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Key vulnerabilities to climate change

Key vulnerabilities to climate change. Some ecosystems are highly vulnerable: Coral reefs, marine shell organisms Tundra, boreal forests, mountain and Mediterranean regions 20-30% of plant and animal species at risk of extinction. Some regions will be more affected than others:

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Key vulnerabilities to climate change

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  1. Key vulnerabilities to climate change • Some ecosystemsare highly vulnerable: • Coral reefs, marine shell organisms • Tundra, boreal forests, mountain and Mediterranean regions • 20-30% of plant and animal species at risk of extinction • Some regionswill be more affected than others: • The Arctic (ice sheet loss, ecosystem changes) • Sub-Saharan Africa (water stress, reduced crops) • Small islands (coastal erosion, inundation) • Asian mega-deltas (flooding from sea and rivers)

  2. Mitigation urgently needed Mitigation needs to start in short term, even when benefits may only arise in a few decades • Continued GHG emissions at or above current rate would induce larger climatic changes than those observed in 20th century • Emissions of the greenhouse gases covered by the Kyoto Protocol increased by about 70% from 1970–2004

  3. Beyond adaptation Making development more sustainable can enhance both mitigative and adaptive capacity, and reduce emissions and vulnerability to climate change • Adaptation to climate change is necessary to address impacts resulting from the warming which is already unavoidable due to past emissions • However: • Adaptation alone cannot cope with all the projected impacts of climate change • The costs of adaptation and impacts will increase as global temperatures increase

  4. Pathways towards stabilization Characteristics of stabilization scenarios • Mitigation efforts over the next two to three decades will have a large impact on opportunities to achieve lower stabilization levels [1] The best estimate of climate sensitivity is 3ºC [WG 1 SPM]. [2] Note that global mean temperature at equilibrium is different from expected global mean temperature at the time of stabilization of GHG concentrations due to the inertia of the climate system. For the majority of scenarios assessed, stabilisation of GHG concentrations occurs between 2100 and 2150. [3] Ranges correspond to the 15th to 85th percentile of the post-TAR scenario distribution. CO2 emissions are shown so multi-gas scenarios can be compared with CO2-only scenarios.

  5. Mitigation costs in 2030 Trajectories towards stabilization levels (ppm CO2-eq) Median GDP reduction (%) Range of GDP reduction (%) Reduction of average annual GDP growth rates (percentage points) 590-710 0.2 -0.6 – 1.2 < 0.06 535-590 0.6 0.2 – 2.5 <0.1 445-535 Not available < 3 < 0.12 Estimated global macro-economic costs in 2030 for least-cost trajectoriestowards different long-term stabilization levels 0.6% gain to 3% decrease of GDP

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