Dominoes fall: Vanishing Arctic ice shifts jet stream, which melts Greenland glaciers


Investigating the factors affecting ice melt in Greenland — one of the most rapidly changing places on Earth — is a major priority for climate scientists. And new research is revealing that there are a more complex set of variables affecting the ice sheet than experts had imagined. A recent set of scientific papers have proposed a critical connection between sharp declines in Arctic sea ice and changes in the atmosphere, which they say are not only affecting ice melt in Greenland, but also weather patterns all over the North Atlantic.

The new studies center on an atmospheric phenomenon known as "blocking" — this is when high pressure systems remain stationary in one place for long periods of time (days or even weeks), causing weather conditions to stay relatively stable for as long as the block remains in place. They can occur when there's a change or disturbance in the jet stream, causing the flow of air in the atmosphere to form a kind of eddy, said Jennifer Francis , a research professor and climate expert at Rutgers University.

Blocking events over Greenland are particularly interesting to climate scientists because of their potential to drive temperatures up and increase melting on the ice sheet.

"When they do happen, and they kind of set up in just the right spot, they bring a lot of warm, moist air from the North Atlantic up over Greenland, and that helps contribute to increased cloudiness and warming of the surface," Francis said. "When that happens, especially in the summer, we tend to see these melt events occur."

Now, two new studies have suggested that there's been a recent increase in the frequency of melt-triggering blocking events over Greenland — and that it's likely been fueled by climate change-driven losses of Arctic sea ice.

A paper published Monday in the International Journal of Climatology reveals an uptick in the frequency of these blocking events over Greenland since the 1980s.

A team of researchers led by the University of Sheffield's Edward Hanna used a global meteorological dataset relying on historical records to measure the frequency and strength of high pressure systems over Greenland all the way back to the year 1851. Previous analyses had only extended the record back to 1948, so the new study is able to place recent blocking events in a much larger historical context.

When the researchers analyzed the data, they found that the increase in blocking frequency over the past 30 years is particularly pronounced in the summer, the time of year when blocking events are likely to have the biggest impact on ice melt.

What's been causing this uptick is a big source of interest for climate scientists hoping to gain a better understanding of the events affecting the vulnerable Greenland ice sheet. In the new paper, Hanna and his colleagues suggested that declines in Arctic sea ice might be playing a role — and it's a theory that's heavily supported by another paper just out in the Journal of Climate. That study used both observational data and computer simulations to investigate the connection between sea ice declines and atmospheric changes in the Arctic.

Diminishing Arctic sea ice is a well-established trend at this point, driven by climate change-induced warming in the region. In fact, just last month, scientists reported that the maximum extent of Arctic sea ice this past winter had reached a record low for the second year straight.

Interestingly, what happens on the surface of the ocean also has the potential to seriously influence activity in the atmospheric, said Francis, a co-author on the study.

"When there's less sea ice, obviously it's a much darker surface that's exposed to the sunshine — and especially in the late spring, early summer when the sun is really strong, that open water that would normally have ice on it absorbs a lot more of the sun's heat," she said. "And so the surface of the ocean in this case warms up quite a bit, and that extra heat then is also transferred into the atmosphere."

When that happens, lower layers of the atmosphere warm and expand, pushing up on higher layers of the atmosphere and causing the jetstream to bulge, she explained. The reason this happens has to do with the physics behind airflow in the atmosphere.

Since warm air takes up more space than cooler air, and the equator is the warmest part of the earth, the atmosphere is generally thickest there. This creates a kind of downhill "slope" from the equator to the poles over which air flows. Because the Earth is spinning so quickly, however, airflow ends up being pushed toward the east. The result is the jetstream — a current of air that generally flows from west to east around the world, but also tends to meander north and south in wavy lines as it goes along.

If the Arctic warms more quickly than the rest of the Earth, however, the downhill slope between the equator and the poles becomes less steep — and this can weaken the jetstream's flow, making it more susceptible to twists and turns. So as sea ice disappears and the atmosphere in the Arctic warms and expands, it can make airflow in the jetstream more likely to loop and bulge, causing the kinds of swirling eddies that result in blocking events.

Both the researchers' observations and their model simulations strongly supported the idea that sea ice declines are a major factor in the frequency of blocking events over Greenland. When the researchers made changes only to sea ice in their model, they found an immediate connection to increased blocking, which in turn has led to increased surface melt on the ice sheet.

"That's a pretty robust connection there," Francis said. "It's not just two things that happened coincidentally."

The findings are consistent with his own study, Hanna noted, and also serve as an example of a kind of "feedback that can actually amplify the climate warming over that region," he said. As the climate continues to warm, more sea ice melts — and as more sea ice is lost, the resulting atmospheric changes cause more warming, which causes more melt.


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