Climate change impacts and vulnerability in Europe 2016
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Changes <strong>in</strong> the climate system<br />
3.2 Atmosphere<br />
Key messages<br />
• Three different long-term observational records show that the global average annual near-surface (l<strong>and</strong> <strong>and</strong> ocean)<br />
temperature <strong>in</strong> the decade 2006–2015 was 0.83 to 0.89 °C higher than the pre-<strong>in</strong>dustrial average. The year 2015 was the<br />
warmest on record globally, at approximately 1 °C above the pre-<strong>in</strong>dustrial level.<br />
• <strong>Europe</strong>an l<strong>and</strong> areas <strong>in</strong> the decade between 2006 <strong>and</strong> 2015 have warmed by around 1.5 °C s<strong>in</strong>ce the pre-<strong>in</strong>dustrial age.<br />
The years 2014 <strong>and</strong> 2015 were jo<strong>in</strong>tly the warmest years on record <strong>in</strong> <strong>Europe</strong>.<br />
• Further global warm<strong>in</strong>g between 0.3 <strong>and</strong> 4.8 °C is projected for the 21st century, depend<strong>in</strong>g on the emissions scenario.<br />
The annual average l<strong>and</strong> temperature across <strong>Europe</strong> is projected to cont<strong>in</strong>ue <strong>in</strong>creas<strong>in</strong>g faster than global average<br />
temperature.<br />
• S<strong>in</strong>ce 2003, <strong>Europe</strong> has experienced several extreme summer heat waves (2003, 2006, 2007, 2010, 2014 <strong>and</strong> 2015).<br />
Such heat waves are projected to occur as often as every two years <strong>in</strong> the second half of the 21st century under a high<br />
emissions scenario (RCP8.5). The <strong>impacts</strong> will be particularly strong <strong>in</strong> southern <strong>Europe</strong>.<br />
• Precipitation <strong>change</strong>s across <strong>Europe</strong> show more spatial <strong>and</strong> temporal variability than temperature <strong>change</strong>s. Annual<br />
precipitation has <strong>in</strong>creased <strong>in</strong> most of northern <strong>Europe</strong>, <strong>in</strong> particular <strong>in</strong> w<strong>in</strong>ter, <strong>and</strong> has decreased <strong>in</strong> most of southern<br />
<strong>Europe</strong>, <strong>in</strong> particular <strong>in</strong> summer. Heavy precipitation events have <strong>in</strong>creased <strong>in</strong> northern <strong>and</strong> north-eastern <strong>Europe</strong> s<strong>in</strong>ce<br />
the 1960s whereas different <strong>in</strong>dices show diverg<strong>in</strong>g trends for south-western <strong>and</strong> southern <strong>Europe</strong>. Heavy precipitation<br />
events are projected to become more frequent <strong>in</strong> most parts of <strong>Europe</strong>.<br />
• Observations of w<strong>in</strong>d storm location, frequency <strong>and</strong> <strong>in</strong>tensity have shown considerable variability across <strong>Europe</strong> dur<strong>in</strong>g<br />
the 20th century. However, most studies agree that the risk of severe w<strong>in</strong>ter storms, <strong>and</strong> possibly of severe autumn<br />
storms will <strong>in</strong>crease <strong>in</strong> the future for the North Atlantic, as well as for northern, north-western <strong>and</strong> central <strong>Europe</strong>.<br />
• Hail is responsible for significant damage to crops, vehicles, build<strong>in</strong>gs <strong>and</strong> other <strong>in</strong>frastructure. Despite improvements<br />
<strong>in</strong> data availability, trends <strong>and</strong> projections of hail events are still subject to large uncerta<strong>in</strong>ties ow<strong>in</strong>g to a lack of direct<br />
observation <strong>and</strong> <strong>in</strong>adequate microphysical schemes <strong>in</strong> numerical weather prediction <strong>and</strong> climate models.<br />
3.2.1 Overview<br />
Relevance<br />
Changes <strong>in</strong> atmospheric composition affect<br />
atmospheric climate variables, <strong>in</strong> particular<br />
temperature, precipitation <strong>and</strong> w<strong>in</strong>d speed, which <strong>in</strong><br />
turn affect almost all natural <strong>and</strong> human-managed<br />
systems, as well as human health <strong>and</strong> well-be<strong>in</strong>g.<br />
In fact, climate <strong>change</strong> is often equated with<br />
atmospheric <strong>change</strong>s, <strong>and</strong> <strong>change</strong>s <strong>in</strong> other climate<br />
system components, such as the hydrosphere <strong>and</strong><br />
the cryosphere, are often considered effects of<br />
atmospheric <strong>change</strong>s. It is therefore not surpris<strong>in</strong>g<br />
that global mean surface temperature is specifically<br />
mentioned as a proxy for the magnitude of global<br />
climate <strong>change</strong> <strong>in</strong> Article 2 of the UNFCCC (UN, 1992),<br />
<strong>and</strong> that the political discussion on global climate<br />
policy often focuses on the most appropriate value<br />
for constra<strong>in</strong><strong>in</strong>g its <strong>in</strong>crease (see Chapter 2 for further<br />
details).<br />
While <strong>change</strong>s <strong>in</strong> annual or seasonal averages of<br />
atmospheric climate variables are easier to monitor<br />
<strong>and</strong> report, <strong>change</strong>s <strong>in</strong> extreme weather events<br />
(e.g. heat waves, heavy precipitation, w<strong>in</strong>d storms <strong>and</strong><br />
hail), which generally have the highest impact <strong>and</strong><br />
cause the greatest damage to humans <strong>and</strong> natural<br />
systems, are more difficult to detect.<br />
Selection of <strong>in</strong>dicators<br />
The follow<strong>in</strong>g are six <strong>in</strong>dicators that describe past<br />
trends <strong>and</strong> projected <strong>change</strong>s <strong>in</strong> the most dynamic<br />
component of the Earth's climate system: the<br />
atmosphere.<br />
• Global <strong>and</strong> <strong>Europe</strong>an temperature consists of two<br />
parts. Global mean surface temperature is the key<br />
climate variable to track anthropogenic climate<br />
<strong>change</strong>. It is also the only climate variable for which<br />
a political target exists. The average <strong>Europe</strong>an l<strong>and</strong><br />
temperature gives a clear signal of climate <strong>change</strong><br />
<strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> <strong>2016</strong> | An <strong>in</strong>dicator-based report<br />
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