Study: climate was more variable during the last inter-glacial period

Does climate vary more from century to century when it is warmer?

Century-scale climate variability was enhanced when the Earth was warmer during the Last Interglacial period (129-116 thousand years ago) compared to the current interglacial (the last 11,700 years), according to a new UCL-led study.

The findings, published today in Nature Communications and funded by the Natural Environment Research Council (NERC) and the Australian Research Council (ARC), reveal that the Last Interglacial period was punctuated by a series of century-scale arid events in southern Europe and cold water-mass expansions in the North Atlantic.

Assessing natural climate variability under relatively warm conditions is crucial to inform projections under future carbon emission scenarios. Professor Chronis Tzedakis (UCL Geography), study lead author, said: “The Last Interglacial is particularly relevant because it provides insights into climate processes during a period of excess warmth.”

The Last Interglacial period contained an interval of intense Arctic warming, with surface air temperatures estimated at 3-11°C above pre-industrial, comparable to high-latitude warming scenarios for the end of this century.

Global sea-level during the Last Interglacial is estimated to have been ~6-9 m above present, with 0.6-3.5 m derived from melting of the Greenland Ice Sheet.

Previously, several North Atlantic and European records have detected century-scale changes in temperature and precipitation within the Last Interglacial, but there has been considerable uncertainty over the timing, extent and origin of these climate oscillations.

This new study by international researchers from twelve institutions used marine and terrestrial geological archives, coupled with climate model experiments, to create the most detailed timeline of ocean and atmosphere changes in the North Atlantic and southern Europe during the Last Interglacial.

To address the uncertainties in comparing records from different environments, researchers produced a “stratigraphic ‘rosetta stone’ by analysing different fossils from the same sediment samples in a marine core off Lisbon,” said Dr Luke Skinner (Cambridge University) who led the palaeoceanographic analyses.

“The marine core also contained pollen transported from the Tagus river into the deep sea, thus enabling a direct comparison of vegetation and North Atlantic ocean changes,” said Dr Vasiliki Margari (UCL Geography), who undertook the pollen analysis.

Changes in vegetation, primarily caused by variations in the amount of rainfall, were then linked to changes in the chemical signature of rainfall recorded in stalagmites from Corchia Cave in northern Italy.

“The Corchia record is particularly important because it is supported by very detailed radiometric dating using the decay of uranium isotopes, producing one of the best chronologies for this period available,” said Dr Russell Drysdale (University of Melbourne), who led the team studying the Italian cave.

Climate model experiments, undertaken by Dr Laurie Menviel and Dr Andrea Taschetto of the University of New South Wales Sydney, revealed that the spatial fingerprint of these changes was consistent with disruptions of the Atlantic meridional overturning circulation.

Greenland ice-melt and runoff as a result of strong high-latitude warming during the Last Interglacial may have contributed to the weakening of the Atlantic meridional overturning circulation and to the observed climate changes.

“Although not a strict analogue for future anthropogenically-driven changes, the profile of the Last Interglacial that emerges is one of enhanced century-scale climate instability, with implications for ice-sheet and ocean dynamics,” said Professor Tzedakis.

“Future research efforts should focus on constraining further the extent of melting and runoff from the Greenland ice-sheet and its effects on ocean circulation during the Last Interglacial.”

###

Source: UNIVERSITY COLLEGE LONDON

The paper: (open access) https://www.nature.com/articles/s41467-018-06683-3

Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial

Abstract

Considerable ambiguity remains over the extent and nature of millennial/centennial-scale climate instability during the Last Interglacial (LIG). Here we analyse marine and terrestrial proxies from a deep-sea sediment sequence on the Portuguese Margin and combine results with an intensively dated Italian speleothem record and climate-model experiments. The strongest expression of climate variability occurred during the transitions into and out of the LIG. Our records also document a series of multi-centennial intra-interglacial arid events in southern Europe, coherent with cold water-mass expansions in the North Atlantic. The spatial and temporal fingerprints of these changes indicate a reorganization of ocean surface circulation, consistent with low-intensity disruptions of the Atlantic meridional overturning circulation (AMOC). The amplitude of this LIG variability is greater than that observed in Holocene records. Episodic Greenland ice melt and runoff as a result of excess warmth may have contributed to AMOC weakening and increased climate instability throughout the LIG.

