Not exact matches
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).
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].
It's a big job, but it's one that has to be done anyway, since if the whole world tries to pull itself into prosperity by burning
carbon at the rate the US does, then we run out of coal even at the highest estimates by 2100, and you wind up
with no fossil energy and the hellish climate you get from 5000 gigatonnes
cumulative emission.
The bottom line is, there is only one scenario
with a good chance of averting irreversible climate change: one that caps global
cumulative industrial - era
carbon emissions at under one trillion tons.
Solomon argues that «long - term temperature change remains primarily associated
with total
cumulative carbon emissions, owing to [their] much longer atmospheric residence time.»
«
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.&ra
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.&ra
with an average contribution to sea - level rise exceeding 3 meters per century during the first millennium.»
Our analysis combines published relationships between
cumulative carbon emissions and warming, together
with two possible versions of the relationship between warming and sea level, to estimate global and regional sea - level commitments from different
emissions totals.
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.
Projections of long - term committed SLR as a function of
cumulative carbon emissions,
with 66 % CIs, assuming (triggered case) or not assuming (baseline case) that eventual collapse of the WAIS is already inevitable.
Shown are three idealized Co2
emission paths (a) each consistent
with total
cumulative emissions (b) of 1 trillion tonnes of
carbon -LSB-...]
This is a serious problem in itself, but a more fundamental problem
with the
emission budget concept seems to be more - or-less unexplored: Do
cumulative carbon emission budgets have a sound scientific foundation?
Armed
with our model ensemble projection, a temperature limit (2 °C), exceedance likelihood (33 %) and our «one model, one vote» ensemble interpretation, we find the
cumulative carbon emission where approximately 33 % of our modeled realizations have warmed more than 2 °C.
Abstract Recent estimates of the global
carbon budget, or allowable
cumulative CO2
emissions consistent
with a given level of climate warming, have the potential to inform climate mitigation policy discussions aimed at maintaining global temperatures below 2 ° C.
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.
Studies surveyed Millar, R. et al. (2017) Emission budgets and pathways consistent
with limiting warming to 1.5 C, Nature Geophysics, doi: 10.1038 / ngeo3031 Matthews, H.D., et al. (2017) Estimating
Carbon Budgets for Ambitious Climate Targets, Current Climate Change Reports, doi: 10.1007 / s40641 -017-0055-0 Goodwin, P., et al. (2018) Pathways to 1.5 C and 2C warming based on observational and geological constraints, Nature Geophysics, doi: 10.1038 / s41561 -017-0054-8 Schurer, A.P., et al. (2018) Interpretations of the Paris climate target, Nature Geophysics, doi: 10.1038 / s41561 -018-0086-8 Tokarska, K., and Gillett, N. (2018)
Cumulative carbon emissions budgets consistent with 1.5 C global warming, Nature Climate Change, doi: 10.1038 / s41558 -018-0118-9 Millar, R., and Friedlingstein, P. (2018) The utility of the historical record for assessing the transient climate response to cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta
Cumulative carbon emissions budgets consistent
with 1.5 C global warming, Nature Climate Change, doi: 10.1038 / s41558 -018-0118-9 Millar, R., and Friedlingstein, P. (2018) The utility of the historical record for assessing the transient climate response to
cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta
cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on
carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0457
«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-.
As fossil - based power generation is replaced
with wind and solar power,
cumulative carbon emissions from centralized power facilities will be greatly reduced.
I may have misunderstood something, but looking at the 2 °C curve I couldn't see how the
cumulative emissions fit
with the 50 % chance of 2 °C
carbon budget from the Synthesis report.
The Intergovernmental Panel on Climate Change in 2013 estimated that
cumulative carbon dioxide
emissions from fossil fuels and cement production — from 1750 to 2011 — was about 365 billion metric tonnes as
carbon (GtC),
with another 180 GtC from deforestation and agriculture.
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.
Overall the G8 pathway has
cumulative carbon dioxide
emissions (2012 — 2100) of 1,485 Gt CO2 for fossil fuels, and 125 for LUCF,
with an additional 45 GtCO2 after 2100 assuming continued exponential decline.
This appears to me to comport
with the «IEO2011 Reference case projects about 1 trillion metric tons of additional
cumulative energy - related
carbon dioxide
emissions between 2009 and 2035» that you cited in # 143, which clearly states CO ₂ in the sentence.
Primary energy demand until 2035, from «Facing China's Coal Future», figure 1, page 7, Increases in
carbon emissions by fuel type for regions
with highest absolute
emissions growth, 2008 - 2035 from IEO2011, figures 115, page 143, and «
Cumulative carbon dioxide
emissions by region», figure 116, also on page 143, same link as above.
The most useful article for the reader unfamiliar
with the literature is probably, «Warming caused by
cumulative carbon emissions towards the trillionth tonne.»