How Did Earth Get Its Long-Standing Stable Climate?

How Did Earth Get Its Long-Standing Stable Climate?

In last week’s blog1 I described how a careful reconstruction of temperature proxies at sites all over the world revealed that the climate stability humans have enjoyed over the past 9,500 years was about twice as stable as scientists had previously concluded. That is, we are twice as blessed as we had previously thought. Thanks to the extreme climate stability of the past 9,500 years, we have been successful in launching and sustaining global high-technology civilization and in building our population up to seven billion individuals.

I stated last week that I would describe in this blog the new discoveries that explain how we got such a long period of extreme climate stability. I now realize that I cannot do justice to all these discoveries in one blog. This blog is the first of two describing the miraculous designs of Earth’s recent history that gave us the remarkable gift of extreme climate stability in the midst of an ice age cycle.

As I briefly summarized in last week’s blog and describe in much more detail in my book, Improbable Planet,2 it is nothing short of a miracle that we have had such a long period of extreme climate stability at the optimal temperature for global high-technology civilization. Making the climate stability epoch all the more miraculous is that it occurred and is occurring in the midst of an ice age cycle. As I explained in last week’s blog, the ice age cycle drives extreme climate instability, not the opposite (stability). In fact, the past 2.588 to 0.009 million years ago has seen the greatest continuous climate instability in the entire 4.566-million-year history of Earth.

Now, thanks to a new discovery and a long-known temperature anomaly that occurred just previous to the 9,500-year epoch of extreme climate stability, scientists may be close to understanding how such an epoch came about. To put that anomaly and the new discovery in context, it is important to understand the nature of the ice age cycle.

Ice Age Cycle
Earth’s ice age cycle has persisted throughout the past 2.588 million years. For all but the last 800,000 years of that cycle the period has been 41,000 years. This 41,000-year periodicity was driven by the 41,000-year cycle of variation in the tilt of Earth’s rotation axis.

I wrote a series of three blogs where I explained how the period of Earth’s ice age cycle transitioned, beginning about 800,000 years ago, from 41,000 years to approximately 100,000 years. One can access those blogs here,3 here,4 and here.5

Figure 1 shows the global mean (average) temperatures throughout the last four ice age cycles. This graph shows that roughly every 100,000 years the global mean temperature very briefly rose to about 2°C above the present temperature. It also shows that whenever that occurred, Earth quickly dropped into a long cold period where 20–23 percent of Earth’s surface was covered with thick sheets of ice.

Figure 1: Antarctic temperature record for the past four ice age cycles. Temperatures are in °C relative to the average for 1900–1950 AD. Image credit: Robert A. Rohde, Global Warming Art Project, CC-by-SA

The current ice age cycle is exceptional. Instead of the global mean temperature rising rapidly from a minimal value of about 8°C colder than the present (1900–1950 AD average) to 2–3°C warmer than the present, the rapid temperature rise was interrupted by a brief major cooling event that apparently prevented the 2–3°C global mean temperature rise.

Younger Dryas Temperature Anomaly
The brief major cooling event is known as the Younger Dryas. It lasted from 12,900–11,700 years ago. Figure 2 shows the Younger Dryas cooling event (see arrow) relative to the reconstruction of the 9,500-year epoch of extreme climate stability that was the subject of last week’s blog.6

Figure 2: Younger Dryas Cooling Event. The temperature figures represent the surface air temperature in the central region of Greenland’s ice sheet. The blue curve shows the newly determined temperature record of the past 9,500 years. The purple curve shows the temperature record from 16,500–9,500 years ago derived from oxygen-18 isotope measures in ice cores drilled in the central region of Greenland’s ice sheet. The two dotted lines delineate the start and end times of the Younger Dryas event. Data credit for blue curve: Shaun A. Marcott et al.; data credit for purple curve: United States Geological Survey; Diagram credit: Hugh Ross

The Younger Dryas cooling event is unique to the last cycle. It is not present in cycles previous to the last. In the midst of a rapid increase in global mean temperature came a sudden drop of 10°C (18°F), a drop that was sustained for 1,200 years, followed by a sudden rise of 13°C (23°F). Both the sudden drop and the sudden rise occurred over periods of under 20–50 years.7

These temperature changes are for central Greenland. The rest of the mid- and high-latitude northern hemisphere landmasses were impacted to nearly the same degree. The tropical and southern hemisphere landmasses were impacted to a lesser, but nevertheless significant, degree.8

Cause of the Younger Dryas Temperature Anomaly
The consensus scientific explanation for the cause of the Younger Dryas is a near total or complete shutdown of the Atlantic Meridional Overturning Circulation (AMOC), popularly known as the Gulf Stream. The termination of the flow of warm tropical water into the North Atlantic would have reversed the melting of the great North American and European ice sheets. The return of the great ice sheets would have cooled all Earth’s continents and especially North America, Europe, and northern Asia.