 

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Steve Keohane
October 12, 2018 8:21 am

So non-anthropogenic warming is more extreme than anthropogenic warming, oh my!

Editor
Reply to  Steve Keohane
October 12, 2018 8:57 am

Took the words right out of my mouth, Steve.

Regards.
Bob

Gums
Reply to  Bob Tisdale
October 12, 2018 3:23 pm

Not only that, but maybe there folks will try to separate natural forcing from human forcing when playing with their models.
Gums sends…

john
Reply to  Steve Keohane
October 12, 2018 10:08 am

We need to try harder! CO2 isn’t working.
More cow farts! I need more cow farts!

Reply to  john
October 14, 2018 1:30 pm

Yeah, but not right in my face.
My cat’s farts are pl3enty aromatic enough, thank you.

Auto

Reply to  auto
October 14, 2018 1:32 pm

‘plenty’ – sorry.

auto

Reply to  Steve Keohane
October 12, 2018 11:40 am

Also my thoughts. Natural range exceeded current interglacial range. So how is the control of CO2 so powerful when we get O.8 Degrees in 288 for a sudden 40% rise in CO2, then? Nothing to see here, never mind pretend to avoid based on no evidence of a real effect that exceeds natural causes. Just saying.

Papa J Picolino
Reply to  Steve Keohane
October 12, 2018 9:08 pm

This is possible. It might be that human land use has a stabilizing effect on climate.

Richard
Reply to  Steve Keohane
October 13, 2018 7:05 pm

That’s worse than even a pessimist such as I could imagine.

Bruce Cobb
October 12, 2018 9:07 am

Yawners. Another lame-o attempt by pseudoscientists to connect previous warm periods to today’s “carbon-enhanced” warming. Next.

Gary
Reply to  Bruce Cobb
October 12, 2018 9:48 am

This cynical comment is unfair and inaccurate. The authors have taken great care to collect, sample, and analyze proxy data from the last interglacial from a high resolution sediment core. Read the methods section; “pseudoscientists” don’t work like this.

On the premise that the last interglacial period could be an analog for the current one, understanding it is valuable for comparison.

Reply to  Gary
October 12, 2018 10:17 am

That premise and the touting of “excess warmth” invite cynicism.

Bruce Cobb
Reply to  Gary
October 12, 2018 10:19 am

The proof is in the pudding:

Assessing natural climate variability under relatively warm conditions is crucial to inform projections under future carbon emission scenarios. Professor Chronis Tzedakis (UCL Geography), study lead author, said: “The Last Interglacial is particularly relevant because it provides insights into climate processes during a period of excess warmth.”

And

“Although not a strict analogue for future anthropogenically-driven changes, the profile of the Last Interglacial that emerges is one of enhanced century-scale climate instability, with implications for ice-sheet and ocean dynamics,” said Professor Tzedakis.

Definitely an agenda there.

GeologyJim
Reply to  Bruce Cobb
October 12, 2018 10:31 am

My thoughts exactly. The “analogue for future anthropogenically driven changes” falls apart because of the ice-core data not mentioned in this study. We have known for more than 20 years that detailed isotopic measurements from ice cores show that T changes 400-800 years before CO2 follows along. Temp is the dog and CO2 is the tail

I give them credit for doing some really detailed measurements from the sediment cores and careful correlation with the cave speleothem record. Good confirmation that the Earth determines its own climatic variations without assistance from us.

Reply to  Bruce Cobb
October 12, 2018 11:31 am

They invoke the ‘state-of-the-art’ pseudo-argument for models, as if they are ‘state-of-the-art’ they actually work. They call the garbage models exponentially amplifying garbage inputs as ‘experiments’. That’s an agenda plain and simple. Also a religion, a blind belief in the crystal globe that shows hallucinations. State-of-the-art garbage hallucinations.

INGIMUNDUR S KJARVAL
Reply to  Bruce Cobb
October 12, 2018 4:21 pm

Be understanding, without funding no future research. Nobody wants to end up like us, excommunicated and expelled.

