Aridification
From Wikipedia, the free encyclopedia
 |
Please help improve this article or section by expanding it. Further information might be found on the talk page or at requests for expansion. (January 2008) |
Aridification is the process of a region becoming increasingly dry. It refers to long term change rather than seasonal variation. It is often measured as the reduction of average soil moisture content. It can be caused by natural or anthropogenic means such as climate change, reduced precipitation, increased evaporation, lowering of water tables or changes in ground cover. Its major consequences include reduced agricultural production, soil degradation, ecosystem changes and decreased water catchment runoff.[1]
[edit] See also
- Climate change
- Climate change and agriculture
- Desertification
- Global warming
- Groundwater
- Soil moisture
- Water balance
- Water content
- Water cycle
[edit] References
- ^ GLASOD Classification of soil degradation
 |
This climatology/meteorology-related article is a stub. You can help Wikipedia by expanding it. |
