Signal detection in global mean temperatures after “Paris”: an uncertainty and sensitivity analysis
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Published:2018-02-05
Issue:2
Volume:14
Page:139-155
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ISSN:1814-9332
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Container-title:Climate of the Past
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language:en
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Short-container-title:Clim. Past
Author:
Visser Hans, Dangendorf Sönke, van Vuuren Detlef P., Bregman Bram, Petersen Arthur C.ORCID
Abstract
Abstract. In December 2015, 195 countries agreed in Paris to “hold the increase in
global mean surface temperature (GMST) well below 2.0 ∘C
above pre-industrial levels and to pursue efforts to limit the temperature
increase to 1.5 ∘C”. Since large financial flows will be
needed to keep GMSTs below these targets, it is important to know how GMST
has progressed since pre-industrial times. However, the Paris Agreement is
not conclusive as regards methods to calculate it. Should trend progression
be deduced from GCM simulations or from instrumental records by (statistical)
trend methods? Which simulations or GMST datasets should be chosen, and which
trend models? What is “pre-industrial” and, finally, are the Paris targets
formulated for total warming, originating from both natural and anthropogenic
forcing, or do they refer to anthropogenic warming only? To find answers to
these questions we performed an uncertainty and sensitivity analysis where
datasets and model choices have been varied. For all cases we evaluated trend
progression along with uncertainty information. To do so, we analysed four
trend approaches and applied these to the five leading observational GMST
products. We find GMST progression to be largely independent of various trend
model approaches. However, GMST progression is significantly influenced by
the choice of GMST datasets. Uncertainties due to natural variability are
largest in size. As a parallel path, we calculated GMST progression from an
ensemble of 42 GCM simulations. Mean progression derived from GCM-based GMSTs
appears to lie in the range of trend–dataset combinations. A difference
between both approaches appears to be the width of uncertainty bands: GCM
simulations show a much wider spread. Finally, we discuss various choices for
pre-industrial baselines and the role of warming definitions. Based on these
findings we propose an estimate for signal progression in GMSTs since
pre-industrial.
Publisher
Copernicus GmbH
Subject
Paleontology,Stratigraphy,Global and Planetary Change
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