Carbon cycle and natural vegetation: Difference between revisions

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|FrameworkElementType=state component
|FrameworkElementType=state component
|Status=On hold
|Status=On hold
|Reference=Van Minnen et al., 2008; Houghton, 2010; Müller et al., 2007; Ballantyne et al., 2012; Van Minnen et al., 2009; Sitch et al., 2003;  
|Reference=Van Minnen et al., 2008; Houghton, 2010; Müller et al., 2007; Ballantyne et al., 2012; Van Minnen et al., 2009; Sitch et al., 2003; Gerten et al., 2004; Bondeau et al., 2007; Klein Goldewijk et al., 1994; Van Minnen et al., 2000;
|InputVar=Temperature; Precipitation; Wet days; Cloudiness; CO2 concentration; Crop and grass fractions; Timber use fraction; Timber harvest;
|InputVar=Temperature; Precipitation; Wet days; Cloudiness; CO2 concentration; Crop and grass fractions; Timber use fraction; Timber harvest;
|OutputVar=Potential natural vegetation; Biomes, ecoregions; Carbon pools and fluxes; NPP; NEP; Respiration; Terrestrial C balance; Carbon sequestration;
|OutputVar=Potential natural vegetation; Biomes, ecoregions; Carbon pools and fluxes; NPP; NEP; Respiration; Terrestrial C balance; Carbon sequestration;

Revision as of 17:05, 16 December 2013

Key policy issues

  • What is the role of the terrestrial biosphere in the global carbon cycle, how will it change in time as a result of climate and land-use change?
  • To what extent can the terrestrial biosphere contribute to reducing the accumulation of CO2 in the atmosphere and what are viable mechanisms?
  • What opportunities exist to reduce land-use related carbon emissions (e.g. REDD) and even enhance the carbon uptake through the establishment of new forests.
  • What are the contributions of land-use change, climate change and CO2 fertilization on the future carbon cycle and how can these be considered in climate policies?

Introduction