Very interesting, says “129-116 thousand years ago” or 13 thousand years, ours 11.700 years. Does that mean we have about 1300 years?

LdB
Reply to  INGIMUNDUR S KJARVAL
October 12, 2018 8:32 pm

No you have 12 years the IPCC said so 🙂

Latitude
October 12, 2018 9:11 am

so as we continue to ride down the hump….weather should get better

http://jonova.s3.amazonaws.com/graphs/lappi/gisp-last-10000-new.png

Steven Fraser
October 12, 2018 9:19 am

Nice pic of the Taku Glacier, I think…

tty
Reply to  Steven Fraser
October 12, 2018 12:26 pm

Nope.

The Perito Moreno glacier in Patagonia. That is a southern beech in the foreground.

John Tillman
Reply to  tty
October 12, 2018 12:39 pm

Which big Argentine Andean glacier is growing, despite its frequent ice dam ruptures in its terminal lake.

Likewise the Chilean glacier Pio XI (aka Brueggen), largest in the SH outside of Antarctica. Patagonia is one of the regions with mainly growing glaciers.

S
Reply to  John Tillman
October 12, 2018 2:00 pm

Ok, I see where the picture comes from now. I was looking at the water, the Ice and the snowcapped mountains, and not the flora.

Its a beautiful sight. Thanks for the tip.

feed berple
October 12, 2018 9:19 am

Just because the climate 130k years ago was different doesn’t make it more variable. Century scale events argue that it was less variable.

Reply to  feed berple
October 13, 2018 8:42 am

Yes, and the 13C and 18O profiles in their benchmark cave show opposite trends before 130kya and then suddenly come into accordance. Quite peculiar. The cave seems very regular at 1mm deposition every thousand years.

observa
October 12, 2018 9:22 am

You mean to tell me that the rocks at Hallett Cove in South Australia that can show 130M sea level rise over 8000 years means the sea level mightn’t have risen the average 16.25mm a year for all those years? It might have been only 16mm for one decade and then 16.5mm for another? Well I’ll be…! Gaia sure can be a capricious creature sometimes.

Walter Sobchak
Reply to  observa
October 12, 2018 12:47 pm

We are going to Italy next week . One of our stops will be Ravenna where there are several ancient churches with mosaics from the Byzantine era 1400 years ago. At the time the Churches were built Ravenna was a sea port. It is now 5 miles from the Adriatic.

commieBob
October 12, 2018 9:26 am

Some time in the late 1970s a visiting scholar pointed out that the climate in the last 10,000 years has been abnormally stable. This has enabled agriculture and civilization as we know it to develop.

The good thing now is that our resources for dealing with an unstable climate are orders of magnitude better than our ancestors had.

ferd berple
October 12, 2018 9:26 am

I expect climate 130k years ago had 1/f variability just like our present climate.

The longer you watch the more likely you are to see an extreme event.

This makes people mistakenly assume the climate is getting worse. In reality the climate is unchanged. What is changing is the length of your sample.

Richard M
October 12, 2018 9:49 am

So, they admit the oceans can drive major changes in climate.

“The spatial and temporal fingerprints of these changes indicate a reorganization of ocean surface circulation”

Now, if only they would apply that knowledge to recent history.

October 12, 2018 10:12 am

As usual, my takeaway is different than the intended one for paleoclimate papers. So, the previous interglacial had Arctic temps up to 11C above temperature projections for 2100 based on pre-industrial levels. Ooookay, so then what happened with this colossal warming? Err…we slipped into another 100,000yr glacial period!!!

What this study is really trying to tell these geographer types is that: heat-shmeat, we are going to freeze our asses off eventually anyway as real big climate takes hold.

Jeff Alberts
Reply to  Gary Pearse
October 12, 2018 4:40 pm

“As usual, my takeaway is different than the intended one for paleoclimate papers. So, the previous interglacial had Arctic temps up to 11C above temperature projections for 2100 based on pre-industrial levels. Ooookay, so then what happened with this colossal warming? Err…we slipped into another 100,000yr glacial period!!!”

