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

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Figure VI.C.2. Daily flows in Ebro river from 1913 to 2001 (PHN, 2000).<br />

There is increasing evidence that global climate is changing <strong>and</strong> most of <strong>the</strong> warming<br />

observed since pre-industrial era is attributable to human activities (IPCC, 2001).<br />

Observed changes in sea level, snow cover, ice extent <strong>and</strong> precipitation patterns are<br />

consistent with <strong>the</strong> current scenario of higher temperatures. Based on current trends<br />

it is reasonable to assume that <strong>the</strong> global hydrologic cycle will be accelerated, with<br />

greater event variability <strong>and</strong> extremes.<br />

Impacts of climate change can be evaluated using three different approaches; in<br />

order of increasing prediction uncertainty those are:<br />

• analysis of changes recorded in <strong>the</strong> current geophysical record;<br />

• analysis of changes predicted from Global Circulation Models (GCMs);<br />

• analysis of changes determined from various assumed scenarios of <strong>the</strong><br />

impact of global climate change.<br />

All three approaches have been adopted for <strong>the</strong> Ebro river basin.<br />

The three factors of global climate change that could most impact <strong>the</strong> hydrology of<br />

<strong>the</strong> Ebro watershed are: increasing air temperature, changes in precipitation (leading<br />

to variations in annual runoff), <strong>and</strong> sea level rise. Findings from <strong>the</strong> various studies,<br />

highlighting <strong>the</strong> effects of climate change on some components of its hydrologic<br />

cycle, as well as on <strong>the</strong> ecological status of <strong>the</strong> river <strong>and</strong> its delta area, are<br />

summarized in <strong>the</strong> following paragraphs. Some of <strong>the</strong> problems arising when trying<br />

to assess <strong>and</strong> quantify <strong>the</strong> effects of climate change are also presented.<br />

VI.C.2. <strong>Climate</strong> <strong>Change</strong> Impacts<br />

Temperatures<br />

According to IPCC (2001), global mean temperature has increased by about 0.6°C<br />

over <strong>the</strong> past 100 years. Globally <strong>the</strong> 1990s were <strong>the</strong> warmest decade on record,<br />

<strong>and</strong> 1998 <strong>the</strong> warmest year. It is likely that <strong>the</strong> increase in temperature in <strong>the</strong> 20 th<br />

century was <strong>the</strong> largest of any century during <strong>the</strong> past 1000 years. There is new <strong>and</strong><br />

stronger evidence that most of <strong>the</strong> warming observed over <strong>the</strong> past 50 years is<br />

attributable to human activities. Based on predictions from seven GCMs, IPCC<br />

(2001) reports that <strong>the</strong>re is a potential for increases in average air temperature by <strong>the</strong><br />

year 2100, ranging from +2 to +4.2 °C,. Under IPCC emission scenarios, global<br />

average temperature are projected to rise by 1.4°C to 5.8°C between 1990 <strong>and</strong> 2100,<br />

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