[Vision2020] PLOS: "Assessing ‘‘Dangerous Climate Change’’: Required Reduction of Carbon Emissions..."
Ted Moffett
starbliss at gmail.com
Sat Feb 14 19:10:19 PST 2015
http://www.plosone.org/article/fetchObject.action?uri=info%3Adoi%2F10.1371%2Fjournal.pone.0081648&representation=PDF
Assessing ‘‘Dangerous Climate Change’’: Required Reduction of Carbon
Emissions to Protect Young People, Future Generations and Nature
James Hansen1*, Pushker Kharecha1,2, Makiko Sato1, Valerie Masson-Delmotte3,
Frank Ackerman4 , David J. Beerling5, Paul J. Hearty6, Ove Hoegh-Guldberg7,
Shi-Ling Hsu8, Camille Parmesan9,10, Johan Rockstrom11, Eelco J. Rohling
12,13, Jeffrey Sachs1, Pete Smith14, Konrad Steffen15, Lise Van Susteren16,
Karina von Schuckmann17, James C. Zachos18
Abstract: We assess climate impacts of global warming
using ongoing observations and paleoclimate data. We
use Earth’s measured energy imbalance, paleoclimate
data, and simple representations of the global carbon
cycle and temperature to define emission reductions
needed to stabilize climate and avoid potentially disastrous
impacts on today’s young people, future generations,
and nature. A cumulative industrial-era limit of
,500 GtC fossil fuel emissions and 100 GtC storage in the
biosphere and soil would keep climate close to the
Holocene range to which humanity and other species are
adapted. Cumulative emissions of ,1000 GtC, sometimes
associated with 2uC global warming, would spur ‘‘slow’’
feedbacks and eventual warming of 3–4uC with disastrous
consequences. Rapid emissions reduction is required to
restore Earth’s energy balance and avoid ocean heat
uptake that would practically guarantee irreversible
effects. Continuation of high fossil fuel emissions, given
current knowledge of the consequences, would be an act
of extraordinary witting intergenerational injustice. Responsible
policymaking requires a rising price on carbon
emissions that would preclude emissions from most
remaining coal and unconventional fossil fuels and phase
down emissions from conventional fossil fuels.
Introduction
Humans are now the main cause of changes of Earth’s
atmospheric composition and thus the drive for future climate
change [1]. The principal climate forcing, defined as an imposed
change of planetary energy balance [1–2], is increasing carbon
dioxide (CO2) from fossil fuel emissions, much of which will
remain in the atmosphere for millennia [1,3]. The climate
response to this forcing and society’s response to climate change
are complicated by the system’s inertia, mainly due to the ocean
and the ice sheets on Greenland and Antarctica together with the
long residence time of fossil fuel carbon in the climate system. The
inertia causes climate to appear
to respond slowly to this humanmade
forcing, but further long-lasting responses can be locked in.
More than 170 nations have agreed on the need to limit fossil
fuel emissions to avoid dangerous human-made climate change, as
formalized in the 1992 Framework Convention on Climate
Change [6]. However, the stark reality is that global emissions
have accelerated (Fig. 1) and new efforts are underway to
massively expand fossil fuel extraction [7–9] by drilling to
increasing ocean depths and into the Arctic, squeezing oil from
tar sands and tar shale, hydro-fracking to expand extraction of
natural gas, developing exploitation of methane hydrates, and
mining of coal via mountaintop removal and mechanized longwall
mining. The growth rate of fossil fuel emissions increased
from 1.5%/year during 1980–2000 to 3%/year in 2000–2012,
mainly because of increased coal use [4–5].
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Vision2020 Post: Ted Moffett
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