It also means there is no tipping point with respect to runaway heat.

Loren Wilson
Reply to  Gary Pearse
October 13, 2018 7:54 am

Agreed, and also – yet we are still here. No tipping point!

AGW is not Science
October 12, 2018 10:24 am

“Assessing natural climate variability under relatively warm conditions is crucial to hyping baseless, bullshit projections about future carbon emission scenarios.”

There, fixed it for ’em.

“Professor Chronis Tzedakis (UCL Geography), study lead author, said: “The Last Interglacial is particularly relevant because it provides insights into climate processes during a period of excess warmth.””

“EXCESS warmth?! The climate is what it is, and the ridiculous assertion that any climate different than the (if anything) anomalously COLD current climate constitutes an “EXCESS” of warmth exposes this as not “science,” but “activism.”

Of course, I knew that as soon as I saw it was published in “Nature PROPAGANDA, er… COMMUNICATIONS.”

Earthling2
October 12, 2018 10:25 am

We can’t even agree on what the actual temperatures were just 150 years ago in any detail for much of the planet when my great grandparents were alive. What likelihood is there that a few proxies here, a few proxies there, has any actual validity as to what was actually happening in any detail 125,000 years ago? The more I learn about modern day climate science, the more suspect I am about what actually happened in any detail with regards to the distant past. Maybe in very wide generalities.

I think we put far too much faith in science and just accept blindly without much evidence what we are told happened so long ago, because of ‘experts’ who declare something. The deceit in modern day climate science as expressed by those with an agenda and socio economic designs on humanity and politics just taint my understanding of many other branches of ‘soft’ sciences now.

Jeff Alberts
Reply to  Earthling2
October 12, 2018 4:42 pm

“We can’t even agree on what the actual temperatures were just 150 years ago in any detail for much of the planet when my great grandparents were alive. What likelihood is there that a few proxies here, a few proxies there, has any actual validity as to what was actually happening in any detail 125,000 years ago?”

Proxies are SWAGS, nothing more. Even ice core data, which supposedly show that CO2 lags temp by ~800 years is probably pretty far off.

Earthling2
Reply to  Jeff Alberts
October 13, 2018 6:33 am

Had to look that one up…lol SWAG…Scientific Wild Ass Guess

TonyL
October 12, 2018 10:37 am

Is there anything good about this paper?
No, not a rhetorical question. If we filter out all the obligatory Global Warming BS, is there any good data underneath?
They make quite the claim, that the last interglacial was more variable than the current one. Then they say:
“The strongest expression of climate variability occurred during the transitions into and out of the LIG.”

Well, we know that transitions into and out of interglacials are marked by what we would call extreme variability. We also expect that the warmer it is, the less variability there is, due to the lessened temperature difference between the equator and the poles. Did they then use a model to “homogenize” the variability from the ends of the interglacial into the middle, more stable portion?
With all this aside, there is probably some good paleo data here, if indeed it is new, and not just another “reanalysis”.

tty
Reply to  TonyL
October 12, 2018 12:04 pm

“is there any good data underneath?”

Yes, but there is no new data. This has all been well known for at least a decade. If you read the paper you will notice that these cold intervals already have generally accepted stratigraphic names: C24 to C28 (“Cold 24” to “Cold 28”). I’m not sure when they were introduced, but at it must be at least 15 years ago.

TonyL
Reply to  tty
October 12, 2018 1:17 pm

Thanks for the extra info.

AGW is not Science
October 12, 2018 10:38 am

““Although not a strict analogue for future anthropogenically-driven changes,”

Objection! Assumes bullshit (anthropogenically-driven changes) to be fact.

“the profile of the Last Interglacial that emerges is one of enhanced century-scale climate instability, with implications for ice-sheet and ocean dynamics,” said Professor Tzedakis.”

So climate is more stable now than in the past when they can’t possibly blame it on fossil fuel use. Interesting how whatever they find, it always is used to perpetrate the “human-induced catastrophe” nonsense.

