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  <front>
    <journal-meta><journal-id journal-id-type="publisher">ESD</journal-id><journal-title-group>
    <journal-title>Earth System Dynamics</journal-title>
    <abbrev-journal-title abbrev-type="publisher">ESD</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Earth Syst. Dynam.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">2190-4987</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/esd-9-1155-2018</article-id><title-group><article-title>ESD Ideas: a simple proposal to improve the <?xmltex \hack{\break}?> contribution of IPCC WGI to the assessment <?xmltex \hack{\break}?> and communication of climate change risks</article-title><alt-title>ESD Ideas: a simple proposal to improve the contribution of IPCC WGI</alt-title>
      </title-group><?xmltex \runningtitle{ESD Ideas: a simple proposal to improve the contribution of IPCC WGI}?><?xmltex \runningauthor{R.~T.~Sutton}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Sutton</surname><given-names>Rowan T.</given-names></name>
          <email>rowan.sutton@ncas.ac.uk</email>
        <ext-link>https://orcid.org/0000-0001-8345-8583</ext-link></contrib>
        <aff id="aff1"><institution>National Centre for Atmospheric Science, Department of Meteorology, <?xmltex \hack{\break}?> University of Reading, Reading, RG6 6BB, UK</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Rowan T. Sutton (rowan.sutton@ncas.ac.uk)</corresp></author-notes><pub-date><day>4</day><month>October</month><year>2018</year></pub-date>
      
      <volume>9</volume>
      <issue>4</issue>
      <fpage>1155</fpage><lpage>1158</lpage>
      <history>
        <date date-type="received"><day>25</day><month>May</month><year>2018</year></date>
           <date date-type="rev-request"><day>11</day><month>June</month><year>2018</year></date>
           <date date-type="rev-recd"><day>28</day><month>August</month><year>2018</year></date>
           <date date-type="accepted"><day>11</day><month>September</month><year>2018</year></date>
      </history>
      <permissions>
        
        
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://esd.copernicus.org/articles/9/1155/2018/esd-9-1155-2018.html">This article is available from https://esd.copernicus.org/articles/9/1155/2018/esd-9-1155-2018.html</self-uri><self-uri xlink:href="https://esd.copernicus.org/articles/9/1155/2018/esd-9-1155-2018.pdf">The full text article is available as a PDF file from https://esd.copernicus.org/articles/9/1155/2018/esd-9-1155-2018.pdf</self-uri>
      <abstract>
    <p id="d1e83">The purpose of the Intergovernmental Panel on Climate Change (IPCC) is to
provide policy-relevant assessments of the scientific evidence about climate
change. Policymaking necessarily involves risk assessments, so it is
important that IPCC reports are designed accordingly. This paper proposes a
specific idea, illustrated with examples, to improve the contribution of IPCC
Working Group I to informing climate risk assessments.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <title>Introduction</title>
      <p id="d1e93">The process of drafting the Working Group I (WGI) contribution to the Sixth
Assessment Report of the Intergovernmental Panel on Climate Change (IPCC AR6)
began recently with the first lead author meeting held in Guangzhou, China,
in June 2018. An issue that merits greater attention than in previous WGI
reports is the assessment and communication of risk. It is now widely
accepted that it is appropriate – and necessary for decision-making – to
frame climate change as a problem in risk assessment and risk management
(King et al., 2015; Weaver et al., 2017). In the AR5 greater use was made
than in previous assessment reports of a formal risk assessment framework
which spans the dimensions of hazard, exposure and vulnerability (IPCC,
2014). However, risk framing had little influence on the WGI report, and this
should be addressed in AR6.</p>
      <p id="d1e96">A common measure of risk is likelihood <inline-formula><mml:math id="M1" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> impact (Fig. 1). It is
standard practice in risk assessment to highlight both the most likely
impacts <italic>and</italic> low-likelihood high-impact scenarios. Such scenarios
merit specific attention because the associated costs can be extremely high,
so decision makers need to know about them. It follows that WGI has a
responsibility to assess and explicitly communicate the scientific evidence
concerning potential high-impact scenarios, even when the likelihood of
occurrence is assessed to be small. In past reports the assessment of key
parameters by WGI has focussed overwhelmingly on likely ranges only. When
information has been provided about the tails of distributions only
likelihoods have been communicated using terms – following the IPCC's
uncertainty guidance (Mastrandrea et al., 2010) – such as “very unlikely”
or “extremely unlikely”: a clear steer that policymakers should largely
ignore such possibilities. But this is wrong. Policymakers care about risk,
not likelihood alone. The IPCC's uncertainty guidance is valuable, but by
itself it is insufficient to guide the assessment of risk. In particular, the
focus on likelihood terminology that is symmetric with respect to high- and
low-impact scenarios downplays the importance of low-likelihood high-impact
risks (Fig. 1).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1" specific-use="star"><caption><p id="d1e111">A schematic representation of how climate change risk depends on
equilibrium climate sensitivity (ECS). <bold>(a)</bold> A possible likelihood
distribution consistent with the IPCC AR5 assessment that “Equilibrium
climate sensitivity is likely in the range 1.5 to 4.5 <inline-formula><mml:math id="M2" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C (high
confidence), extremely unlikely less than 1 <inline-formula><mml:math id="M3" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C (high confidence) and
very unlikely greater than 6 <inline-formula><mml:math id="M4" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C (medium confidence)”.
<bold>(b)</bold> A schematic illustration of the fact that, for a given emissions scenario, the cost of impacts
and adaptation rises very rapidly (shown here as an exponential damage
function) with ECS. <bold>(c)</bold> In this example, the resultant risk
(quantified here as likelihood <inline-formula><mml:math id="M5" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> impact) is highest for high ECS
values. The precise shape of the risk curve is dependent on assumptions about
the shape of the likelihood and damage functions at high sensitivity
(Weitzman, 2011) (figure by Ed Hawkins).</p></caption>
        <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://esd.copernicus.org/articles/9/1155/2018/esd-9-1155-2018-f01.png"/>

