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Water availability

July 23, 2010

From The UK

The impacts for the availability of water were generated from work from a variety of sources. These include the Intergovernmental Panel on Climate Change Working Group 2 report, Impacts, adaptation and vulnerability, 2007, published research and research done by the Walker Institute for Climate System Research, University of Reading.


In addition the IPCC WG2 report has collated a great deal of research about the availability of water, and this resource was used to support statements about glacier melt and the contribution of different water sources. 

Finally, specific research was done by Prof. Nigel Arnell at the Walker Institute for Climate System Research, University of Reading, looking at the affect of an increase of global average temperature of +4 ºC, on the run off and water availability. A description of this research is given below.

Climate change and water resources: Walker Institute for Climate System Research, University of Reading

A rise in global temperature of 4oC would have a substantial effect on river flows and the availability of water resources. Average runoff decreases by up to 70% (compared to present) around the Mediterranean, southern Africa, central Asia and large areas of north and South America (Figure 1), although the amounts of change are different between different climate models.

In some parts of the world – such as high latitudes and the wet tropics – runoff would likely increase due to climate change. However, this additional runoff may not add to that available for use because it may occur during the wet season and there may be insufficient storage to hold the water through to the dry season; it may also lead to increased flood risk.

The broad patterns of change in runoff are reasonably consistent between different climate models, but there is considerable uncertainty in how runoff may change across south Asia, due largely to differences between climate models in projected changes in the south Asian monsoon.

Climate change will affect not only the volume, but also the timing of river flows in some regions. This may arise because of changes in the timing of the onset or end of a wet season, but is particularly likely to occur where precipitation in winter currently falls as snow. Higher temperatures would mean that winter precipitation falls as rain rather than snow, and runs off rapidly during winter rather than being stored as snow until spring.

Figure 1. Change in river flow for an increase in global average temperature of +4 ºC 

From The UK

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