Comprehensive Risk Assessment for Natural Hazards - Planat
Comprehensive Risk Assessment for Natural Hazards - Planat
Comprehensive Risk Assessment for Natural Hazards - Planat
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(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.