I agree about such disagreement. And thank you for replying offering clarifications. An attitude to be emulated.
About clarifications, just one, if by saying «
we are looking at a tripling (at least) of pre-industrial CO2 ratios (~750-1000ppm), and conditions that have not been seen since mammals have been the dominant major forms of life on this planet.» you were implying in any way or measure that our planet is going to show that moment or a few decades after that moment the climate it experienced during such ancient eras.
In general, it is my understanding* that full climate equilibration to factors such as CO2 forcing require several centuries or more before the various climate elements are stabilized at the current level. This is why there are two measures of climate sensitivity to such issues, short-term and longer-term sensitivities. If you are asking me if I expect the general climate to reflect prehistoric climate episodes in the past that were slowly and naturally equilibrated to such levels as soon (or even shortly thereafter) as the modern climate forcings touch upon those prehistoric markers, the answer is, "no." Nor do I believe such was implicit in my statements which contain the qualification that:
...For instance, it is important to understand that even if we could stop all human-sourced emissions tomorrow, the atmospheric changes are already set much higher than the system has equilibrated to as of yet. In other words, if we stopped tomorrow, temperatures and climate changes will continue to occur for several more centuries before all of the feed back systems have brought the climate response up to the forcing level of the GHGs in the atmosphere...
...If this is not what you are asking me, please clarify your question.
*References for climate sensitivity and equilibration for atmospheric CO2:
"Global Warming: The Science of Climate Change - Climate Sensitivity"
Dept. of Geophysical Sciences, University of Chicago - Professor David Archer
(4:38 sec. video lecture clip)
http://www.kaltura.com/index.php/ex...f_id/20652192/entry_id/1_y7pofyu4/embed/auto?
"High Earth-system climate sensitivity determined from Pliocene carbon dioxide concentrations" - Mark Pagani, Zhonghui Liu, Jonathan LaRiviere and Ana Christina Ravelo (full paper available at -
http://people.earth.yale.edu/sites/default/files/files/Pagani/1_2009 Pagani_NatureGeosci.pdf)
abstract - Climate sensitivity—the mean global temperature response
to a doubling of atmospheric CO2 concentrations through radiative forcing and associated feedbacks—is estimated at 1.5–4.5°C (ref. 1). However, this value incorporates only relatively rapid feedbacks such as changes in atmospheric
water vapour concentrations, and the distributions of sea ice, clouds and aerosols. Earth-system climate sensitivity, by contrast, additionally includes the effects of long-term feedbacks such as changes in continental ice-sheet extent, terrestrial ecosystems and the production of greenhouse gases other than CO2. Here we reconstruct atmospheric carbon dioxide concentrations for the early and middle Pliocene, when temperatures were about 3–4°C warmer than preindustrial values, to estimate Earth-system climate sensitivity from a
fully equilibrated state of the planet. We demonstrate that only a relatively small rise in atmospheric CO2 levels was associated with substantial global warming about 4.5 million years ago, and that CO2 levels at peak temperatures were between about 365 and 415 ppm. We conclude that the Earth-system climate sensitivity has been significantly higher over the past five
million years than estimated from fast feedbacks alone.
"Millennial Atmospheric Lifetime of Anthropogenic CO2" - David Archer,
Victor Brovkin (full paper available at -
http://link.springer.com/article/10.1007/s10584-008-9413-1)
Abstract - The notion is pervasive in the climate science community and in the public at large that the climate impacts of fossil fuel CO2 release will only persist for a few centuries. This conclusion has no basis in theory or models of the atmosphere / ocean carbon cycle, which we review here. Although the models vary widely in their formulation and underlying assumptions, they are quite consistent in their prediction that release of fossil
fuel CO2 will impact climate for tens of millennia and longer into the future, subsiding on time scales typically associated with nuclear waste. Many slowly-responding components of the climate system, such as ice sheets, deep ocean temperature, permafrost, and methane hydrates, will be sensitive to the long tail of the CO2 climate impact. Most of the CO2 drawdown will take place on time scales of centuries, as CO2 invades the ocean, but it is too simplistic to call the invasion timescale the atmospheric lifetime of the CO2, as is commonly done in popular and scientific discussion. We argue that a better shorthand for the lifetime of anthropogenic CO2 would be "hundreds of years
plus a significant fraction that changes climate forever".
(I just noticed that this abstract is from a copy of the pre-publication paper that I have, the published abstract is a touch different and I am including it as it is on the published paper which appears at the above link -
" Abstract - The notion is pervasive in the climate science community and in the public at large that the climate impacts of fossil fuel CO2 release will only persist for a few centuries. This conclusion has no basis in theory or models of the atmosphere/ocean carbon cycle, which we review here. The largest fraction of the CO2 recovery will take place on time scales of centuries, as CO2 invades the ocean, but a significant fraction of the fossil fuel CO2, ranging in published models in the literature from 20–60%, remains airborne for a thousand years or longer. Ultimate recovery takes place on time scales of hundreds of thousands of years, a geologic longevity typically associated in public perceptions with nuclear waste. The glacial/interglacial climate cycles demonstrate that ice sheets and sea level respond dramatically to millennial-timescale changes in climate forcing. There are also potential positive feedbacks in the carbon cycle, including methane hydrates in the ocean, and peat frozen in permafrost, that are most sensitive to the long tail of the fossil fuel CO2 in the atmosphere."
I include both versions as they are a reflection of the authors' original findings and the modifications that are presumably tied to the science/editorial review that is a part of journal publication.)