Global warming in the pipeline
Improved knowledge of glacial-to-interglacial global temperature change implies that fast-feedback equilibrium climate sensitivity (ECS) is 1.2 +/- 0.3{\deg}C (2$\sigma$) per W/m$^2$. Consistent analysis of temperature over the full Cenozoic era -- including "slow" feedbacks by ice sheets...
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Zusammenfassung: | Improved knowledge of glacial-to-interglacial global temperature change
implies that fast-feedback equilibrium climate sensitivity (ECS) is 1.2 +/-
0.3{\deg}C (2$\sigma$) per W/m$^2$. Consistent analysis of temperature over the
full Cenozoic era -- including "slow" feedbacks by ice sheets and trace gases
-- supports this ECS and implies that CO$_2$ was about 300 ppm in the Pliocene
and 400 ppm at transition to a nearly ice-free planet, thus exposing
unrealistic lethargy of ice sheet models. Equilibrium global warming including
slow feedbacks for today's human-made greenhouse gas (GHG) climate forcing (4.1
W/m$^2$) is 10{\deg}C, reduced to 8{\deg}C by today's aerosols. Decline of
aerosol emissions since 2010 should increase the 1970-2010 global warming rate
of 0.18{\deg}C per decade to a post-2010 rate of at least 0.27{\deg}C per
decade. Under the current geopolitical approach to GHG emissions, global
warming will likely pierce the 1.5{\deg}C ceiling in the 2020s and 2{\deg}C
before 2050. Impacts on people and nature will accelerate as global warming
pumps up hydrologic extremes. The enormity of consequences demands a return to
Holocene-level global temperature. Required actions include: 1) a global
increasing price on GHG emissions, 2) East-West cooperation in a way that
accommodates developing world needs, and 3) intervention with Earth's radiation
imbalance to phase down today's massive human-made "geo-transformation" of
Earth's climate. These changes will not happen with the current geopolitical
approach, but current political crises present an opportunity for reset,
especially if young people can grasp their situation. |
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DOI: | 10.48550/arxiv.2212.04474 |