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Climate change, impacts and vulnerability in Europe ... - MemoFin.fr

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Changes <strong>in</strong> the climate system2 Changes <strong>in</strong> the climate system2.1 Human <strong>in</strong>fluence on the climatesystem2.1.1 The climate system<strong>Climate</strong> denotes the statistics (average conditions<strong>and</strong> variability) of the day-to-day weather over along time period (usually 30 years). In contrast,weather denotes the state of the atmosphere at anygiven time, such as the day-to-day temperature <strong>and</strong>precipitation activity.The Earth's climate system is a complex systemconsist<strong>in</strong>g of several closely l<strong>in</strong>ked subsystems:the atmosphere, the hydrosphere (oceans, lakes<strong>and</strong> rivers), the cryosphere (snow <strong>and</strong> ice), <strong>and</strong> thelithosphere (soils). The climate system is closelyl<strong>in</strong>ked to the other components of the Earth system,such as the biosphere (see Figure 2.1).The climate system is <strong>in</strong>fluenced by many factors,such as solar activity, the Earth's orbit aroundthe Sun, atmospheric composition <strong>and</strong> volcanicactivity. <strong>Climate</strong> has always been chang<strong>in</strong>g as aresult of <strong>change</strong>s <strong>in</strong> these factors. For example, thetransitions between ice ages <strong>and</strong> <strong>in</strong>termediate warmphases (<strong>in</strong>terglacials) dur<strong>in</strong>g the last one millionyears were triggered by predictable <strong>change</strong>s <strong>in</strong> theposition of the Earth's axis with respect to the Sun,followed by an amplification of the <strong>in</strong>itial <strong>change</strong>sthrough feedback mechanisms <strong>in</strong> the climatesystem. In addition to the long-term <strong>change</strong>s, theclimate is characterised by substantial variability onmultiple time scales. Examples <strong>in</strong>clude daily <strong>and</strong>seasonal cycles but also more irregular multi‐year<strong>and</strong> multi-decadal phenomena such as ENSO(El Niño-Southern Oscillation), NAO (North Atlanticoscillation), PDO (Pacific decadal oscillation), <strong>and</strong>the Arctic <strong>and</strong> Antarctic oscillations.Figure 2.1Components of the climate system, their processes <strong>and</strong> <strong>in</strong>teractionsSource: IPCC, 2007 (FAQ 1.2, Figure 1).<strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> 201249

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