A global warming target is converted to a fossil fuel emissions target with the help of global climate - carbon - cycle models, which reveal that eventual warming depends
on cumulative carbon emissions, not on the temporal history of emissions [12].
Today,
with cumulative carbon emissions ∼ 370 GtC from all fossil fuels, we are at a point of severely escalating ecological and environmental impacts from fossil fuel use and fossil fuel mining, as is apparent from the mountaintop removal for coal, tar sands extraction of oil, and fracking for gas.
In a paper published online today in Nature, they conclude that between 2000 and 2013,
cumulative carbon emissions for the energy and cement sectors were about 2.9 gigatons — or 13 % less than previous estimates, which pegged China's carbon emissions at something over 22 gigatons.
The United States is the second biggest emitter of carbon dioxide worldwide (and has contributed, with Europe, 52 % of the share of
cumulative carbon emissions since industrialization).
Today, with
cumulative carbon emissions ∼ 370 GtC from all fossil fuels, we are at a point of severely escalating ecological and environmental impacts from fossil fuel use and fossil fuel mining, as is apparent from the mountaintop removal for coal, tar sands extraction of oil, and fracking for gas.
Goodwin, P., R.G. Williams and A. Ridgwell, 2014: Sensitivity of climate to
cumulative carbon emissions due to compensation of ocean heat and carbon uptake.
Meeting this goal would require capping humanity's
cumulative carbon emissions at about a trillion tons, and we've already burned through about two - thirds of that «allowed» carbon budget.
This latest research reinforces their previous conclusions that «the
more cumulative carbon emissions are allowed to increase, the more global surface warming will also increase.
If we were certain that the ensemble mean warming represents the real climate systemt we could read out from figure 1c at
which cumulative carbon emission we could expect to cross this threshold.
Though cumulative carbon emissions have a tight correlation with peak warming, figure 5a shows that they share only a very weak correlation with the peak rate of warming.
One way this work can inform current policy targets is for policy - makers to
view cumulative carbon emission budgets as spread over, say, four periods: (i) 2010 — 2020, (ii) 2020 — 2050, (iii) 2050 — 2100, and (iv) 2100 — 2200.
But they have not been doing so at a rate consistent with
keeping cumulative carbon emissions low enough to reliably stay below the international target of less than 2 degrees Centigrade of global warming.
Unless one thinks that a person in China has intrinsically less right to the net allowable carbon emissions than a person in the United States or European Union, the appropriate measure of fairness would have to be based on some kind of
cumulative carbon emission per person.
In addition to it's focus on temperature increase, the report also suggests the use of
cumulative carbon emissions over time as a valuable metric for linking emissions to impacts.
A number of recent studies have found a strong link between peak human - induced global warming and
cumulative carbon emissions from the start of the industrial revolution, while the link to emissions over shorter periods or in the years 2020 or 2050 is generally weaker.
This ends up changing estimates of
cumulative carbon emissions since the pre-industrial period, but given the large uncertainties involved the authors caution against using these revisions to draw conclusions about remaining carbon budgets associated with staying within the 2C or 1.5 C warming targets.
Through their projections, Dr Goodwin and Professor Williams advise
that cumulative carbon emissions needed to remain below 195 - 205 PgC (from the start of 2017) to deliver a likely chance of meeting the 1.5 °C warming target while a 2 °C warming target requires emissions to remain below 395 - 455 PgC.
«The higher
the cumulative carbon emissions are, the warmer it gets.»
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).
The emission limit depends on climate sensitivity, but central estimates [12]--[13], including those in the upcoming Fifth Assessment of the Intergovernmental Panel on Climate Change [14], are that a 2 °C global warming limit implies
a cumulative carbon emissions limit of the order of 1000 GtC.
Michael R. Raupach, Steven J. Davis, Glen P. Peters, Robbie M. Andrew, Josep G. Canadell, Philippe Ciais, Pierre Friedlingstein, Frank Jotzo, Detlef P. van Vuuren and Corinnele Quéré, Sharing a quota on
cumulative carbon emissions, Nature Climate Change, 4, 873 - 879 (2014), doi: 10.1038 / nclimate2384.
Solomon argues that «long - term temperature change remains primarily associated with total
cumulative carbon emissions, owing to [their] much longer atmospheric residence time.»
Solomon argued a couple of years ago
that cumulative carbon emissions are the best way of assessing climate risk, since they avoid problems such as time lags that mess with other measures, such as atmospheric concentrations.
This means that only two emission targets — the peak rate and
cumulative carbon emissions — are needed to constrain two key indicators of CO2 - induced climate change (peak warming and peak warming rate), as evidenced by the maximum - likelihood estimation method used above.