Physics
Scientific paper
Oct 2007
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007georl..3419703w&link_type=abstract
Geophysical Research Letters, Volume 34, Issue 19, CiteID L19703
Physics
13
Global Change: Climate Dynamics (0429, 3309), Global Change: Earth System Modeling (1225), Global Change: Global Climate Models (3337, 4928), Biogeosciences: Carbon Cycling (4806)
Scientific paper
A coupled atmosphere-ocean-carbon cycle model is used to examine the long term climate implications of various 2050 greenhouse gas emission reduction targets. All emission targets considered with less than 60% global reduction by 2050 break the 2.0°C threshold warming this century, a number that some have argued represents an upper bound on manageable climate warming. Even when emissions are stabilized at 90% below present levels at 2050, this 2.0°C threshold is eventually broken. Our results suggest that if a 2.0°C warming is to be avoided, direct CO2 capture from the air, together with subsequent sequestration, would eventually have to be introduced in addition to sustained 90% global carbon emissions reductions by 2050.
Eby Michael
Montenegro Alvaro
Weaver Andrew J.
Zickfeld Kirsten
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