A major conundrum in climate science is how to account for dependence between climate
models. This complicates interpretation of probabilistic projections derived from such
models. Here we show that this problem can be addressed using a novel method to test
multiple non-exclusive hypotheses, and to make predictions under such hypotheses. We
apply the method to probabilistically estimate the level of global warming needed for a
September ice-free Arctic, using an ensemble of historical and representative concentration
pathway 8.5 emissions scenario climate model runs. We show that not accounting for model
dependence can lead to biased projections. Incorporating more constraints on models may
minimize the impact of neglecting model non-exclusivity. Most likely, September Arctic sea
ice will effectively disappear at between approximately 2 and 2.5 K of global warming. Yet,
limiting the warming to 1.5 K under the Paris agreement may not be sufficient to prevent the
ice-free Arctic.
Key Figure
Figure 4. Probability density functions (pdfs) of global mean surface
temperature change required for September Arctic sea ice to effectively
vanish. a Pdfs for runs with and without interactions (to illustrate the
effects of accounting for model interactions). b Pdfs from all runs
accounting for interactions, to illustrate the impact of different
assumptions. Vertical dotted line: lower desirable warming limit of 1.5°
under the Paris agreement. The projections are sensitive to the datasets
used, and to the assumptions about the cause of the recent Arctic sea ice
decline. There is a distinct probability that keeping global warming below
the 1.5° target of the Paris agreement may not be enough to stave off an
essential disappearance of summer Arctic sea ice. The figure illustrates
the capacity of the method to make predictions of a variable of interest
conditioned on a set of non-exclusive hypotheses while accounting for all
orders of hypothesis interactions
This page is maintained by Jason Evans |
Last updated 23 January 2018