      </fig>

      <p id="d1e164">I suggest the WGI authors should agree on a modest number of key parameters for
which an assessed physically plausible high-impact scenario (PPHIS)
or storyline (e.g. Zappa and Shepherd, 2017) can be provided. This should be
done for core parameters such as climate sensitivity and TCRE (the transient
climate response to cumulative carbon emissions: Allen et al., 2009; Matthews
et al., 2009) and could also be done for some large-scale impact-relevant
metrics (informed by WGII), such as the magnitude of increases in extreme
rainfall. There will be a need to agree on consistent procedures for the
definition, description and use of such storylines; for example, they could
be associated with a specific<?pagebreak page1156?> assessed likelihood, and their characterisation
should emphasise physical constraints and evidence, not model results alone.
This will be helped by a growing literature on which to draw (e.g. Hazeleger
et al., 2015; Zappa and Shepherd, 2017). Physically based high-impact
storylines are distinct from socioeconomic scenarios, but the WGI report
could usefully provide information on outcomes that could arise from a
combination of e.g. high climate sensitivity and a high-emissions scenario.</p>
</sec>
<sec id="Ch1.S2">
  <title>Practical implementation and examples</title>
      <p id="d1e173">WGI could adopt a practical definition of a physically plausible high-impact
scenario (PPHIS) along the following lines:
<list list-type="bullet"><list-item>
      <p id="d1e178">an assessed physically based storyline for specific aspects of future
climate change that is consistent with all available evidence and would
result in impacts that are substantially greater than those implied by the
relevant <italic>likely</italic> range.</p></list-item></list>
The characterisation of each PPHIS should include (1) an assessment of
likelihood and (2) an assessment of impact <italic>explicitly framed in conditional terms</italic> (i.e. conditional on the PPHIS being realised in the real
world), with separate assessed confidence levels for each of these two
components. This approach is in line with the IPCC uncertainty guidelines
(Mastrandrea et al., 2010), which state the following: “For findings (effects) that are
conditional on other findings (causes) … [author teams should]
consider independently evaluating the degrees of certainty in both causes
and effects, with the understanding that the degree of certainty in the
causes may be low.”</p>
      <p id="d1e188">With regard to likelihood, I propose that WGI should base PPHIS on scenarios
that are assessed to be <italic>very unlikely</italic> (0 %–10 %) rather than
<italic>extremely unlikely</italic> (0 %–5 %) or <italic>exceptionally unlikely</italic> (0 %–1 %). In
the context of deep uncertainty, attempts to quantify the likelihood of a
PPHIS more precisely are unlikely to be fruitful and are not necessary to
provide information that is useful for risk assessment (see
e.g. <uri>http://www.deepuncertainty.org</uri>, 27 September 2018).
Information about impacts should be limited in WGI
to physical climate variables but should be quantitative where possible and
include an assessed confidence level. WGII could make use of the WGI PPHIS
to provide further information about impacts; this would help with coordination
between the working group reports and the production of the AR6 Synthesis Report.</p>
      <p id="d1e203">Potential abrupt changes have long been recognised as an important
risk-relevant issue for IPCC WGI to assess (e.g. Sect. 12.5.5 in Collins
