Poster's note : relevant to timescales for deployment

http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate3058.html

Role of volcanic and anthropogenic aerosols in the recent global surface
warming slowdown

Doug M. Smith, et al
Nature Climate Change (2016)
doi:10.1038/nclimate3058

Published online 20 June 2016

The rate of global mean surface temperature (GMST) warming has slowed this
century despite the increasing concentrations of greenhouse gases. Climate
model experiments show that this slowdown was largely driven by a negative
phase of the Pacific Decadal Oscillation (PDO), with a smaller external
contribution from solar variability, and volcanic and anthropogenic
aerosols. The prevailing view is that this negative PDO occurred through
internal variability. However, here we show that coupled models from the
Fifth Coupled Model Intercomparison Project robustly simulate a negative
PDO in response to anthropogenic aerosols implying a potentially important
role for external human influences. The recovery from the eruption of Mount
Pinatubo in 1991 also contributed to the slowdown in GMST trends. Our
results suggest that a slowdown in GMST trends could have been predicted in
advance, and that future reduction of anthropogenic aerosol emissions,
particularly from China, would promote a positive PDO and increased GMST
trends over the coming years. Furthermore, the overestimation of the
magnitude of recent warming by models is substantially reduced by using
detection and attribution analysis to rescale their response to external
factors, especially cooling following volcanic eruptions. Improved
understanding of external influences on climate is therefore crucial to
constrain near-term climate predictions.

Subject terms:
Attribution
Projection and prediction

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