Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ... Natural Hazards: Causes and Effects - Disaster Management Center ...
1. Environmental Effects Drought Disaster Overview Effects Consequences Reduced cloud cover; increased daytime Dramatic reduction of surface water; severe crop temperatures;increased evaporation rates losses; soil erosion Increasing likelihood of dust and sandstorms Food shortages; increased hunger and malnutrition Losses to livestock Population shifts and migration 2. Patterns of Injury and Surgical Needs in Disasters Few or no surgical needs. 3. Patterns of Disease Resulting from Disasters Actual Immediate Epidemiological Threat Secondary Epidemiological Threat Malnutrition Malnutrition increases susceptibility to all diseases, but particularly measles, diarrhea. 4. Immediate Social and Economic Consequences of Disasters Short-term migrations Long-term migration Loss of crops 5. Effects of Natural Hazards On Land Structures Agriculture Trees Dry soils No major damage Kills crops Kills some trees Windstorms Minor damage Erodes topsoil Minor damage Desertification No major damage Covers farmland Kills trees, increases with sand shrub growth 6. Response to Disasters (Ideal) Initial Response: By Local Authorities By Foreign Intervenors Medical, nutritional services, water (on site if Medical, nutritional services, water (on site if possible); epidemiological surveillance possible); epidemiological surveillance Secondary Response: Re-establishment of agricultural sector (loans, Re-establishment of agricultural sector (loans, seeds, farm equipment, animals); seeds, farm equipment, animals); technical assistance, nutritional surveillance technical assistance, nutritional surveillance 7. Appropriate Aid cash immunizations short- and long-term food aid (normal foods) intensive feeding medical supplies loans or credit agricultural assistance
Chapter 8 Desertification Introduction and Definition Although deserts are not without life, they can be viewed as areas with extremely limited agricultural potential. Deserts occur in a variety of types, hot and cold, stony and sandy, but all are characterized by rainfall deficiencies so marked that cultivation or stock-rearing are possible only with special adaptations, as, for example, by the development of irrigation. Desertification, as the extension or intensification of desert conditions, involves a decline in the productivity of the land. Desertification, especially in developing countries, worsens conditions of poverty, brings malnutrition and disease, erodes the basis of the national economy and then brings deterioration of social services already hampered by remoteness and lack of funds. All this affects the ability of dryland communities to respond to succeeding droughts, each of which would then tend to advance further the deterioration of living standards, which represents the human aspect of desertification. Desertification, as part of the cycle of agriculturally good and bad years, is a slow-onset disaster. Signs of its approach are in evidence well before the situation becomes catastrophic. Desertification arises from the interaction between a difficult, unreliable and sensitive dryland environment and the human use and occupation of it in an effort to make a living. For this reason people who live in susceptible areas must learn how to live and work in harmony with the constant threat of desertification. If desertification were allowed to develop uncontrolled, almost the entire population of the earth’s drylands could be said to face eventual risk. These drylands contain between 600 and 700 million people, and in terms of broad areas and livelihood systems their numbers are as shown in Table 8.1. 1 The number of people immediately threatened, their general location and livelihood systems, are shown in Table 8.2. 2 Of the 78 million people threatened, about a third may be in a position, because of high income or other advantages, to avoid the worst consequences of desertification. This still leaves about 50 million people who are immediately menaced through the destruction of their livelihoods. These people face the grim prospect of uprooting themselves from everything familiar and migrating to other areas frequently ill-equipped to receive them. Historical Examples The Sahara In Arabic sahra means “desert.” Sahara is plural. Indeed, the Sahara is not one but many deserts. It contains half the desert surface of the world. In the past 65 million years the borders of the Sahara have expanded and retreated many times. Oak and cedar trees once grew in the Saharan highlands, and rock paintings portray abundant wildlife. But about 3000 B.C. the current drying trend began setting in, and humans, relative newcomers to north Africa, had to contend with desertification of the worst degree.
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Chapter 8<br />
Desertification<br />
Introduction <strong>and</strong> Definition<br />
Although deserts are not without life, they can be viewed as areas with extremely limited<br />
agricultural potential. Deserts occur in a variety of types, hot <strong>and</strong> cold, stony <strong>and</strong> s<strong>and</strong>y, but all<br />
are characterized by rainfall deficiencies so marked that cultivation or stock-rearing are possible<br />
only with special adaptations, as, for example, by the development of irrigation. Desertification,<br />
as the extension or intensification of desert conditions, involves a decline in the productivity of<br />
the l<strong>and</strong>. Desertification, especially in developing countries, worsens conditions of poverty,<br />
brings malnutrition <strong>and</strong> disease, erodes the basis of the national economy <strong>and</strong> then brings<br />
deterioration of social services already hampered by remoteness <strong>and</strong> lack of funds. All this<br />
affects the ability of dryl<strong>and</strong> communities to respond to succeeding droughts, each of which<br />
would then tend to advance further the deterioration of living st<strong>and</strong>ards, which represents the<br />
human aspect of desertification.<br />
Desertification, as part of the cycle of agriculturally good <strong>and</strong> bad years, is a slow-onset<br />
disaster. Signs of its approach are in evidence well before the situation becomes catastrophic.<br />
Desertification arises from the interaction between a difficult, unreliable <strong>and</strong> sensitive dryl<strong>and</strong><br />
environment <strong>and</strong> the human use <strong>and</strong> occupation of it in an effort to make a living. For this<br />
reason people who live in susceptible areas must learn how to live <strong>and</strong> work in harmony with<br />
the constant threat of desertification.<br />
If desertification were allowed to develop uncontrolled, almost the entire population of the<br />
earth’s dryl<strong>and</strong>s could be said to face eventual risk. These dryl<strong>and</strong>s contain between 600 <strong>and</strong><br />
700 million people, <strong>and</strong> in terms of broad areas <strong>and</strong> livelihood systems their numbers are as<br />
shown in Table 8.1. 1<br />
The number of people immediately threatened, their general location <strong>and</strong> livelihood systems,<br />
are shown in Table 8.2. 2 Of the 78 million people threatened, about a third may be in a position,<br />
because of high income or other advantages, to avoid the worst consequences of<br />
desertification. This still leaves about 50 million people who are immediately menaced through<br />
the destruction of their livelihoods. These people face the grim prospect of uprooting<br />
themselves from everything familiar <strong>and</strong> migrating to other areas frequently ill-equipped to<br />
receive them.<br />
Historical Examples<br />
The Sahara<br />
In Arabic sahra means “desert.” Sahara is plural. Indeed, the Sahara is not one but many<br />
deserts. It contains half the desert surface of the world.<br />
In the past 65 million years the borders of the Sahara have exp<strong>and</strong>ed <strong>and</strong> retreated many times.<br />
Oak <strong>and</strong> cedar trees once grew in the Saharan highl<strong>and</strong>s, <strong>and</strong> rock paintings portray abundant<br />
wildlife. But about 3000 B.C. the current drying trend began setting in, <strong>and</strong> humans, relative<br />
newcomers to north Africa, had to contend with desertification of the worst degree.