Earth Chgs Sea ice triggered the Little Ice Age, finds a new study

Housecarl

On TB every waking moment
Hummm.....

Posted for fair use.....

September 16th, 2020
Sea ice triggered the Little Ice Age, finds a new study


Takeaways
  • Sea ice can act as an agent of climate change on a variety of timescales and spatial scales—it’s not just a passive responder to change.
  • The Little Ice Age may have arisen “out of the blue,” from internal variability within the climate system, rather than in response to an external push from volcanic eruptions or other factors.
  • A far-flung pulse of sea ice may have contributed to the demise of the Norse colonies in Greenland in the 14th and 15th centuries.


martinmiles_270_192.jpg
INSTAAR Research Associate Martin Miles in a modern subarctic fjord setting.

A new study finds a trigger for the Little Ice Age that cooled Europe from the 1300s through mid-1800s, and supports surprising model results suggesting that under the right conditions sudden climate changes can occur spontaneously, without external forcing.

The study, published in Science Advances, reports a comprehensive reconstruction of sea ice transported from the Arctic Ocean through the Fram Strait, by Greenland, and into the North Atlantic Ocean over the last 1400 years. The reconstruction suggests that the Little Ice Age—which was not a true ice age but a regional cooling centered on Europe—was triggered by an exceptionally large outflow of sea ice from the Arctic Ocean into the North Atlantic in the 1300s.

While previous experiments using numerical climate models showed that increased sea ice was necessary to explain long-lasting climate anomalies like the Little Ice Age, physical evidence was missing. This study digs into the geological record for confirmation of model results.
Researchers pulled together records from marine sediment cores drilled from the ocean floor from the Arctic Ocean to the North Atlantic to get a detailed look at sea ice throughout the region over the last 1400 years.

“We decided to put together different strands of evidence to try to reconstruct spatially and temporally what the sea ice was during the past one and a half thousand years, and then just see what we found,” said Martin Miles, an INSTAAR researcher who also holds an appointment with NORCE Norwegian Research Centre and Bjerknes Centre for Climate Research in Norway.

The cores included compounds produced by algae that live in sea ice, the shells of single-celled organisms that live in different water temperatures, and debris that sea ice picks up and transports over long distances. The cores were detailed enough to detect abrupt (decadal scale) changes in sea ice and ocean conditions over time.

The records indicate an abrupt increase in Arctic sea ice exported to the North Atlantic starting around 1300, peaking in midcentury, and ending abruptly in the late 1300s.

MartinM_mapgraph_535_234.jpg
The map shows Greenland and adjacent ocean currents. Colored circles show where some of the sediment cores used in the study were obtained from the seafloor. The small historical map from the beginning of the 20th century shows the distribution of Storis, or sea ice from the Arctic Ocean, which flows down the east coast of Greenland. The graphs show the reconstructed time series of changes in the occurrence of sea ice and polar waters in the past. The colors of the curves correspond to the locations on the map. The blue shading represents the period of increased sea ice in the 1300s. The figures are modified from Miles et al., 2020.

“I've always been fascinated by not just looking at sea ice as a passive indicator of climate change, but how it interacts with or could actually lead to changes in the climate system on long timescales,” said Miles. “And the perfect example of that could be the Little Ice Age.”

“This specific investigation was inspired by an INSTAAR colleague, Giff Miller, as well as by some of the paleoclimate reconstructions of my INSTAAR colleagues Anne Jennings, John Andrews, and Astrid Ogilvie,” added Miles. Miller authored the first paper to suggest that sea ice played an essential role in sustaining the Little Ice Age.

Scientists have argued about the causes of the Little Ice Age for decades, with many suggesting that explosive volcanic eruptions must be essential for initiating the cooling period and allowing it to persist over centuries. One the hand, the new reconstruction provides robust evidence of a massive sea-ice anomaly that could have been triggered by increased explosive volcanism. On the other hand, the same evidence supports an intriguing alternate explanation.

