My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD03837
CWCB
>
Floodplain Documents
>
Backfile
>
3001-4000
>
FLOOD03837
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 6:44:29 PM
Creation date
10/5/2006 12:06:09 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
Confronting Natural Disasters
Date
11/2/1987
Prepared By
Natural Resource Council
Floodplain - Doc Type
Educational/Technical/Reference Information
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
72
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br /> <br />they are not typified by a rapid onset. Instead, <br />these hazards are relatively slow in their onset but <br />prolonged in their impact. Droughts, famines, <br />epidemics, and desertification are well-known <br />long-term disasters. <br />Drought may be defined as any unusual pro- <br />longed dry period. Though generally associated <br />with semiarid or desert climates, they also occur <br />in areas that normally enjoy adequate rainfall. <br />Droughts are usually accompanied by dry, hot <br />winds, and they may be terminated by violent <br />storms. <br />The basic causes of drought are still not clear. It <br />is generally believed that droughts are a con- <br />sequence of changing global weather patterns <br />triggered by such ecological events as solar radia- <br />tion, excessive build-up of heat on the earth's <br />surface, and increased particulate matter in the <br />earth's atmosphere. Droughts are accompanied <br />by reduced cloud cover, thus increasing exposure <br />of the land to solar radiation. The result - <br />increased transpiration and evaporation rates - <br />tends to perpetuate the drought. Once estab- <br />lished, these conditions are difficult to reverse. <br />Human activities also contribute to develop- <br />ment of drought conditions. Overgrazing, poor <br />cropping methods, deforestation, and improper <br />soil conservation techniques often help to create a <br />drought. <br />Desertification is a secondary effect of drought. <br />Technically, desertification occurs when the soil <br />reaches a given level of dryness. Simply stated, <br />desertification occurs when land takes on the <br />characteristics of a desert. It can mean the <br />encroachment of sand dunes and the loss of most <br />vegetation or replacement of normal vegetation <br />with desert scrub bushes and other plants espe- <br />cially adapted to the desert environment. In either <br />case, the land is rendered useless without large- <br />scale and costly reclamation measures. <br /> <br />51 <br /> <br />Fighting desertification is both costly and frus- <br />trating. Few developing countries have the re- <br />sources necessary to stop this process once it takes <br />hold, and reclamation successes have been rather <br />limited. The best way to stop desertification is to <br />prevent its initiation, and the best way to accom- <br />plish this is through measures that address wide- <br />spread economic and agricultural development. <br />Reducing the hazards of drought and des- <br />ertification requires a balanced program that <br />develops good water resources, addresses the <br />problems of soil erosion, and adopts realistic <br />limits on the expansion of animal herds, or <br />accompanies the expansion of herds with compre- <br />hensive range management. Agricultural im- <br />provements to prevent these hazards include <br />modifying cropping patterns and introducing <br />drought-resistant crop varieties; rangeland man- <br />agement includes improvement of grazing lands <br />and grazing patterns, introduction of feedlots, and <br />protection of shrubs and trees. <br />Expansive soils - soils that exhibit large poten- <br />tial for shrinking and swelling with changes in <br />moisture content - are another long-term hazard. <br />Construction on these soils is extremely vulnera- <br />ble to damage - even total destruction - as the <br />ground surface elevation changes in response to <br />seasonal fluctuations and rainfall. The problem is <br />particularly acute in arid and semiarid regions. <br />Shrinking and swelling soils are found in indus- <br />trialized and developing nations alike. The total <br />cost of damage associated with expansive soils is <br />estimated at a minimum of $6 billion per year in <br />the United States alone; it is the nation's most <br />costly natural hazard. Extremely high costs are <br />likely to be typical for many other nations as well. <br />Though mitigation measures involving land use <br />and building design are well known, they are often <br />not applied due to ignorance, cost, and lack of <br />enforcement. <br />
The URL can be used to link to this page
Your browser does not support the video tag.