What I get from this is the climate is far more variable, both in terms of the temperatures at any point in time and the variability of “climate” in all its components, than we are experiencing today. Which means they can pound all their claims of anything “unprecedented” going on where the sun doesn’t shine.

donb
October 12, 2018 10:51 am

Conclusion not surprising. From Antarctica ice core data: Temperature increased above today’s ~131 kyr ago; peaked several degrees above today’s ~128 kyr ago; decreased several degrees; then increased ~124 kyr ago; then steadily decreased into the glaciation. Depending on the ice core, polar temperature was above today’s for ~10 kyr.
By contrast, temperature over past ~8 kyr of the Holocene has been a slow decrease, without the variations apparent in Eemian ice core data.

ironocman
Reply to  donb
October 12, 2018 4:36 pm

Perhaps the Younger Dryas meteor impact put a damper on the Holocene, producing a slower decrease.

From a philosophical point of view I wonder if civilisation could have evolved under any other circumstances.

M.W.Plia
October 12, 2018 10:58 am

I remember reading, about 3 decades ago, a very interesting article in the Toronto Star about the “Sangamonian Interglacial”. Climate zone boundaries were discovered to be much further north than their current positions as their was tremendously abundant evidence indicating it was much warmer then than now.

Given the academic climate community’s expressed concern on the current “warming” why would a newspaper of such standing (among others) not report on this now?

tty
Reply to  M.W.Plia
October 12, 2018 11:53 am

It is perfectly well known that the Sangamonian/Eemian interglacial was much warmer (up to 10 degrees C in the Arctic) without any catastrophic effects (e. g. no methane release as the permafrost melted).

However it is definitely not mentioned in MSM nowadays.

taxed
October 12, 2018 11:17 am

The key takeaway point from this study is to understand how weather interacts with climate. Because if the climate was more variable during the last LIG then that means the weather patterns were more static during the LIG.
In order to get stable climate there needs to be highly variable weather as this is the cause of a stable climate because it avoids the extremes in climate from forming. So the climate becoming more arid in southern europe during these events, meant the weather had became more prone to blocking in this area and so deducing the amount of rainfall that took place. So the take home point from this study is that the weather patterning was more prone to become static during the LIG over the area in question in this study then it is current warm period.

jim hogg
October 12, 2018 11:22 am

Assuming the data is accurate, that it has been interpreted effectively and that there are no relevant unknowns (always a consideration) that might render the study useless, there appears to be something in this study for everyone:

CAGW adherents can show evidence of raised sea levels (with all the appropriate implications) and more, related to higher temperatures, and,

sceptics can point out that higher temperatures than those we’re experiencing and we’re being warned to expect, somehow occurred without fossil fuel users lending a hand. What’s not to like . . ?

This one appears to be worthy of some very close examination.

John Mason
October 12, 2018 11:30 am

I find it amazing that an article such as this has as its purpose to know what we might be in for in this supposed era of human induced warming while at the same time this article proves that natural cycles dwarf any human influence.

I’m looking for a wall to bang my head against.

Anthony Banton
Reply to  John Mason
October 12, 2018 12:02 pm

“Climate model experiments, undertaken by Dr Laurie Menviel and Dr Andrea Taschetto of the University of New South Wales Sydney, revealed that the spatial fingerprint of these changes was consistent with disruptions of the Atlantic meridional overturning circulation.”

First off “Climate model experiments” …. they are OK are they now ?

Do we have any “disruptions of the Atlantic meridional overturning circulation” identified in the Holocene?
This study ….

Says:
“Abrupt changes in climate have occurred in many locations around the globe over the last glacial cycle, with pronounced temperature swings on timescales of decades or less in the North Atlantic. The global pattern of these changes suggests that they reflect variability in the Atlantic meridional overturning circulation (AMOC). This review examines the evidence from ocean sediments for ocean circulation change over these abrupt events. The evidence for changes in the strength and structure of the AMOC associated with the Younger Dryas and many of the Heinrich events is strong. Although it has been difficult to directly document changes in the AMOC over the relatively short Dansgaard-Oeschger events, there is recent evidence supporting AMOC changes over most of these oscillations as well. The lack of direct evidence for circulation changes over the shortest events leaves open the possibility of other driving mechanisms for millennial-scale climate variability.”

