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Climate Change and the European Water Dimension - Agri ...

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<strong>Climate</strong> <strong>Change</strong><br />

<strong>and</strong> <strong>the</strong><br />

<strong>European</strong> <strong>Water</strong> <strong>Dimension</strong><br />

Chapter II. <strong>Climate</strong> <strong>Change</strong> at <strong>the</strong> <strong>European</strong><br />

scale<br />

Key Points<br />

• The average increase in <strong>the</strong> observed annual mean<br />

temperature across <strong>the</strong> <strong>European</strong> continent is 0.8 0 C. The<br />

temperatures during <strong>the</strong> winter season have in general<br />

increased more than during <strong>the</strong> summer.<br />

• The summer of 2003 was very likely <strong>the</strong> hottest summer <strong>and</strong><br />

<strong>the</strong> last 30 years appear to have had <strong>the</strong> warmest climate<br />

within <strong>the</strong> last five centuries.<br />

• Aerosols <strong>and</strong> ozone appear to exert an important influence<br />

on radiative forcing in <strong>the</strong> Mediterranean basin.<br />

• Annual precipitation over Nor<strong>the</strong>rn Europe has increased<br />

by between 10 <strong>and</strong> 40% in <strong>the</strong> last century while <strong>the</strong><br />

Mediterranean basin has experienced up to 20% reduction<br />

in precipitation.<br />

• Heat waves as well as intense precipitation events,<br />

especially in winter, will become more frequent throughout<br />

Europe. Risk of drought is likely to increase in central <strong>and</strong><br />

sou<strong>the</strong>rn Europe.<br />

29

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