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- "Most aspects of climate change will persist for many centuries even if emissions of CO2 are stopped," the authors write.
- "It is very likely that the Arctic sea ice cover will continue to shrink and thin and that Northern Hemisphere spring snow cover will decrease during the 21st century as global mean surface temperature rises."
- "Global glacier volume will further decrease." That's worldwide, from Greenland to the Andes.
- "Global surface temperature change for the end of the 21st century is likely to exceed 1.5°C relative to 1850 to 1900 … and more likely than not to exceed 2°C" for typical warming scenarios. That's a lowball, too.
- "The contrast in precipitation between wet and dry regions and between wet and dry seasons will increase…" Read: Drier deserts and flooded wetlands.
- "Global mean sea level will continue to rise during the 21st century … the rate of sea level rise will very likely exceed that observed during 1971–2010 due to increased ocean warming and increased loss of mass from glaciers and ice sheets," the paper notes. According to Stefan Rahmstorf of RealClimate, this means "a much more rapid sea-level rise is now projected (28-97 cm by 2100). This is more than 50% higher than the old projections (18-59 cm) when comparing the same emission scenarios and time periods.With unabated emissions (and not only for the highest scenario), the IPCC estimates that by the year 2300 global sea levels will rise by 1-3 meters."
- "It is virtually certain that near-surface permafrost extent at high northern latitudes will be reduced as global mean surface temperature increases. By the end of the 21st century, the area of permafrost near the surface (upper 3.5 m) is projected to decrease by between 37% to 81%." That means the icy ground that's currently locking methane underground is melting, releasing more global-warming gases.
- "Further uptake of carbon by the ocean will increase ocean acidification."
- "The global ocean will continue to warm during the 21st century. Heat will penetrate from the surface to the deep ocean and affect ocean circulation."