Droughts John Rundle GEL 131 WQ2014

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Presentation transcript:

Droughts John Rundle GEL 131 WQ2014 Lecture 27 Droughts John Rundle GEL 131 WQ2014

Global Drought Statistics http://www. preventionweb Persons Affected Economic Damage (USD in B$) Persons Killed Number of Reported Events

Global Drought Summary Statistics http://www. preventionweb

Drought http://en.wikipedia.org/wiki/Drought Drought is an extended period when a region notes a deficiency in its water supply whether surface or underground water. A drought can last for months or years, or may be declared after as few as 15 days. Generally, this occurs when a region receives consistently below average precipitation. It can have a substantial impact on the ecosystem and agriculture of the affected region. Although droughts can persist for several years, even a short, intense drought can cause significant damage and harm to the local economy. Many plant species, such as cacti, have adaptations such as reduced leaf area and waxy cuticles to enhance their ability to tolerate drought. Some others survive dry periods as buried seeds. Semi-permanent drought produces arid biomes such as deserts and grasslands. Most arid ecosystems have inherently low productivity Drought http://en.wikipedia.org/wiki/Drought Sonoran desert, Mexico

Drought http://en.wikipedia.org/wiki/Drought This global phenomenon has a widespread impact on agriculture. Lengthy periods of drought have long been a key trigger for mass migration and played a key role in a number of ongoing migrations and other humanitarian crises in the Horn of Africa and the Sahel.  According to F. Bagouls and Henri Gaussen's definition, a month (or other period) is considered dry when the mean monthly precipitation in millimeters is equal to or lower than twice the mean monthly temperature in °C. Dust bowl days, South Dakota, 1936

Consequences http://en.wikipedia.org/wiki/Drought Periods of droughts can have significant environmental, agricultural, health, economic and social consequences. The effect varies according to vulnerability. For example, subsistence farmers are more likely to migrate during drought because they do not have alternative food sources. Areas with populations that depend on as a major food source are more vulnerable to famine. Drought can also reduce water quality, because lower water flows reduce dilution of pollutants and increase contamination of remaining water sources. Common consequences of drought include: Diminished crop growth or yield productions and carrying capacity for livestock Dust bowls, themselves a sign of erosion, which further erode the landscape Dust storms, when drought hits an area suffering from desertification and erosion Famine due to lack of water for irrigation Habitat damage, affecting both terrestrial and aquatic wildlife[5] Hunger, drought provides too little water to support food crops. Malnutrition, dehydration and related diseases Mass migration, resulting in internal displacement and international refugees Reduced electricity production due to reduced water flow through hydroelectric dams[6] Shortages of water for industrial users[7][8] Snake migration, which results in snakebites[9] Social unrest War over natural resources, including water and food Wildfires, such as Australian bushfires, are more common during times of drought.[10]

Causes http://en.wikipedia.org/wiki/Drought Generally, rainfall is related to the amount and dew point [determined by air temperature] of water vapor carried by regional atmosphere, combined with the upward forcing of the air mass containing that water vapor. If these combined factors do not support precipitation volumes sufficient to reach the surface, the result is a drought. This can be triggered by high level of reflected sunlight, [high albedo], and above average prevalence of high pressure systems, winds carrying continental, rather than oceanic air masses (i.e. reduced water content), and ridges of high pressure areas from behaviors which prevent or restrict the developing of thunderstorm activity or rainfall over one certain region. Oceanic and atmospheric weather cycles such as the El Niño-Southern Oscillation (ENSO) make drought a regular recurring feature of the Americas along the Midwest and Australia. Causes http://en.wikipedia.org/wiki/Drought Drought in Karnataka India, 2012

Causes http://en.wikipedia.org/wiki/Drought Guns, Germs, and Steel author Jared Diamond sees the stark impact of the multi-year ENSO cycles on Australian weather patterns as a key reason that Australian aborigines remained a hunter-gatherer society rather than adopting agriculture.[35] Another climate oscillation known as the North Atlantic Oscillation has been tied to droughts in northeast Spain. Human activity can directly trigger exacerbating factors such as over farming, excessive irrigation, deforestation, and erosion adversely impact the ability of the land to capture and hold water. While these tend to be relatively isolated in their scope, activities resulting in global climate change are expected to trigger droughts with a substantial impact on agriculture throughout the world, and especially in developing nations. Overall, global warming will result in increased world rainfall. Along with drought in some areas, flooding and erosion will increase in others. Paradoxically, some proposed solutions to global warming that focus on more active techniques, solar radiation management through the use of a space sunshade for one, may also carry with them increased chances of drought

Classification of Droughts http://en.wikipedia.org/wiki/Drought As a drought persists, the conditions surrounding it gradually worsen and its impact on the local population gradually increases. Droughts can be defined in three main ways: Meteorological drought is brought about when there is a prolonged period with less than average precipitation. Meteorological drought usually precedes the other kinds of drought. Agricultural droughts are droughts that affect crop production or the ecology of the range. This condition can also arise independently from any change in precipitation levels when soil conditions and erosion triggered by poorly planned agricultural endeavors cause a shortfall in water available to the crops. However, in a traditional drought, it is caused by an extended period of below average precipitation. Hydrological drought is brought about when the water reserves available in sources such as aquifers, lakes and reservoirs fall below the statistical average. Hydrological drought tends to show up more slowly because it involves stored water that is used but not replenished

Protection and Relief http://en.wikipedia.org/wiki/Drought Strategies for drought protection, mitigation or relief include: Dams - many dams and their associated reservoirs supply additional water in times of drought. Cloud seeding - a form of intentional weather modification to induce rainfall.[48] Desalination - of sea water for irrigation or consumption. Drought monitoring - Continuous observation of rainfall levels and comparisons with current usage levels can help prevent man-made drought. For instance, analysis of water usage in Yemen has revealed that their water table (underground water level) is put at grave risk by over-use to fertilize their Khat crop.[49] Careful monitoring of moisture levels can also help predict increased risk for wildfires, using such metrics as the Keetch-Byram Drought Index[10] or Palmer Drought Index. Land use - Carefully planned crop rotation can help to minimize erosion and allow farmers to plant less water-dependent crops in drier years. Outdoor water-use restriction - Regulating the use of sprinklers, hoses or buckets on outdoor plants, filling pools, and other water-intensive home maintenance tasks. Rainwater harvesting - Collection and storage of rainwater from roofs or other suitable catchments. Recycled water - Former wastewater (sewage) that has been treated and purified for reuse. Transvasement - Building canals or redirecting rivers as massive attempts at irrigation in drought-prone areas.