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| | = Effects of Climate Change<br/> = | | = Effects of Climate Change<br/> = |
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| − | == Precipitation ==
| + | [[Climate_Change_and_Agriculture|Climate change]] however adds a number of new aspects to the quantity and availability of water. There has been scientific discourse about an intensification of the [[influence_on_the_water_cycle|water cycle]], but empirical evidence does not consistently support the idea.<ref>Huntington, T. G. (2005). Evidence for intensification of the global water cycle:Review and synthesis. Journal of Hydrology 319 (2006) 83–95. http://www.ic.ucsc.edu/~mdmccar/ocea213/readings/discuss_1_Oki_Huntington/Huntington_2006_JHydrol_Evidence_intensification_Hydrologic_cycle.pdf [03 June 2013]</ref> |
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| − | Climate Change results in a change of precipitation patterns that differ substantially from region to region. It is likely that rainfall increases in high latitudes and the tropics. This is related to an increase in the average river runoff. Subtropic and low-latitude regions (esp.the Mediterranean basin, western USA, southern Africa and north-eastern Brazil) will experience less precipitation. Heavy storms have been happening more frequently.<ref name="ipcc 2008">Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref> It has been widely noticed that dry regions tend to dry out, while wet regions become even wetter.<ref name="water climate change">s</ref> | + | == Precipitation<br/> == |
| | + | |
| | + | Climate Change results in a change of precipitation patterns that differ substantially from region to region. It is likely that rainfall increases in high latitudes and the tropics. This is related to an increase in the average river runoff. Subtropic and low-latitude regions (esp.the Mediterranean basin, western USA, southern Africa and north-eastern Brazil) will experience less precipitation. Heavy storms have been happening more frequently.<ref name="ipcc 2008">Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref> It has been widely noticed that dry regions tend to dry out, while wet regions become even wetter.<ref name="water climate change">s</ref><br/> |
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| | + | == Atmosphere == |
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| | + | It is by now common knowledge that increased anthropogenic[[gas_emissions|emissions of green house gases]] result in rising [[Temperature|temperatures]]. Warmer air in the atmosphere can hold more evaporated water.<br/> |
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| | == Soils == | | == Soils == |
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| | Furthermore, soil moisture affected. Back in the 1970ies half of the area that is today classified as very dry was fertile.<ref name="ipcc 2008">Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref> | | Furthermore, soil moisture affected. Back in the 1970ies half of the area that is today classified as very dry was fertile.<ref name="ipcc 2008">Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref> |
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| − | == Ice melting == | + | == Melting Ice == |
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| | Climate change substantially contributed to the melting of mountain glaciers as well as the ice at the poles. The availability of water in regions that are traditionally supplied by glacier water is lowered, affecting the lives of about 15 % of the world population. Also, seasonal differences in water supply are affected: The ratio of winter to annual water flow is lower, too. <ref name="ipcc 2008">Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref><br/> | | Climate change substantially contributed to the melting of mountain glaciers as well as the ice at the poles. The availability of water in regions that are traditionally supplied by glacier water is lowered, affecting the lives of about 15 % of the world population. Also, seasonal differences in water supply are affected: The ratio of winter to annual water flow is lower, too. <ref name="ipcc 2008">Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref><br/> |
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| | = Further Remarks = | | = Further Remarks = |
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| − | The changes in water quantity that climate change brings about are very likely to negatively affect food security and public health. Additionally the existing water infrastructure (power plants, flood defences, drainage, and irrigation systems) will face major challenges when dealing with the expected quality and quantity of water. Climate Change will further aggravate the current issues with regard to urbanisation, land management, population growth, economic intensification. The water management systems applied today don't sufficiently prepare for the upcoming changes. <ref>Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref> | + | The changes in water quantity that climate change brings about are very likely to negatively affect [[Definition_and_Dimensions_of_Food_Security|food security]] and public health. Additionally the existing water [[Infrastructure|infrastructure]] (power plants, [[Flood_protection|flood defences]], [[Drainage_and_irrigation|drainage]], and [[Design_for_irrigation|irrigation systems]]) will face major challenges when dealing with the expected [[Quality|quality]] and quantity of water. Climate change will further aggravate the current issues with regard to urbanisation, [[Land_use_planning|land management]], population growth and economic intensification. The [[IWRM|water management systems]] applied today don't sufficiently prepare for the upcoming changes. <ref>Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]</ref> |
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| | = References = | | = References = |
| | | | |
| | <references /><br/> | | <references /><br/> |
Revision as of 10:05, 3 June 2013
Climate change is already and will continue to affect the availability of water.
Background
There are five primary categories: [1]
- oceans (96.5 %)
- liquid freshwater (frozen freshwater in glacier and permafrost, 2 %)
- non-seasonal frozen water (depends on season)
- groundwater (1.6 %) and
- water vapor, lakes and rivers (< 1 %).
The amount of water, neither absolute nor relative, is not constant. Scientists believe that hydrogen is lost into space, leaving less H for H2O on earth. Water of course also moves between the different categories. Generally, the earth has become drier over the last 10.000 years.[2]
Effects of Climate Change
Climate change however adds a number of new aspects to the quantity and availability of water. There has been scientific discourse about an intensification of the water cycle, but empirical evidence does not consistently support the idea.[3]
Precipitation
Climate Change results in a change of precipitation patterns that differ substantially from region to region. It is likely that rainfall increases in high latitudes and the tropics. This is related to an increase in the average river runoff. Subtropic and low-latitude regions (esp.the Mediterranean basin, western USA, southern Africa and north-eastern Brazil) will experience less precipitation. Heavy storms have been happening more frequently.[4] It has been widely noticed that dry regions tend to dry out, while wet regions become even wetter.[1]
Atmosphere
It is by now common knowledge that increased anthropogenicemissions of green house gases result in rising temperatures. Warmer air in the atmosphere can hold more evaporated water.
Soils
Furthermore, soil moisture affected. Back in the 1970ies half of the area that is today classified as very dry was fertile.[4]
Melting Ice
Climate change substantially contributed to the melting of mountain glaciers as well as the ice at the poles. The availability of water in regions that are traditionally supplied by glacier water is lowered, affecting the lives of about 15 % of the world population. Also, seasonal differences in water supply are affected: The ratio of winter to annual water flow is lower, too. [4]
The changes in water quantity that climate change brings about are very likely to negatively affect food security and public health. Additionally the existing water infrastructure (power plants, flood defences, drainage, and irrigation systems) will face major challenges when dealing with the expected quality and quantity of water. Climate change will further aggravate the current issues with regard to urbanisation, land management, population growth and economic intensification. The water management systems applied today don't sufficiently prepare for the upcoming changes. [5]
References
- ↑ 1.0 1.1 Peter H. Gleick (editor), 1993, Water in Crisis: A Guide to the World's Fresh Water Resources (Oxford University Press, New York).
- ↑ Pielou, E. C. (2008). After the Ice Age. Chicago: University of Chicago Press.
- ↑ Huntington, T. G. (2005). Evidence for intensification of the global water cycle:Review and synthesis. Journal of Hydrology 319 (2006) 83–95. http://www.ic.ucsc.edu/~mdmccar/ocea213/readings/discuss_1_Oki_Huntington/Huntington_2006_JHydrol_Evidence_intensification_Hydrologic_cycle.pdf [03 June 2013]
- ↑ 4.0 4.1 4.2 Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]
- ↑ Intergovernmental Panel on Climate Change (2008): Technical Paper on Climate Change and Water. Finalized at the 37th Session of the IPCC Bureau. http://www.ipcc.ch/meetings/session28/doc13.pdf [accessed 31 May 2013]