Climate models called “control models” are run to understand how the climate system works through time without being influenced by outside forces like volcanic activity or greenhouse gas emissions. A set of recent control model experiments included results that portrayed sudden cold events that lasted several decades. The model results seemed too extreme to be realistic—so-called Ugly Duckling simulations—and researchers were concerned that they were showing problems with the models.

Miles’ study found that there may be nothing wrong with those models at all.

“We actually find that number one, we do have physical, geological evidence that these several decade-long cold sea ice excursions in the same region can, in fact do, occur,” he said. In the case of the Little Ice Age, “what we reconstructed in space and time was strikingly similar to the development in an Ugly Duckling model simulation, in which a spontaneous cold event lasted about a century. It involved unusual winds, sea ice export, and a lot more ice east of Greenland, just as we found in here.” The provocative results show that external forcing from volcanoes or other causes may not be necessary for large swings in climate to occur. Miles continued, “These results strongly suggest...that these things can occur out of the blue due to internal variability in the climate system.”

The marine cores also show a sustained, far-flung pulse of sea ice near the Norse colonies on Greenland coincident with their disappearance in the 15th century. A debate has raged over why the colonies vanished, usually agreeing only that a cooling climate pushed hard on their resilience. Miles and his colleagues would like to factor in the oceanic changes nearby: very large amounts of sea ice and cold polar waters, year after year for nearly a century.

“This massive belt of ice that comes streaming out of the Arctic—in the past and even today—goes all the way around Cape Farewell to around where these colonies were,” Miles said. He would like to look more closely into oceanic conditions along with researchers who study the social sciences in relation to climate.

Camilla S. Andresen, of the Geological Survey of Denmark and Greenland, and Christian V. Dylmer, of MMT Sweden AB, were coauthors of the study.
 

TxGal

Day by day
This is an excellent find, Housecarl!

I posted a link to your post in the Grand Solar Minimum thread. Folks that read the GSM thread should read this article. Here's the link to the GSM thread:

 

Delta

Has No Life - Lives on TB
I have a hard time accepting an event without a cause. Give me either a physical cause or a divine one. But give me a cause.
 

Housecarl

On TB every waking moment
Here's another take on Miles' work.....

Posted for fair use.....

What actually started the Little Ice Age?
It all may have started with sea ice, and the changes may have happened all by themselves without the influence of volcanoes or the Sun, researchers behind a new study say.
1592727.jpg
Elise Kjørstad journalist
friday 23. october 2020 - 12:12

The ninth century seems to have experienced a warmer climate, which has been called the Medieval Warm Period.

But from the 14th century things were different. It rained "without stopping" in 1315, and grain didn’t ripen. The situation was much the same the following year. Later in the 14th century there were several episodes of wild weather and cold periods.

The Little Ice Age can be divided into two phases, according to an article in The New Yorker. It began with a cooling period in 1300 - 1400. The coldest period was from the end of the 1500s to 1850.
This cooling caused glaciers to expand in Scandinavia, the Alps, in Iceland, Alaska, China, in the southern Andes and in New Zealand.

Londoners were able to skate on the Thames now and then. In France and Switzerland, advancing glaciers crushed villages, according to the Encyclopaedia Britannica. Wet summers and icy winters led to poor crops and famine for several years in Northern and Central Europe.

What started it all? Researchers behind a new study have an unusual proposal.

They suggest that the cooling may have occurred spontaneously and by itself.

Ugly ducklings
Generally speaking, the Little Ice Age is said to have begun because of an increase in volcanism and reduced activity of the Sun.

A large volcanic eruption in 1257 followed by three smaller eruptions through the end of the13th century have been suggested as the cause of the Little Ice Age. Aerosols from the eruptions may have shaded the Sun and made the Earth colder. Thereafter, feedback related to northern sea ice ensured that there were cold periods long afterwards.

