Sebastian Ostberg

TL;DR: Seven global vegetation models are used to analyze possible responses to future climate simulated by a range of general circulation models run under all four representative concentration pathway scenarios of changing concentrations of greenhouse gases, finding uncertainties explain 30% more variation in modeled vegetation carbon change than responses of net primary productivity alone.

TL;DR: In Paris, France, December 2015, the Conference of the Parties (COP) to the United Nations Framework Concerning on Climate Change (UNFCCC) invited the Inter- governmental Panel on Climate change (IPCC).

TL;DR: It is shown that HI drastically change the critical dimensions of water scarcity, aggravating water scarcity for 8.8% of the global population but alleviating it for another 8.3% (6.4–15.8%).

TL;DR: In Paris, France, December 2015, the Conference of the Parties (COP) to the United Nations Framework Concerning on Climate Change (UNFCCC) invited the Inter- governmental Panel on Climate change (IPCC) as mentioned in this paper.

TL;DR: In this paper, the authors use the dynamic global vegetation model LPJmL, which simulates plant physiological and ecological processes and includes a newly developed discrete layer energy balance permafrost module and a vertical carbon distribution within the soil layer.