So plenty of changes in the Holocene too … as should be expected in a transition out of Glaciation.

None of which invalidates warming due to anthro increases in GHGs over the last ~150 years – the forcing of which only really overcame -ve natural ones (>1 W/m^2) in the 1970’s – and then interrupted by several volcanic aerosol events …..

comment image

tty
Reply to  Anthony Banton
October 12, 2018 12:09 pm

The difficulty in explaining those coolings as being due excessive melting of Greenland ice is that there is very strong evidence that arctic ice caps grew, not melted, while they were happening:

https://www.researchgate.net/publication/320750356_Eemian_estuarine_record_forced_by_glacio-isostasy_S_Iceland_-_link_with_Greenland_and_deep_sea_records

tty
October 12, 2018 11:49 am

I would say this is a pretty clear case of agenda science.

It has been clear for quite some time that there were marked cold/dry oscillations in the early Eemian, at least in the North Atlantic area. Note that all these ‘newly discovered’ cold intervals already have generally used and accepted stratigraphic names (C24 to C28)

Here is a ten year old paper with well-nigh identical results but without the CAGW flourishes:

https://www.whoi.edu/fileserver.do?id=23643&pt=2&p=18528

However that these cold episodes were due to “Greenland ice-melt and runoff“ is patently ridiculous since sea level declined during the cold intervals and arctic ice grew not melted. Which is hardly unexpected by the way:

https://www.researchgate.net/publication/320750356_Eemian_estuarine_record_forced_by_glacio-isostasy_S_Iceland_-_link_with_Greenland_and_deep_sea_records

And it is depressing to see that “6-9 meter sea-level rise” being hauled out again and again. It is a AGW factoid with essentially no factual support. Actual study of tectonically stable last interglacial coastlines suggest about 4-5 meters is more likely:

https://www.researchgate.net/publication/322843264_The_last_interglacial_MIS_5e_sea_level_highstand_from_a_tectonically_stable_far-field_setting_Yorke_Peninsula_southern_Australia
https://www.researchgate.net/publication/228565750_Relative_sea-level_fall_since_the_last_interglacial_stage_Are_coasts_uplifting_worldwide

Why is this important for CAGW? Because it is essentially impossible to suggest “collapse” of the West Antarctic ice-sheet with less than about 7 meters sea-level rise.

Anthony Banton
October 12, 2018 12:05 pm
John Tillman
Reply to  Anthony Banton
October 12, 2018 12:29 pm

Anthony,

That study concerns the last glacial interval, not the Eemian interglacial which preceded it.

D/O and Heinrich events during glacial phases might share some causes with Bond cycles during interglacials, but the magnitude of warm and cold snaps is larger during glacials.

Heinrich events, ie armadas of icebergs released into the North Atlantic, associated with the coldest interval during glaciations, might be caused by ice shelf collapses (as perhaps off Labrador), or some other surge of land ice into the ocean, as from the outlet to Hudson Bay under the Laurentide Ice Sheet or similar outlets on the other side of the Atlantic. When the freshwater from these bergs melts, it puts a lid of cool, less saline water over the North Atlantic, easing sea ice formation and affecting circulation patterns.

tty
Reply to  John Tillman
October 12, 2018 12:36 pm

Or it might be the other way around. Changes in ocean circulation might destabilize ice shelves. Or it might be secular changes in tidal amplitudes that does it.

John Tillman
Reply to  tty
October 12, 2018 12:41 pm

Hope we don’t have to wait for the next ice sheet advance to figure out what causes HEs.

John Tillman
Reply to  John Tillman
October 12, 2018 12:47 pm

To me, they look like icy versions of the cold meltwater events during deglaciation which probably caused the YD and 8.2 Ka cold snaps.

It’s remarkable how icy was the North Atlantic during the Last Glacial Maximum and other of the coldest stadials. This, combined with much lower sea level, spawned the Solutrean hypothesis to explain the (much later) Clovis Culture in North America.

MarkW
October 12, 2018 12:14 pm

“Century-scale climate variability was enhanced when the Earth was warmer during the Last Interglacial period (129-116 thousand years ago) compared to the current interglacial (the last 11,700 years), according to a new UCL-led study.”