“The timing agrees quite well with the great eruptions from the 13th century. So there is good empirical evidence that this could be true,” said Martin Miles, a researcher at NORCE Norwegian Research Centre, and the Bjerknes Centre for Climate Research in Bergen, and at the University of Colorado at Boulder in the USA.

But in a new study, Miles and his colleagues have looked at another possibility.

Sometimes climate models behave strangely. These models may show sudden changes in the north, without added climate drivers such as volcanism or changing solar activity. These computer runs have been called "ugly ducklings", because they seem to have something wrong with them.
But it is not clear that these computer simulations are wrong.

“It may be that changes in sea ice and sea ice outflow from the Arctic Ocean have happened randomly due to internal variability in the climate system. Maybe these models, which people are sceptical of, are actually correct,” says Miles.
Martin Miles is a researcher at NORCE Norwegian Research Centre and the Bjerknes Centre for Climate Research in Bergen, and at the University of Colorado, Boulder in the USA.

Martin Miles is a researcher at NORCE Norwegian Research Centre and the Bjerknes Centre for Climate Research in Bergen, and at the University of Colorado, Boulder in the USA. (Photo: Martin Miles)

Lots of ice on the go
In their new study, Miles and his colleagues looked at the transport of sea ice from the Arctic over a 1400 year period.

They compiled data from seabed samples from areas outside Greenland, the eastern part of the Fram Strait, the Greenland Sea and off Iceland. The samples contained small fossils that give researchers information about sea temperatures and loose material that sea ice had carried with it.

In several of these areas, ice will only be found if there is an especially large amount flowing out of the Arctic Ocean. This is particularly true during cold periods and when there is also a lot of sea ice formation.

“We discovered that an unusually large amount of sea ice flowed out of the Arctic Ocean from the beginning of the 14th century. It is very interesting, and the biggest event we found during the last 1400 years,” says Miles.

“It happened right around the start of the Little Ice Age. This indicates that it was very important, and was perhaps a necessary kickstart for the Little Ice Age.”

A lot of ice flowed out of this region for almost 100 years. At the beginning of the 15th century, ice flow decreased, but the amount of meltwater in the area had increased and remained elevated for a long time afterwards.

The transport of sea ice is due to wind fields that also affect ocean currents in the Arctic Ocean, Miles said. Most of the ice exits the area through the Fram Strait, and amounts vary a lot.

“In some periods, there’s a lot of ice, such as during the Great Salinity Anomaly in the 1960s. For three or four years, an unusual amount of sea ice flowed out through the Fram Strait, which had an impact in the Nordic seas for many years afterwards. What we have discovered is very similar to the Great Salinity Anomaly, but it lasted much longer, almost 100 years,” he said.
The strait between Greenland and Svalbard is the only deep connection between the Arctic Ocean and the world's oceans.

The strait between Greenland and Svalbard is the only deep connection between the Arctic Ocean and the world's oceans. (Image: Bdushaw / CC BY-SA 3.0 / Wikimedia Commons)

Can’t explain everything
Miles says sea ice may have affected the climate in Europe in the 14th century in this way.
The ice that melts and turns into fresh water can affect ocean currents, which in turn affect the atmosphere and climate, he says.

“Ocean currents are very important for transporting heat to Europe. If the currents weaken a little, it will be much colder than usual,” he said.

Sea ice is not only a reaction to climate change, but can also trigger climate change, Miles says.

However, sea ice changes during the 14th century can’t fully explain why it was cold for several centuries during the Little Ice Age.

“There must have been some kind of influence or event during the period afterwards for it to continue to be relatively cold. There was a lot of volcanism during the Little Ice Age and three or four periods with less solar radiation. So it is not necessarily just the one incident that can explain everything, of course,” Miles said.

During the Little Ice Age, global temperatures dropped by about 0.5 degrees C. But it was not the same everywhere.

