Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ...
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Seasonality —Inundation of l<strong>and</strong> during a growing season can have a completely destructive<br />
effect on agricultural production, as severe in fact as a prolonged drought. If flood waters occur<br />
during cold weather <strong>and</strong> if they derive predominantly from snow-melt with possible ice flows,<br />
general discomfort <strong>and</strong> subsistency levels of affected communities are also considerably<br />
influenced. Seasonality in large floods is therefore an important influence on severity of flood<br />
hazard. 7<br />
Forecasting, Warning, <strong>and</strong> Monitoring Systems<br />
Forecasting<br />
The ability to forecast flooding is limited to the time during which changes in the hydrological<br />
conditions necessary for flooding to occur have begun to develop. The formulation of a forecast<br />
for flood conditions requires information on current hydrological conditions such as precipitation,<br />
river stage, water equivalent of snowpack, temperature, soil conditions over the entire drainage<br />
basin, as well as weather reports <strong>and</strong> forecasts.<br />
In small headwater regions a forecast of crest height <strong>and</strong> time of occurrence is all the<br />
information required to initiate effective adjustments; the relatively rapid rate of rise <strong>and</strong> fall<br />
makes the period of time above flood stage relatively short. In lower reaches of large river<br />
systems where rates of rise <strong>and</strong> fall are slower, it is important to forecast the time when various<br />
critical stages of flow will be reached over the rise <strong>and</strong> fall. Reliability of forecasts for large<br />
downstream river systems is generally higher than for headwater systems.<br />
Warning<br />
Warning time for peak or overbank conditions can range from a few minutes in cloudburst<br />
conditions to a few hours in small headwater drainages to several days in the lower reaches of<br />
large river systems. As with forecasting, the time <strong>and</strong> reliability of the warning increase with<br />
distance downstream where adequate knowledge of upstream conditions exists. (Additional<br />
discussion on warning is found under the section, <strong>Disaster</strong> Mitigation Strategies.)<br />
Clearly the amount of information required, the data collection network necessary for collecting<br />
the information, the technical expertise required for interpretation, <strong>and</strong> the communication<br />
system needed to present timely information to potential victims are services that many poor<br />
<strong>and</strong> developing nations find difficult to provide. The World Meteorological Organization of the<br />
United Nations, through its World Weather Watch <strong>and</strong> Global Data Processing System, hopes<br />
to coordinate efforts to improve forecasting. 8 This is especially important (<strong>and</strong> difficult) when<br />
conditions creating floods lie outside of the national boundaries of the downstream region.<br />
Remote Sensing Monitoring<br />
One of the most effective methods of monitoring floodplains is through remote sensing. Of the<br />
various techniques available L<strong>and</strong>sat is perhaps the most versatile. L<strong>and</strong>sat satellites (formally<br />
called Earth Resources Technology Satellites or ERTS) are used to map, inventory, <strong>and</strong> monitor<br />
earth features.<br />
The major sensing instrument in L<strong>and</strong>sat is a multispectral scanner that produces images of the<br />
earth in green, red, <strong>and</strong> two wavelengths of infrared radiation. The products are black-<strong>and</strong>white<br />
images, <strong>and</strong> images in digital form that can be processed by computers.