Evidence for the termination of the AMOC throughout the Younger Dryas is threefold. First, the Southern Ocean waters became warmer9 as a result of the AMOC being turned back into tropical waters. Second, cold water flowed from the seas adjacent to East Greenland and Iceland into the Nordic seas.10 Third, the injection of cold fresh water into the North Atlantic interrupted deep and intermediate depth AMOC circulations.11

Scientists debate the cause of AMOC shutdown. The most widely accepted scientific explanation is that the AMOC was shut down by a sudden influx of glacial meltwater from Lake Agassiz (figure 3) into the North Atlantic. This rush of cold fresh water into the North Atlantic would have turned back the flow of warm salt water from the tropical Atlantic.

Lake Agassiz formed during the deglaciation of North America. Figure 3 shows Lake Agassiz as it was 13,000 years ago.

Figure 3: Lake Agassiz just before the beginning of the Younger Dryas event. By this time, the North American ice sheets in the west had largely melted away, leaving behind a gigantic lake of glacial meltwater. Ice sheets remained that covered the entire Canadian arctic archipelago, Hudson Bay, the eastern Northwest Territories as far west as Great Slave and Great Bear Lakes, and Ontario and Quebec down to within a few tens of miles of the Great Lakes and the St. Lawrence River. North America image credit: NASA

Once Lake Agassiz formed, it drained southward into the Gulf of Mexico. There is evidence that the flow was interrupted at the time of the Younger Dryas event.12 Sudden breaches to the east and north of Lake Agassiz could have caused a rush of fresh meltwater to burst through the St. Lawrence River into the North Atlantic,13 through the Mackenzie River into the Beaufort Sea, along the Canadian Archipelago, through the Fram Strait, and into the Nordic Seas,14 and/or under the ice that covered the Hudson Bay region and into the North Atlantic.

Asteroidal Impact?
In 2007 a team of 26 physicists, geologists, anthropologists, and chemists noted that at Clovis age sites across North America, thin layers exist. They contain magnetic grains with iridium, magnetic microspherules, charcoal, soot, glass-like carbon containing nanodiamonds, and fullerenes with extraterrestrial helium that date to 12,900 years ago.15 The team demonstrated that these ingredients are or could be evidence for an extraterrestrial impact event. They concluded that a large extraterrestrial object exploded over northern North America which destabilized the Laurentide Ice Sheet and triggered the Younger Dryas cooling event.

Two research teams called into question the nanodiamond16 and charcoal/soot17 evidence, respectively. However, a team of Harvard University planetary scientists led by Michail Petaev noted that a large platinum anomaly in the Greenland ice cores—a signature of an iridium-poor iron asteroid—corresponds to the onset of the Younger Dryas.18 Petaev’s team calculated that the asteroid would need to be 0.8 kilometers in diameter to explain the observed platinum anomaly.

Physicist Mark Boslough, in a reply to the Petaev team’s paper, expressed doubt about a collision event by such a large asteroid.19 He pointed out that collision events by iron asteroids as large as 0.8 kilometers are extremely rare events, occurring only once every several tens of millions of years. Furthermore, he calculated that such an iron asteroid collision event would yield a crater 15–20 kilometers in diameter. It would be nearly impossible, Boslough claimed, for such a large crater created as recently as 11,900 years ago, to elude discovery. He suggested instead that the platinum anomaly was caused by the Cape York meteorite (see figure 4). Eight large iron meteorites, weighing 34, 22, 3.8, 3.3, 0.9, 0.6, 0.1, and 0.02 tons, respectively, have been recovered from northwestern Greenland. Their common chemical makeup and element abundance ratios affirm that they are all from the same body.

Figure 4: Robert Peary Beside the Largest Fragment of the Cape York Meteorite. This 34-ton fragment now is on display at the American Museum of Natural History. Image credit: Robert E. Peary

Petaev’s team responded to Boslough’s reply.20 They pointed out that the platinum anomaly persisted for far too long in the Greenland GISP2 ice core for the meteorite body to be only 10–100 times larger than the combination of the eight large meteorite fragments comprising the Cape York meteorite. They stood by their claim that the platinum anomaly resulted from an extraterrestrial impactor that generated global consequences.

The Drama Continues
Just a few weeks ago, a team of seven geologists announced their discovery of the nearly impossible crater, very recently formed, not just 15–20 but 31 kilometers in diameter! While it’s “nearly impossible” for some people, this kind of miraculous activity appears to be routine for an intelligent, loving Creator who fashioned this improbable planet for human flourishing. In my next blog I will describe this discovery and the likely role it played in granting us a 9,500-year period of extreme climate stability.