That’s impossible. CO2 was lower during the last interglacial so the temperature had to have been lower.
That’s what the models say and models are never wrong. (Genuflect towards the computer)

old construction worker
Reply to  MarkW
October 13, 2018 2:25 am

‘That’s impossible. CO2 was lower during the last interglacial so the temperature had to have been lower.
That’s what the models say and models are never wrong. (Genuflect towards the computer)’ But, ‘This Time It’s Different” don’t cha know.

Samuel C Cogar
October 12, 2018 12:24 pm

Excerpted from published commentary:

Century-scale climate variability was enhanced when the Earth was warmer during the Last Interglacial period (129-116 thousand years ago) compared to the current interglacial.

The Last Interglacial period contained an interval of intense Arctic warming, with surface air temperatures estimated at 3-11°C above pre-industrial, comparable to high-latitude warming scenarios for the end of this century.

But, but, but, …… just prior to the Last Interglacial period (129-116 thousand years ago) atmospheric CO2 was below 200 ppm …… and then the CO2 increased to about 280 ppm for a short time as the Interglacial temperatures increased …… and then began its decline down to about 180 ppm (see following proxy graph) at the Last Glacial Maximum at 21,000 YBP.

CO2 proxy graph for the past 800,000 years
comment image

So geeeeeze, …… given the fact that there were not tens-of-millions of humans burning fossil fuels during the past Interglacial, …… just what caused that high-latitude temperature increase of 3-11°C?

Was the “cause” the same as it was for the 2.5° to 7.0°C “warmer-than-modern” high-latitude temperatures that occurred during the current Interglacial, ….. between 9,000 and 7,000 YBP?

tty
Reply to  Samuel C Cogar
October 12, 2018 12:31 pm

“Yes”

In both cases it was the sun of course. More sun at higher northern latitudes due to orbital changes.

CO2 just tails along. About 800 years later at the beginning of an interglacial and about 5,000 years later at the end.

Peta of Newark
October 12, 2018 12:39 pm

Just quickly and as best I can, they are saying (estimated most of the time) that The Main Action happened towards the end of the interglacial. Circa 115ky ago.
Main action being the extended droughts and decline of the trees and presumably the ‘interval’ of (estimated) 11 degC warmth.
And all along, no mention of what actually caused anything. All they have is a list of occurrences and the reader is left to puzzle out what happened. Aided and prodded into a particular Conclusion Jump with talk of something similar happening now.

The dirt did it.
It wore out, got weathered and eroded and washed out to sea. Or blew away and mostly landed in the sea.

Surely, extended droughts, big temperature variations tell of a big desert coming into existence. The dirt was wearing out, the trees were struggling and catching fire. Like SoCal now.
Once they start burning, that is it. End Game. Desert.

And deserts are cold places. Maybe have high temperatures at mid-day but have next to zero heat storage. No thermal inertia. No trapped heat. haha.
And once the desert extends far enough North, winter ice & snow melt later and later in the year, effectively creeping South.
Enter the Ice Age.

And they tell us that when they say xyz all occurred barely 1,000 years before the ice cover was complete.

Warmists really do want to be careful with what they wish for. Their assertion, that everyone becoming vegetarian will slow climate change, is flat out wrong.
Why.
Because they are asking farmers to accelerate the rate of soil erosion growing these veggies.
The buffalo knew how to manage dirt, as did the people who lived with them.
Did anyone ask (what’s left of) them?

And we know that farming is eroding the soil – Global Greening is in part** caused by dust coming off dry farmland (rich in potash & phosphate) landing on places that have never known the stuff in such quantities.
**In part because nitrogen and sulphur oxides do the rest.

And their blind insanity is complete with the assertion that burning biomass will be a saviour also.
It’s impossible to be more wrong.

Richard
October 12, 2018 2:00 pm

“Century-scale climate variability was enhanced when the Earth was warmer during the Last Interglacial period (129-116 thousand years ago) compared to the current interglacial (the last 11,700 years), according to a new UCL-led study.”
University College London
But here we are being told that all our variability is entirely due to us. And we can fully control our climate.