“The Little Ice Age was certainly not global. More and more researchers have found that it was regional and that it was not completely cold throughout the period. There was a lot of variability from place to place. I think the best expression for the period is ‘the European Little Ice Age’, because it was mostly the North Atlantic, Greenland and Northern Europe that were affected,” he said.
Changes in average global temperature over the last 2000 years.

Changes in average global temperature over the last 2000 years. (Graphics: Ed Hawkins / RCraig09 / Wikimedia Commons)

Previous study supports the findings
The results of the new study are supported by geologist Willem van der Bilt, a postdoctoral fellow at the University of Bergen.

Van der Bilt led a study published last year, in which he and his fellow researchers promoted the idea that growth in Arctic sea ice may have occurred spontaneously at an earlier stage.

He and his colleagues used geological data to look at the distribution of sea ice and glaciers on land. They found that sea ice in the Arctic advanced a few centuries before the Little Ice Age, between the years 650 and 950. During this period there was little volcanic activity, and more stable solar activity, according to the article published in Quaternary Science Reviews.

“In both the new study and in our work, we see that there is a fairly dramatic increase in sea ice cover through the region. This seems to coincide with all other types of evidence for cooling in the area,” van der Bilt said.

“People have long argued that this type of change must have been triggered by external influences, such as volcanic eruptions and the amount of solar radiation that hits the earth's surface. But the timing of these changes in our study does not really fit with this,” he said.

Van der Bilt and his colleagues also took a closer look at the ugly duckling models. They found that the changes they discovered were similar to what happened during these anomalous model simulations.
Willem van der Bilt is a postdoctoral fellow at the University of Bergen.

Willem van der Bilt is a postdoctoral fellow at the University of Bergen. (Photo: Cedric Hamelin)

Still an open question
Van der Bilt thinks we need to be aware that abrupt climate change may have taken place in the past, without any external drivers or mechanism to cause it.

“Broadly speaking, this could open our eyes to the possibility that abrupt climate change is an inherent feature of the Earth’s climate system, in that there are now a couple of studies that show this has happened at different times,” he said.

Van der Bilt thinks it is gratifying when theoretical climate models and actual data from the past support the same findings.

“It’s quite valuable in helping us better understand whether the climate models are correct or if something interesting is happening that we can’t really explain. We can compare our different datasets and work together to better understand what the climate system may have in store for us in the future,” he said.

Miles says it remains an open question whether the Little Ice Age and other past changes in the climate may have occurred spontaneously.

“We have focused on only one incident. But it looks like there were perhaps four or five of these in the past. The next step will be to see if we can map these and check them against volcanic eruptions and solar variability. That may help us figure out if they happened by chance or were due to other influences,” he said.

But today's climate change is not accidental, says van der Bilt.

“We have an incredible understanding of how our planet is changing. We can see the changes in the sea day by day and measure temperatures around the world,” he said.

“This allows us to say that yes, today, what we see is definitely driven by what our species has done to the atmosphere when it comes to greenhouse gases, which is a very different climate mechanism.”

Translated by Nancy Bazilchuk
References:
Martin W. Miles et.al.: “Evidence for extreme export of Arctic sea ice leading the abrupt onset of the Little Ice Age”, Science Advances, 2020.
Willem van der Bilt et.al.: “Was Common Era glacier expansion in the Arctic Atlantic region triggered by unforced atmospheric cooling?", Quaternary Science Reviews, 2019.
———
Read the Norwegian version of this article at forskning.no

rELATED:



Scientists are seeing ice age beginnings for very first time
 

Housecarl

On TB every waking moment
Posted for fair use.....

Possible 1,000-kilometer-long river running deep below Greenland’s ice sheet
Research Press Release | November 12, 2020
Computational models suggest that melting water originating in the deep interior of Greenland could flow the entire length of a subglacial valley and exit at Petermann Fjord, along the northern coast of the island. Updating ice sheet models with this open valley could provide additional insight for future climate change predictions.


Satellite image of Greenland (Suomi NPP/VIIRS satellite image; NASA Worldview).

