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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every circumstance. However, the Commission is concerned that if <strong>to</strong>day’s extreme events become<br />
more frequent, as the modelled climate projections suggest, so <strong>to</strong>o will the level of disruption that<br />
it causes if appropriate action is not taken. Not only will <strong>to</strong>day’s extreme weather events become<br />
more commonplace, but it is also likely that the events themselves will become more extreme.<br />
GLOBAL CLIMATE CHANGE<br />
2.8<br />
2.9<br />
Scientists have a range of <strong>to</strong>ols that they can call upon for informing policy-makers about climate<br />
change – both changes that have already occurred and projections for the future. These include<br />
weather measurements from a variety of sources and climate simulations from computerised<br />
Global Circulation Models (GCMs). GCMs are used <strong>to</strong> provide the basis from which future<br />
climate projections are made, and the boundary conditions that enable more regional and<br />
local-scale projections, through a process of regional climate downscaling, <strong>to</strong> be made.<br />
Globally, data from land-based weather stations and ships as well as from satellites confirm that,<br />
although there are regional variations in temperature, the planet is warming (see Figure 2-I and<br />
the more recent literature cited). 1,2 Generally, the warming trend is observed in both maximum<br />
and minimum recorded temperatures, with air masses over land warming faster than those over<br />
oceans, and winter months warming faster than summer. The number of days with temperatures<br />
below freezing declined during the second half of the 20th century in most land areas of the<br />
Northern hemisphere. In the Arctic region, temperatures have increased at almost twice the<br />
average global rate in the last century. 3<br />
FIGURE 2-I<br />
Global average near-surface temperatures 1850-2006 4<br />
The deviation of annual average global mean near-surface temperature (red bars) from the average over the<br />
1961-1990 baseline. 5 The blue line shows the data smoothed <strong>to</strong> emphasise decadal variations.<br />
Temperature change (°C)<br />
with respect <strong>to</strong> 1961–1990<br />
0.8<br />
0.6<br />
0.4<br />
0.2<br />
0.0<br />
-0.2<br />
-0.4<br />
-0.6<br />
-0.8<br />
1860 1880 1900 1920 1940 1960 1980 2000<br />
Year<br />
7<br />
Chapter 2