Ancient cold period could provide clues about future climate change

Ancient cold period could provide clues about future climate change
The entrance to the cave in Puerto Princesa Subterranean River National Park in Palawan, Philippines. The researchers used a stalagmite growing from the floor of the cave to learn about rainfall in the Philippines during the Younger Dryas. Credit: Jud Partin

Researchers at The University of Texas at Austin have found that a well-known period of abrupt climate change 12,000 years ago occurred rapidly in northern latitudes but much more gradually in equatorial regions, a discovery that could prove important for understanding and responding to future climate change.

The research, published Sept. 2 in Nature Communications, focuses on the Younger Dryas, a cooling period that started when the North Atlantic Current, an , stopped circulating. The event caused Earth's northern hemisphere to enter into a deep chill, with temperatures in Greenland dropping by approximately 18 degrees Fahrenheit in less than a decade.

The event also caused rainfall to decrease in places as far away as the Philippines. However, whereas temperatures in Greenland responded quickly to the ocean current shutdown and subsequent reboot 1,000 years later, it took hundreds of years for rainfall in the Philippines to be affected and to recover.

"We found that the temperature in Greenland is like a small ship that you can stop and turn quickly because of the influence of in the region, while rainfall in the tropics is like a big ship that takes a long time to course correct," said Jud Partin, a research associate at the University of Texas Institute for Geophysics (UTIG) who led the study.

The changes in temperature and rainfall are linked to a common cause: the slowdown of the ocean currents in the North Atlantic, which affect climate and temperature as they move warm water from the Gulf of Mexico toward the Arctic. As the world warmed after the last , glaciers melted and diluted northern seawater with freshwater. The resulting change in ocean water density disrupted the current and, in effect, the climate, causing a period of global cooling.

The event also inspired the premise of the 2004 disaster flick "The Day After Tomorrow," which exaggerates the speed and strength of the cooling by depicting the planet entering an ice age in a matter of weeks after the ocean current collapses.

Ancient cold period could provide clues about future climate change
Jud Partin, a research associate at the University of Texas Institute for Geophysics who led the study, in the cave. Credit: Raf Rios

Although other studies well document the changes in temperature and precipitation around the world, this new study concludes that these changes do not occur or recover at the same rate, as had been previously assumed.

Understanding the relationship between temperature and precipitation in the wake of is particularly important because it previews what could happen if the planet's ice sheets continue to lose mass and add freshwater to the North Atlantic.

At a conference in Paris during July of more than 2,000 climate scientists, the potential collapse of the North Atlantic Current's circulation was identified as a possible catastrophic consequence of climate change.

"A slowdown of the ocean circulation is a double-edged sword: If we see some temperature changes associated it ... and somehow are quick to act and alleviate the change, then we have the potential to stop it before it impacts rainfall globally," Partin said. "The longer the circulation event lasts means that it will take that much longer for rainfall to recover."

The researchers discovered how rainfall in the Philippines was affected by the Younger Dryas event by analyzing minerals deposited in a stalagmite growing from the floor of a cave in Puerto Princesa Subterranean River National Park in Palawan. They found that it took more than 550 years for drought conditions to reach their full extent in the region, and about 450 years to return to pre-Younger Dryas levels after the North Atlantic Current began circulating again. The record suggests was about 25 percent lower than present levels during the cold snap.

Ancient cold period could provide clues about future climate change
The room in the cave where the scientists obtained the stalagmite used in the research. Credit: Raf Rios

They then compared these findings with previously published ice core data. According to these records, it took a decade or less for temperatures in Greenland to drop by approximately 18 degrees Fahrenheit once the current collapsed and about 40 years to rebound after it returned.

Partin conducted the work with UTIG Director Terry Quinn and collaborators from the National Taiwan University and the University of the Philippines-Diliman. UTIG is a research unit of The University of Texas at Austin Jackson School of Geosciences.

Computational models of the Younger Dryas temperature and precipitation also provided insight into the role of sea ice in Greenland's abrupt temperature change.

"Sea ice around Greenland acts as a 'switch,' causing that region to respond more quickly than the rest of the planet does by insulating the air from heat stored in the deep ocean," said Yuko Okumura, a UTIG research associate and a co-author on the study.

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Journal information: Nature Communications

Citation: Ancient cold period could provide clues about future climate change (2015, September 2) retrieved 17 September 2019 from
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Nov 02, 2015
Since the YD was associated with a climate change, an extinction event, and a continent-wide 'black mat', it would seem likely that the YD was the result of a meteor impact. But where is the impact crater.

Actually, we may not have a single impact crater, but several thousand of them - the Carolina Bays.

The reason why the Carolina, Maryland, Georgia and Nebraska Bays have been rejected as impact craters, is that they are too shallow, plus they are strangely elliptical. But there is a solution to this, because all these Bays point in one direction - a triangulation onto the Great Lakes region. In which case, the Bays are likely to be the result of secondary impacts that sprayed out from a primary impact on the Great Lakes. And since a secondary projectile will be traveling much slower, it will not create the classic impact crater.

See the article on Academia edu "The Carolina Bays and the Destruction of North America".

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