Drought
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A Drought is a climate-related event with reduced rainfall that leads to ecosystem shrinkage.
- Context:
- It can range from being a Short-Term Drought to being a Long-Term Drought.
- It can range from being a Localized Drought to being a Regional Drought.
- …
- Example(s):
- California Drought 1895-.
- the Yucatan Peninsula droughts of ~810, ~860, and ~910 A.D.
- …
- Counter-Example(s):
- See: Surface Water, Ground Water, Precipitation, Ecosystem, Agriculture, Timeseries Prediction.
References
2014
- (Wikipedia, 2014) ⇒ http://en.wikipedia.org/wiki/drought Retrieved:2014-12-29.
- Drought is an extended period when a region receives a deficiency in its water supply, whether atmospheric, surface or ground water. A drought can last for months or years, or may be declared after as few as 15 days. [1] 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 [2] and harm to the local economy. [3] Prolonged droughts have caused mass migrations and humanitarian crises. Many plant species, such as those in the family Cactaceae or 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. [4] Most arid ecosystems have inherently low productivity.
- ↑ It's a scorcher - and Ireland is officially 'in drought' Irish Independent, 2013-07-18.
- ↑ Living With Drought
- ↑ Australian Drought and Climate Change, retrieved on June 7th 2007.
- ↑ Keddy, P.A. 2007. Plants and Vegetation: Origins, Processes, Consequences. Cambridge University Press, Cambridge, UK. 666 p.
2006
- Emilio F. Moran, Ryan Adams, Bryn Bakoyéma, Stefano Fiorini, and Bruce Boucek. (2006). “Human Strategies for Coping with El Niño Related Drought in Amazônia.” In: Climatic Change, 77.
2003
- (Haug et al., 2003) ⇒ Gerald H. Haug, Detlef Günther, Larry C. Peterson, Daniel M. Sigman, Konrad A. Hughen, and Beat Aeschlimann. (2003). “Climate and the Collapse of Maya Civilization." Science, 299(5613). doi:10.1126/science.1080444