| Literature DB >> 34526406 |
Johan Rockström1,2, Tim Beringer3, David Hole4, Bronson Griscom4, Michael B Mascia4, Carl Folke2,5, Felix Creutzig6,7.
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Year: 2021 PMID: 34526406 PMCID: PMC8463783 DOI: 10.1073/pnas.2115218118
Source DB: PubMed Journal: Proc Natl Acad Sci U S A ISSN: 0027-8424 Impact factor: 11.205
Fig. 1.(A) Carbon sinks in major biomes (SI Appendix, Table 1). Grey areas indicate regions dominated by agriculture. (B) Carbon stocks in vegetation and soils in major biomes and the share of each biome remaining intact today (SI Appendix, Table 1). (C) Global average temperature changes relative to pre-industrial levels under RCP2.6, where the pathway meeting the “Paris target” is the standard RCP2.6 simulation. “Biosphere loss” shows global temperature change without land carbon sinks from 1900. The Δ0.4 °C arrow shows the estimated dampening effect up until today from land-based ecosystems. “Full NCS” assumes large-scale restoration of land-based natural carbon sinks in forests, grasslands, peatlands, and wetlands, as well as avoided future ecosystem degradation, amounting to total emission reductions of 4.6 GtC per year after 2030 (SI Appendix, Methods for details).