http://www.nature.com/nature/journal/v529/n7585/full/529162a.html
http://www.nature.com/nature/journal/v529/n7585/full/nature16494.html

"The past rapid growth of Northern Hemisphere continental ice sheets, which 
terminated warm and stable climate periods, is generally attributed to reduced 
summer insolation in boreal latitudes. Yet such summer insolation is near to 
its minimum at present, and there are no signs of a new ice age. This 
challenges our understanding of the mechanisms driving glacial cycles and our 
ability to predict the next glacial inception. Here we propose a critical 
functional relationship between boreal summer insolation and global carbon 
dioxide (CO2) concentration, which explains the beginning of the past eight 
glacial cycles and might anticipate future periods of glacial inception. Using 
an ensemble of simulations generated by an Earth system model of intermediate 
complexity constrained by palaeoclimatic data, we suggest that glacial 
inception was narrowly missed before the beginning of the Industrial 
Revolution. The missed inception can be accounted for by the combined effect of 
relatively high late-Holocene CO2 concentrations and the low orbital 
eccentricity of the Earth. Additionally, our analysis suggests that even in the 
absence of human perturbations no substantial build-up of ice sheets would 
occur within the next several thousand years and that the current interglacial 
would probably last for another 50,000 years. However, moderate anthropogenic 
cumulative CO2 emissions of 1,000 to 1,500 gigatonnes of carbon will postpone 
the next glacial inception by at least 100,000 years. Our simulations 
demonstrate that under natural conditions alone the Earth system would be 
expected to remain in the present delicately balanced interglacial climate 
state, steering clear of both large-scale glaciation of the Northern Hemisphere 
and its complete deglaciation, for an unusually long time."

GR- While it is one thing to warm and acidify the planet, it takes some serious 
juju to override the orbital control of glacial-interglacial cycles. While we 
can debate whether this is a good or bad thing and unintentional, is there now 
any doubt about the ability for humans to affect the climate and chemistry of 
the entire planet for many millennia? Given that we are capable of these 
amazing powers, it would seem a small step to figure out how to do this in a 
way that is in the best interest of Earth's inhabitants. 

As to where to start, the prologue by Michael Crucifix provides a clue:"Such 
long-term consequences [of our CO2 emissions] may seem surprising, given that 
the emissions will occur over a few centuries at most and that anthropogenic 
CO2 will eventually be absorbed by the oceans. But for this absorption to 
occur, carbonate minerals in the ocean will need to be dissolved, to counteract 
the increase in ocean acidity that occurs when CO2 is absorbed, and which 
limits the amount of CO2 that can be dissolved. This takes time. In fact, the 
mean half-life of CO2 in the atmosphere is of the order of 35,000 years6. 
Consequently, anthropogenic CO2 will still be in the atmosphere in 50,000 
years' time, and even 100,000 years, which is enough to prevent any glaciation."
GR - So, in addition to figuring out how to reduce emissions, might focussing 
on how to hasten mineral weathering and thus reducing the half life of CO2 in 
the atmosphere be a more obvious starting point, than say asking land biology 
to (unnaturally) do the heavy lifting as advocated by IPCC et al?  Shall we try 
to enhance existing, proven, global scale CO2 capture and sequestration, or try 
to convert biology from a major carbon and nutrient recycler to to a major 
carbon and nutrient storer?  Or worse, shall we place all of our money on a 
completely artificial, costly and risky system that bears no resemblance to 
proven, global scale processes (CCS)?  I'd say its time for a rational 
discussion about the pathways facing us and where to focus our efforts and 
treasure, assuming we decide that warming, acidification and  lack of glacials 
isn't a good thing. 
Greg
https://www.researchgate.net/profile/Greg_Rau


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