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|a When could global warming reach 4 degrees C? |h [electronic resource]. |
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|a [S.l.] : |b The Royal Society, |c 2011. |
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|a Philosophical Transactions of the Royal Society. |
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|a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights. |
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|a The Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report
(AR4) assessed a range of scenarios of future greenhouse-gas emissions without policies
to specifically reduce emissions, and concluded that these would lead to an increase
in global mean temperatures of between 1.6◦C and 6.9◦C by the end of the twentyfirst
century, relative to pre-industrial. While much political attention is focused on the
potential for global warming of 2◦C relative to pre-industrial, the AR4 projections clearly
suggest that much greater levels of warming are possible by the end of the twentyfirst
century in the absence of mitigation. The centre of the range of AR4-projected
global warming was approximately 4◦C. The higher end of the projected warming was
associated with the higher emissions scenarios and models, which included stronger
carbon-cycle feedbacks. The highest emissions scenario considered in the AR4 (scenario
A1FI) was not examined with complex general circulation models (GCMs) in the AR4,
and similarly the uncertainties in climate–carbon-cycle feedbacks were not included in
the main set of GCMs. Consequently, the projections of warming for A1FI and/or with
different strengths of carbon-cycle feedbacks are often not included in a wider discussion
of the AR4 conclusions. While it is still too early to say whether any particular scenario
is being tracked by current emissions, A1FI is considered to be as plausible as other
non-mitigation scenarios and cannot be ruled out. (A1FI is a part of the A1 family of
scenarios, with ‘FI’ standing for ‘fossil intensive’. This is sometimes erroneously written
as A1F1, with number 1 instead of letter I.) This paper presents simulations of climate
change with an ensemble of GCMs driven by the A1FI scenario, and also assesses the
implications of carbon-cycle feedbacks for the climate-change projections. Using these
GCM projections along with simple climate-model projections, including uncertainties
in carbon-cycle feedbacks, and also comparing against other model projections from the
IPCC, our best estimate is that the A1FI emissions scenario would lead to a warming
of 4◦C relative to pre-industrial during the 2070s. If carbon-cycle feedbacks are stronger,
which appears less likely but still credible, then 4◦C warming could be reached by the
early 2060s in projections that are consistent with the IPCC’s ‘likely range’. |
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|a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software. |
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|a. |x Intergovernmental Panel on Climate Change |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15042653/00001 |y Click here for full text |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/04/26/53/00001/Betts et al_2011_When could global warming reach 4 Cthm.jpg |
