) public education and awareness;<br />

(b) flood <strong>for</strong>ecasting (prediction of flood levels hours or<br />

days in advance);<br />

(c) disaster response planning, including evacuation planning<br />

and preparation of emergency shelter and<br />

services.<br />

The value of public education and awareness cannot be<br />

overestimated. Experience has shown that many people tend<br />

to ignore flood warnings. Effective public education should<br />

warn of the existence of the hazard, provide in<strong>for</strong>mation<br />

about the nature of the hazard, and what individuals can do<br />

to protect their lives and possessions. For example, coastal<br />

residents should be aware that tsunamis are a series of waves<br />

that may occur over a six-hour period; it is not safe to go<br />

back after the first wave has passed. Motorists should be<br />

aware that, at least in certain developed countries, most<br />

people who die in flash floods do so in their cars; they<br />

should never drive into a flooded area.<br />

Flood <strong>for</strong>ecasts can be made using a variety of techniques<br />

ranging from simple approaches to complex<br />

procedures. The selection of the technique to be used is<br />

largely dependent on the needs of the community and the<br />

physical setting. One approach is to use mathematicallybased<br />

hydrological process models. Such models trans<strong>for</strong>m<br />

the most recent conditions (e.g., rainfall, soil moisture,<br />

snowpack state and water equivalence), upstream flow<br />

conditions, and <strong>for</strong>ecasted precipitation and temperatures<br />

into hydrological predictions of streamflow. In larger river<br />

systems, <strong>for</strong>ecasts could be made through use of mathematically-based<br />

hydraulic models, wherein existing conditions<br />

upstream are projected downstream based on the physical<br />

conditions of the river’s channels and the specific properties<br />

of the flood wave. In some cases a combination of models<br />

may be required. A common example results from tropical<br />

and extratropical storms wherein high winds can cause<br />

marine waters to rise above normal levels. These same<br />

storms can carry large amounts of rain inland, resulting in<br />

dramatically increased streamflow in river systems. In lowlying<br />

areas, where the slope of the river may be very low, the<br />

rising water level of the surge restricts the passage of freshwater,<br />

combining in effect to increase the consequences and<br />

gravity of the event. In such cases, flood <strong>for</strong>ecasting would<br />

comprise a combination of river-runoff process modelling,<br />

river hydraulic modelling and coastal surge modelling in<br />

order to provide projections of conditions at specific<br />

locations.<br />

The availability of a flood-<strong>for</strong>ecasting programme<br />

enhances the opportunity <strong>for</strong> taking protective action.<br />

Protective actions include evacuation, moving possessions<br />

to higher ground, moving hazardous materials to higher<br />

ground, building temporary levees with sandbags, filling in<br />

weak spots in existing levees, and mobilizing heavy equipment<br />

<strong>for</strong> construction of temporary preventative measures<br />

and <strong>for</strong> clearing flood debris.<br />

Hazard and risk in<strong>for</strong>mation can be used to design flood<strong>for</strong>ecasting<br />

systems that are more effective because they:<br />

(a) <strong>for</strong>ecast floods <strong>for</strong> the geographic areas with the greatest<br />

hazards and risks; and<br />

(b) are sensitive to the flow levels at which flood damage<br />

commences.<br />

Similarly, disaster planning should take into account the<br />

nature of the flood hazards. For example, the effect of flooding<br />

on roads and bridges should be taken into account when<br />

selecting shelter facilities, evacuation routes and supply routes.<br />

Because floods often contaminate water supplies, plans should<br />

be made to obtain a safe supply of drinking water.<br />

3.12 GLOSSARY OF TERMS<br />

Chapter 3 — Hydrological hazards<br />

* Definitions taken from (WMO/UNESCO, 1992)<br />

** Definition taken from (UNDHA, 1992)<br />

*** Definitions taken from (WMO, 1992)<br />

Annual peak: The largest instantaneous flow rate in a given<br />

year at a given river location.<br />

<strong>Assessment</strong>:** Survey of real or potential disaster to estimate<br />

the actual or expected damages and to make recommendations<br />

<strong>for</strong> prevention, preparedness and response.<br />

Bathymetry: Underwater or submarine topography.<br />

Depth-duration-frequency curve:*** Curve showing the relation<br />

between the depth of precipitation and the<br />

frequency of occurrence of different duration periods.<br />

Disaster:* A serious disruption of the functioning of society,<br />

casing widespread human, material or environmental<br />

losses which exceed the ability of the affected society to<br />

cope using only its own resources.

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