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C equilibrium climate sensitivity), the diagnosis is 2.07 W m-2 K-1 (about 1.8 deg. If I add in some time-varying radiative forcing like we have addressed in our recent papers (e.g.
Our most complete analysis of the effect was described here.
BACKGROUND It’s been quite a while since I’ve discussed why the diagnosis of feedbacks in the climate system (and thus climate sensitivity) from observations is biased toward high climate sensitivity.
It’s a controversial topic, one which we have a few published papers on, yet one I am more firmly convinced about than any other climate research I have ever published.
I answer questions submitted by email ONLY (I do not do telephone Q&A), and I never give free private answers.
"When you email me, I own it." The price of the information I give is that it is given only in this public forum. No information you provide through this website shall be deemed confidential.
I’m pretty convinced that most of our detractors on the subject don’t even know what we are talking about.