et al., 2013). However, abrupt changes are only a subset – and not obviously
the most<?pagebreak page1157?> important subset – of PPHIS. It is notable that hardly any
information about abrupt changes was included in the AR5 WGI Summary for
Policymakers, and where information was included (e.g. for the Atlantic Meridional Overturning Circulation,
Sect. E.4 in IPCC, 2013), it addressed likelihood only with little or no information provided about impact.</p>
      <p id="d1e206">Below are three examples of how PPHIS could be used by WGI, adapted from the
WGI AR5 Summary for Policymakers. In these examples all the information used
can be found somewhere within the AR5 report, but the synthesis and
communication (including framing) of this information is different.
<list list-type="order"><list-item>
      <p id="d1e211"><italic>ECS</italic>. It is <italic>very unlikely</italic> that ECS is greater than 6 <inline-formula><mml:math id="M6" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C (medium confidence) but this value may be considered
a physically plausible high-impact scenario (PPHIS). If realised, such a
value for ECS would <italic>very likely</italic> result in an increase in global mean temperature
by 2100 well above 2 <inline-formula><mml:math id="M7" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C relative to 1850–1900 under all RCP scenarios
except RCP2.6 (high confidence).</p></list-item><list-item>
      <p id="d1e241"><italic>Sea level</italic>. A partial collapse of the marine-based sectors of the Antarctic ice sheet is
considered <italic>unlikely</italic> during the 21st century (medium confidence). However, if realised this PPHIS
could cause an additional contribution to sea level rise of up to several
tenths of a metre during the 21st century (medium confidence).</p></list-item><list-item>
      <p id="d1e250"><italic>Atlantic Meridional Overturning Circulation (AMOC)</italic>. It is
<italic>very unlikely</italic> that the AMOC will undergo an abrupt transition or collapse in the
21st century for the scenarios considered (medium confidence). However, if it did occur
such a transition would have very large rapid (decadal timescale) impacts on
the regional climate of the North Atlantic and surrounding continents (high confidence) and
substantial impacts on the climate of regions further afield (medium confidence). (More
quantitative information on impacts could and should be provided.)</p></list-item></list></p>
</sec>
<sec id="Ch1.S3" sec-type="conclusions">
  <title>Concluding remarks</title>
      <p id="d1e264">Some will argue that the WGII report is needed to provide information on
impacts. For detailed information this is certainly the case, but the
general shape of the damage function for a large basket of impacts (Fig. 1)
is insensitive to such details and is all that is needed to justify WGI
providing a much more thorough assessment of relevant scenarios. Other
critics will suggest that for WGI to explicitly identify high-impact scenarios
would constitute scaremongering; this concern is no doubt one
reason why previous WGI reports have focussed so much on the likely range.
But it is misguided (see also Emanuel, 2014). Policymakers need to know
about high-impact scenarios and WGI has a responsibility to contribute its
considerable expertise to making the appropriate assessments.</p>
</sec>

      
      </body>
    <back><notes notes-type="dataavailability">

      <p id="d1e271">No data sets were used in this article.</p>
  </notes><notes notes-type="competinginterests">