Radar surveys have previously mapped Greenland’s bedrock buried beneath two to three thousand meters of ice. Mathematical models were used to fill in the gaps in survey data and infer bedrock depths. The surveys revealed the long valley, but suggested it was segmented, preventing water from flowing freely through it. However, the peaks breaking the valley into segments only show up in areas where the mathematical modelling was used to fill in missing data, so could not be real.

Christopher Chambers and Ralf Greve, scientists at Hokkaido University’s Institute of Low Temperature Science, wanted to explore what might happen if the valley is open and melting increases at an area deep in Greenland’s interior known for melting. Collaborating with researchers at the University of Oslo, they ran numerous simulations to compare water dynamics in northern Greenland with and without valley segmentation.

The results, recently published in The Cryosphere, show a dramatic change in how water melting at the base of the ice sheet would flow, if the valley is indeed open. A distinct subglacial watercourse runs all the way from the melting site to Petermann Fjord, which is located more than 1,000 kilometers away on the northern coast of Greenland. The watercourse only appears when valley segmentation is removed; there are no other major changes to the landscape or water dynamics.

“The results are consistent with a long subglacial river,” Chambers says, “but considerable uncertainty remains. For example, we don’t know how much water, if any, is available to flow along the valley, and if it does indeed exit at Petermann Fjord or is refrozen, or escapes the valley, along the way.”


The suggested valley and possible river flowing from the deep interior of Greenland to Petermann Fjord deep below Greenland’s ice sheet (500 meters below sea level). (Christopher Chambers et al, The Cryosphere, November 12, 2020).

If water is flowing, the model suggests it could traverse the whole length of the valley because the valley is relatively flat, similar to a riverbed. This suggests no parts of the ice sheet form a physical blockade. The simulations also suggested that there was more water flow towards the fjord with a level valley base set at 500 meters below sea level than when set at 100 meters below. In addition, when melting is increased only in the deep interior at a known region of basal melting, the simulated discharge is increased down the entire length of the valley only when the valley is unblocked. This suggests that a quite finely tuned relationship between the valley form and overlying ice can allow a very long down-valley water pathway to develop.

“Additional radar surveys are needed to confirm the simulations are accurate,” says Greve, who has been developing the model used in the study, called Simulation Code for Polythermal Ice Sheets (SICOPOLIS). “This could introduce a fundamentally different hydrological system for the Greenland ice sheet. The correct simulation of such a long subglacial hydrological system could be important for accurate future ice sheet simulations under a changing climate.”


Christopher Chambers (left) and Ralf Greve (right), (Photo: Ralf Greve).

Original Article:
Christopher Chambers et al. Possible impacts of a 1000km long hypothetical subglacial river valley towards Petermann Glacier in northern Greenland. The Cryosphere. November 12, 2020.
DOI: 10.5194/tc-14-3747-2020

Funding:
This work was supported by the Japan Society for the Promotion of Science (JSPS) KAKENHI (JP16H02224, JP17H06104, JP17H06323), the Arctic Challenge for Sustainability (ArCS) project of the Japanese Ministry of Education, Culture, Sports, Science and Technology (MEXT; JPMXD1300000000), the CryoJaNo project funded by SIU (Norwegian Centre for International Cooperation in Higher Education; HNP-2015/10010), the European Union FP7 European Research Council (ERC) project ICEMASS (320816), the European Space Agency (ESA) project ICEFLOW (4000125560 18 I-NS), the Norwegian Research Council-funded CalvingSEIS project (244196/E10), and the Norwegian Ministry of Climate and Environment.

Contacts:
Dr. Christopher Chambers
Institute of Low Temperature Science
Hokkaido University
Email: youstormorg[at]gmail.com

Sohail Keegan Pinto
International Public Relations Specialist
Hokkaido University
Tel: +81-11-706-2185
Email: en-press[at]general.hokudai.ac.jp
 
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