Not exact matches
It has been estimated that to have at least a 50
per cent chance of keeping warming below 2 °C throughout the twenty - first century, the
cumulative carbon emissions between 2011 and 2050 need to be limited to around 1,100 gigatonnes of
carbon dioxide (Gt CO2).
«With
cumulative fossil fuel
emissions of 10,000 gigatonnes of
carbon (GtC), Antarctica is projected to become almost ice - free with an average contribution to sea - level rise exceeding 3 meters
per century during the first millennium.»
Cumulative carbon dioxide
emissions should be calculated on a
per capita basis for each country, so that every nation can shoulder a common but differentiated responsibility for climate change... Such a calculation «better reflects the principal of equity for developing countries»...
They estimate the relationship between observed warming and observed
cumulative CO2
emissions, calculating the «transient climate response to
cumulative emissions» — the amount of warming
per teratonne
carbon (TtC, or 1000 gigatonnes
carbon).
«The proportionality of warming to
cumulative emissions depends in part on a cancellation of the saturation of
carbon sinks with increasing
cumulative emissions (leading to a larger airborne fraction of
cumulative emissions for higher
emissions) and the logarithmic dependence of radiative forcing on atmospheric CO2 concentration [leading to a smaller increase in radiative forcing
per unit increase in atmospheric CO2 at higher CO2 concentrations; Matthews et al. (2009)-RSB-.
Other key variables such as
per capita
emissions, energy and
carbon intensity of the economy (tonnes C
per dollar of real GDP), and
cumulative emissions are also displayed.