      <p id="d1e277">The author was a lead author of the WGI contribution to
the IPCC Fifth Assessment Report and a participant in the scoping meeting
for the Sixth Assessment Report.</p>
  </notes><ack><title>Acknowledgements</title><p id="d1e284">I would like to thank Ed Hawkins for making the figure and for valuable
discussions. I would also like to thank Ted Shepherd and all the reviewers
and referees for their valuable comments, which improved the paper. <?xmltex \hack{\newline}?><?xmltex \hack{\newline}?>
Edited by: Pierre Friedlingstein <?xmltex \hack{\newline}?>
Reviewed by: Francis Zwiers and Stephane Hallegatte</p></ack><ref-list>
    <title>References</title>

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  </ref-list></back>
    <!--<article-title-html>ESD Ideas: a simple proposal to improve the  contribution of IPCC WGI to the assessment  and communication of climate change risks</article-title-html>
<abstract-html><p>The purpose of the Intergovernmental Panel on Climate Change (IPCC) is to
provide policy-relevant assessments of the scientific evidence about climate
change. Policymaking necessarily involves risk assessments, so it is
important that IPCC reports are designed accordingly. This paper proposes a
specific idea, illustrated with examples, to improve the contribution of IPCC
Working Group I to informing climate risk assessments.</p></abstract-html>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
Allen, M. R., Frame, D. J., Huntingford, C., Jones, C.-D.,  Lowe, J. A.
Meinshausen, M., and Meinshausen, N.: Warming caused by cumulative carbon
emissions towards the trillionth tonne, Nature, 458, 1163–1166, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
Collins, M., Knutti, R., Arblaster, J., Dufresne, J.-L., Fichefet, T.,
Friedlingstein, P., Gao, X., Gutowski, W. J., Johns, T., Krinner, G., Shongwe,
M., Tebaldi, C., Weaver, A. J., and Wehner, M.: Long-term Climate Change:
Projections, Com mitments and Irreversibility, in: Climate Change 2013: The
Physical Science Basis. Contribution of Working Group I to the Fifth Assessment
Report of the Intergovernmental Panel on Climate Change, edited by: Stocker, T.
F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels,
A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge,
UK and New York, NY, USA, 2013.
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</mixed-citation></ref-html>
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Hazeleger, W., van den Hurk, B. J. J. M., Min, E., van Oldenborgh, G. J.,
Petersen, A. C., Stainforth, D. A., Vasileiadou, E., and Smith, L. A.: Tales of
future weather, Nat. Clim. Change, 5, 107–113, <a href="https://doi.org/10.1038/nclimate2450" target="_blank">https://doi.org/10.1038/nclimate2450</a>, 2015.
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Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y.,
Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge, UK and
New York, NY, USA, 2013.
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Climate Change, edited by: Field, C. B., Barros, V. R., Dokken, D. J., Mach,
K. J., Mastrandrea, M. D., Bilir, T. E., Chatterjee, M., Ebi, K. L., Estrada,
Y. O., Genova, R. C., Girma, B., Kissel, E. S., Levy, A. N., MacCracken, S.,
Mastrandrea, P. R., and White, L. L., Cambridge University Press, Cambridge,
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assessement, Cambridge University Centre for Science and Policy, Cambridge, 2015.
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<ref-html id="bib1.bib8"><label>8</label><mixed-citation>
Mastrandrea, M. D., Field, C. B., Stocker, T. F., Edenhofer, O., Ebi, K. L.,
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G.-K., Yohe, G. W., and Zwiers, F. W.: Guidance Note for Lead Authors of the
IPCC Fifth Assessment Report on Consistent Treatment of Uncertainties,
Intergovernmental Panel on Climate Change (IPCC), 2010.
</mixed-citation></ref-html>
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Matthews, H. D., Gillett, N. P., Stott, P. A., and Zickfeld, K.: The proportionality
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</mixed-citation></ref-html>
<ref-html id="bib1.bib10"><label>10</label><mixed-citation>
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C., Wilson, R. S., and Arvai, J. L.: Reframing climate change assessments around
risk: recommendations for the US National Climate Assessment, Environ. Res. Lett.,
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