164 NATURE CLIMATE CHANGE | VOL 4 | MARCH 2014 | www.nature.com/natureclimatechange
opinion & comment
COMMENTARY:
The climate policy narrative for
a dangerously warming world
Todd Sanford, Peter C. Frumhof, Amy Luers and Jay Gulledge
It is time to acknowledge that global average temperatures are likely to rise above the 2 °C policy
target and consider how that deeply troubling prospect should afect priorities for communicating and
managing the risks of a dangerously warming climate.
W
hen world leaders signed the
Copenhagen Accord in 2009,
they agreed to limit the increase
in global average surface temperature to
less than 2 °C above the pre-industrial level,
a target then widely viewed as consistent
with avoiding dangerous climate change
and feasible to achieve through ambitious
reductions in heat-trapping emissions.
he climate policy agenda has since been
dominated by the narrative that swit and
deep reductions in emissions are urgently
needed to stay below 2 °C (refs 1–4).
his global temperature target has brought
a valuable focus to international climate
negotiations, motivating commitment to
emissions reductions from several nations
5
.
But a policy narrative that continues to frame
this target as the sole metric of success or
failure to constrain climate change risk is
now itself becoming dangerous, because it
ill-prepares society to confront and manage
the risks of a world that is increasingly likely
to experience warming well in excess of 2 °C
this century.
Inadvertently, the Intergovernmental Panel
on Climate Change (IPCC) — the scientiic
body charged with informing governments
about climate change — reinforces the
present narrative by failing to provide
policymakers with guidance on how to weigh
the relative likelihood of the scenarios of
future concentrations of heat-trapping gases
and other drivers of warming on which its
climate change projections are based.
Science and the climate policy narrative
Since Copenhagen, the foundation on which
the 2 °C target was built has steadily eroded.
Both human populations and natural systems
are now understood to face serious risks of
substantial climate change damages with
less than 2 °C warming
6
, leading many of
the most vulnerable developing nations to
argue, with just cause, that the target should
be lowered to 1.5 °C. Indeed, the relatively
modest warming experienced so far (0.85 °C
increase since 1880)
7
is already driving
arguably dangerous impacts, including more
deaths from extreme heat
8
, widespread forest
die-of from climate-driven heat stress and
drought
9
, and more extreme coastal looding
from higher storm surges resulting from
sea-level rise
10
. Such impacts underlie recent
demands by developing countries for so-
called loss and damage payments, a prevalent
topic of negotiations during the COP19
climate meeting in November 2013.
Global carbon emissions have also
continued to rise, unabated, on average by
3% per year since 2000, including the years
since the Copenhagen Accord was signed
2
.
At present, emissions are tracking just above
the highest Representative Concentration
Pathway (RCP 8.5) used by the IPCC to assess
projected climate change; a pathway in which
emissions would hurtle past the 2 °C carbon
budget before mid-century (Fig. 1). Keeping
global temperatures from rising above 2 °C
could be achieved by rapidly transitioning
to a trajectory similar to RCP 2.6, the lowest
concentration pathway used by the IPCC.
Following RCP 2.6 would require global
carbon emissions to decline by 50% below
1990 levels by mid-century and, according to
several models, may well require sustained
global net negative emissions a few decades
later (Fig. 1). his might, in principle,
be achieved by coupling biomass energy
production with carbon capture and storage
on a massive scale or by other yet-to-be-
developed technologies
2
.
Such heroic assumptions lead a growing
number of analysts to conclude that
prospects for limiting warming to 2 °C are
becoming vanishingly small
2,11
. One recent
study excluded climate model outputs using
RCP 2.6 from interscenario comparisons of
projected changes on the assumption that
RCP 2.6 is currently unfeasible
12
. A projection
is not destiny, of course, but some are surely
more likely than others. Yet, in its most recent
assessment, the IPCC makes no judgement
on the relative likelihood of the magnitude
of future warming associated with each RCP
in presenting climate model projections,
implicitly treating all scenarios as equivalently
plausible. Some scenarios are also projected
to lead to very divergent futures in terms of
impacts
1
. his leads to efective responses to
manage climate risk heavily depending, in
some cases, on the scenario actually realized.
Policymakers thus have no clear scientiic
guidance for confronting and managing the
growing risk of high-magnitude warming.
Building on its strong legacy of rigorous
and detailed treatments of likelihood and
uncertainty of observed trends, attribution of
change and model output (including future
projections)
13
, and on recommendations irst
made
14
and subsequently elaborated on
15
more than a decade ago, the IPCC should
provide policymakers with guidance on the
relative likelihood of diferent magnitudes of
future warming. One path forward would be
to build on the approach of soliciting expert
judgement found on other subjects, such
as transient climate response to alternative
radiative forcing trajectories
16
, eliciting input
that considers both climate sensitivities
and the biophysical, socioeconomic,
technological and policy drivers of future
emissions and concentrations.
Towards a new climate policy narrative
An ambitious goal for stabilizing global
temperatures must remain a central focus of
climate policy within a comprehensive risk-
management framework. But calling for swit
and deep reductions in emissions, although
essential, is not suicient. Confronting
and managing the risks of high-magnitude
warming will require a science-based policy
narrative that honestly communicates these
risks, accounts for potential policy failures
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