Implications of the Developed Scenarios for Climate Change

@article{Meinshausen2019ImplicationsOT,
  title={Implications of the Developed Scenarios for Climate Change},
  author={Malte Meinshausen},
  journal={Achieving the Paris Climate Agreement Goals},
  year={2019}
}
  • M. Meinshausen
  • Published 2019
  • Environmental Science
  • Achieving the Paris Climate Agreement Goals
This section provides a summary of the implications of the developed 2.0 °C and 1.5 °C scenarios for global mean climate change. Specifically, we consider atmospheric CO2 concentrations, radiative forcing, global-mean surface air temperatures and sea level rise. 
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References

SHOWING 1-3 OF 3 REFERENCES

Synthesizing long-term sea level rise projections - the MAGICC sea level model v2.0

Abstract. Sea level rise (SLR) is one of the major impacts of global warming; it will threaten coastal populations, infrastructure, and ecosystems around the globe in coming centuries.

Risks to coral reefs from ocean carbonate chemistry changes in recent earth system model projections

Coral reefs are among the most biodiverse ecosystems in the world. Today they are threatened by numerous stressors, including warming ocean waters and coastal pollution. Here we focus on the

Synthesizing long-term sea level rise projections-the MAGICC sea level model v2.0

ion is projected to increase to around 50% by 2100 (Wada, 2015). This indicates that, ultimately, the total amount of groundwater available for abstraction is limited. To account for such an upper