Featured image: A portion of a Greenland ice core. Image credit: K. Makinson

  1. Hugh Ross, “Present Climate Epoch Has Been Extremely Stable,” Today’s New Reason to Believe (blog), Reasons to Believe, December 3, 2018,
  2. Hugh Ross, Improbable Planet: How Earth Became Humanity’s Home (Grand Rapids: Baker, 2016), 198–219.
  3. Hugh Ross, “Miracles of the Mid-Pleistocene Transition, Part 1,” Today’s New Reason to Believe (blog), Reasons to Believe, October 1, 2018,
  4. Hugh Ross, “Miracles of the Mid-Pleistocene Transition, Part 2,” Today’s New Reason to Believe (blog), Reasons to Believe, October 8, 2018,
  5. Ross, “Miracles of the Mid-Pleistocene Transition, Part 3,” Today’s New Reason to Believe (blog), Reasons to Believe, October 15, 2018,
  6. Ross, “Present Climate Epoch.”
  7. Richard B. Alley et al., “Abrupt Increase in Greenland Snow Accumulation at the End of the Younger Dryas Event,” Nature 362 (April 8, 1993): 527–29, doi:10.1038/362527a0; Richard B. Alley, “The Younger Dryas Cold Interval as Viewed from Central Greenland,” Quaternary Science Reviews 19 (January 2000): 213–26, doi:10.1016/S0277-3791(99)00062-1.
  8. Paul I. Abell and Ina Plug, “The Pleistocene/Holocene Transition in South Africa: Evidence for the Younger Dryas Event,” Global and Planetary Change 26 (November 2000): 173–79, doi:10.1016/S0921-8181(00)00042-4.
  9. Bernhard Bereiter et al., “Mean Global Ocean Temperatures during the Last Glacial Transition,” Nature 553 (January 4, 2018): 39–44, doi:10.1038/nature25152.
  10. Tine L. Rasmussen et al., “Atlantic Surface Water Inflow to the Nordic Seas during the Pleistocene-Holocene Transition (Mid-Late Younger Dryas and Pre-Boreal Periods, 12,450–10,000 a BP),” Journal of Quaternary Science 26 (October 2011): 723–733, doi:10.1002/jqs.1496.
  11. Selene F. Eltgroth et al., “A Deep-Sea Coral Record of North Atlantic Radiocarbon through the Younger Dryas: Evidence for Intermediate Water/Deepwater Reorganization,” Paleoceanography and Paleoclimatology 21 (December 2006): PA4207, doi:10.1029/2005PA001192; J. F. McManus et al., “Collapse and Rapid Resumption of Atlantic Meridional Circulation Linked to Deglacial Climate Changes,” Nature 428 (April 22, 2004): 834–37, doi:10.1038/nature02494.
  12. Wallace S. Broecker et al., “Routing of Meltwater from the Laurentide Ice Sheet during the Younger Dryas Cold Episode,” Nature 341 (September 28, 1989): 318–21, doi:10.1038/341318a0.
  13. Anders E. Carlson et al., “Geochemical Proxies of North American Freshwater Routing during the Younger Dryas Cold Event,” Proceedings of the National Academy of Sciences USA 104 (April 17, 2007): 6556–61, doi:10.1073/pnas.0611313104; A. E. Carlson and P. U. Clark, “What Caused the Younger Dryas? An Assessment of Existing Hypotheses,” American Geophysical Union, Fall Meeting 2009, (December 2009): abstract id. PP31D–1381.
  14. L. D. Keigwin et al., “Deglacial Floods in the Beaufort Sea Preceded Younger Dryas Cooling,” Nature Geoscience 11 (July 9, 2018): 599–604, doi:10.1038/s41561-018-0169-6.
  15. R. B. Firestone et al., “Evidence for an Extraterrestrial Impact 12,900 Years Ago that Contributed to the Megafaunal Extinctions and the Younger Dryas Cooling,” Proceedings of the National Academy of Sciences USA 104 (October 2007): 16016–21, doi:10.1073/pnas.0706977104.
  16. Tyrone L. Daulton et al., “Comprehensive Analysis of Nanodiamond Evidence Relating to the Younger Dryas Impact Hypothesis,” Journal of Quaternary Science 32 (January 2017): 7–34, doi:10.1002/jqs.2892.
  17. Andrew C. Scott et al., “Interpreting Palaeofire Evidence from Fluvial Sediments: A Case Study from Santa Rosa Island, California, with Implications from the Younger Dryas Impact Hypothesis,” Journal of Quaternary Science 32 (January 2017): 35–47, doi:10.1002/jqs.2914.
  18. Michail I. Petaev et al., “Large Pt Anomaly in the Greenland Ice Core Points to a Cataclysm at the Onset of the Younger Dryas,” Proceedings of the National Academy of Sciences USA 110 (August 6, 2013): 12917–20, doi:10.1073/pnas.1303924110.
  19. Mark Boslough, “Greenland Pt Anomaly May Point to Noncataclysmic Cape York Meteorite Entry,” Proceedings of the National Academy of Sciences USA 110 (December 24, 2013): E5035, doi:10.1073/pnas.1320328111.
  20. Michail I. Petaev et al., “Reply to Boslough: Is Greenland Pt Anomaly Global or Local?” Proceedings of the National Academy of Sciences USA 110 (December 24, 2013): E5036, doi:10.1073/pnas.1320772111.