Twenty-eighth Report Adapting Institutions to Climate Change Cm ...
Twenty-eighth Report Adapting Institutions to Climate Change Cm ...
Twenty-eighth Report Adapting Institutions to Climate Change Cm ...
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FIGURE 2-IV<br />
<strong>Change</strong> in observed temperature over Western Europe over a 200-year period 34<br />
The black-line graph shows the change in observed temperatures from 1900, including the unusual 2003<br />
temperature (see 2003 arrow). Superimposed in red are the modelled temperature changes extended <strong>to</strong> 2100.<br />
The projections suggest that the unusual temperature experienced over Western Europe in 2003 could be<br />
considered normal by 2040 and cool by 2060. Temperature change is illustrated as a change from the<br />
1961-1990 baseline.<br />
2.42 Because of these complex interactions, the hydrological system is non-linear; small changes in<br />
precipitation may cause disproportionate changes in other fac<strong>to</strong>rs such as the environmental<br />
quality of rivers and streams, for example, if abstraction rates increase <strong>to</strong> meet the needs for water.<br />
And changes in demand for water as a result of policy, technology or behavioural changes may<br />
mitigate some of the impact of drier summers.<br />
2.43<br />
Temperature change (°C)<br />
8<br />
6<br />
4<br />
2<br />
0<br />
Observed temperatures<br />
Simulated temperatures<br />
-2<br />
1900 1950 2000<br />
Date<br />
© Crown copyright Met Office<br />
Western Europe<br />
In this section we shall illustrate the likely impact of climate change on demand for water, water<br />
quality and the risks of drought or flooding.<br />
Demand for water<br />
2.44 <strong>Climate</strong> change is unlikely <strong>to</strong> be the most significant influence on the demand for water. People may<br />
use slightly more water for showering or for domestic gardening, for example, during hot periods<br />
(which will become more common) and industrial use may also change. Other fac<strong>to</strong>rs such as<br />
demographic change and greater use of domestic appliances are more significant drivers for higher<br />
demand. Other influences, such as policies <strong>to</strong> reduce demand (for example <strong>to</strong> charge according <strong>to</strong><br />
metering or <strong>to</strong> promote water efficiency), will offset some of these upward pressures.<br />
19<br />
2003<br />
2040s<br />
2060s<br />
Summer 2003<br />
normal by 2040s, cool by 2060s<br />
2050 2100<br />
Chapter 2