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Will Howard's avatar

Historical contribution of aerosols to radiative forcing remains the largest source of uncertainty in IPCC syntheses. See: https://www.ipcc.ch/report/ar6/wg1/figures/technical-summary/figure-ts-15/

In particular the kind of cloud-aerosol interactions Jim is concerned about. Given the far shorter mean lifetimes of most aerosols, compared to anthropogenic CO2, changes in their forcing could act faster than changes to CO2 emissions, as Quico notes.

I know and respect Jim Hansen. Most people in the climate science community have a lot of respect for him. You can agree or disagree but I would never dismiss Jim's concerns out of hand.

A 5-degree warmer would be a different planet from the one we inhabit now. Consider the transition from the Last Glacial Maximum included a warming of ~5 degrees (estimates vary). That was over a far longer time scale than the current anthropogenic perturbation. Uncertainty "bars" (however derived) have two ends. Prudent risk management should consider the implications of both ends.

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Robert Tulip's avatar

The precautionary principle means restoring planetary albedo should be the top climate priority, walking back from the heat precipice of tipping points.

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