Local drivers of amplified Arctic warming

November 19, 2018, Institute for Basic Science
The observations show a clear enhancement of warming In the Arctic region and across Siberia, Northern Canada and Alaska. Credit: Institute for Basic Science (IBS)

Long-term observations of surface temperatures show an intensified surface warming in Canada, Siberia, Alaska and in the Arctic Ocean relative to global mean temperature rise. This warming pattern, commonly referred to as Arctic amplification, is consistent with computer models, simulating the response to increasing greenhouse gas concentrations. However, the underlying physical processes for the intensified warming still remain elusive.

A new international research study on the cause of Arctic amplification published this week in the journal Nature Climate Change shows that local greenhouse gas concentrations, and Arctic climate feedbacks outweigh other processes. Using complex computer simulations, the scientists were able to disprove previously suggested hypotheses, that emphasized the role of transport of heat from the tropics to the poles as one of the key contributors to the amplified in the Arctic.

"Our study clearly shows that local carbon dioxide forcing and polar feedbacks are most effective in Arctic amplification compared to other processes," said corresponding author Malte Stuecker, project leader at the IBS Center for Climate Physics (ICCP) in Busan, South Korea.

Increasing anthropogenic carbon dioxide (CO2) concentrations trap heat in the atmosphere, which leads to surface warming. Regional processes can then further amplify or dampen this effect, thereby creating the typical pattern of global warming. In the Arctic region, surface warming reduces snow and sea-ice extent, which in turn decreases the reflectivity of the surface. As a result, more sunlight can reach the top of layers of the soil and ocean, leading to accelerated warming. Furthermore, changes in Arctic clouds and of the vertical atmospheric temperature profile can enhance warming in the polar regions.

In addition to these factors, heat can be transported into the Arctic by winds. "We see this process for instance during El Niño events. Tropical warming, caused either by El Niño or anthropogenic greenhouse emissions, can cause global shifts in atmospheric weather patterns, which may lead to changes in surface temperatures in remote regions, such as the Arctic," said Kyle Armour, co-author of the study and professor of Atmospheric Sciences and Oceanography at the University of Washington.

Moreover, global warming outside the Arctic region will also lead to an increase in Atlantic Ocean temperatures. Ocean currents, such as the Gulf Stream and the North Atlantic drift can then transport the warmer waters to the Arctic ocean, where they could melt sea ice and experience further amplification due to local processes.

To determine whether tropical warming, atmospheric wind and ocean current changes contribute to future Arctic Amplification, the team designed a series of computer model simulations. "By comparing simulations with only Arctic CO2 changes with simulations that apply CO2 globally, we find similar Arctic warming patterns. These findings demonstrate that remote physical processes from outside the do not play a major role, in contrast to previous suggestions," says co-author Cecilia Bitz, professor of Atmospheric Sciences at the University of Washington.

In the tropics—fueled by high temperature and moisture—air can easily move up to high altitudes, meaning the atmosphere is unstable. In contrast, the Arctic atmosphere is much more stable with respect to vertical air movement. This condition enhances the CO2-induced warming in the Arctic near the surface. In the tropics—due to the unstable atmosphere—CO2 mostly warms the upper atmosphere and energy is easily lost to space. This is opposite to what happens in the Arctic: Less outgoing infrared radiation escapes the atmosphere, which further amplifies the surface-trapped warming.

"Our computer simulations show that these changes in the vertical atmospheric temperature profile in the Arctic region outweigh other regional feedback factors, such as the often-cited ice-albedo feedback" says Malte Stuecker.

The new findings of this study highlight the importance of Arctic processes in controlling the pace at which sea-ice will retreat in the Arctic Ocean. The results are also important to understand how sensitive polar ecosystems, Arctic permafrost and the Greenland ice-sheet will respond to Global Warming.

Explore further: Pacific Ocean's effect on Arctic warming

More information: Malte F. Stuecker et al, Polar amplification dominated by local forcing and feedbacks, Nature Climate Change (2018). DOI: 10.1038/s41558-018-0339-y

Related Stories

Pacific Ocean's effect on Arctic warming

August 7, 2018

New research, led by former Carnegie postdoctoral fellow Summer Praetorius, shows that changes in the heat flow of the northern Pacific Ocean may have a larger effect on the Arctic climate than previously thought. The findings ...

Recommended for you

Matter waves and quantum splinters

March 25, 2019

Physicists in the United States, Austria and Brazil have shown that shaking ultracold Bose-Einstein condensates (BECs) can cause them to either divide into uniform segments or shatter into unpredictable splinters, depending ...

How tree diversity regulates invading forest pests

March 25, 2019

A national-scale study of U.S. forests found strong relationships between the diversity of native tree species and the number of nonnative pests that pose economic and ecological threats to the nation's forests.

Study suggests trees are crucial to the future of our cities

March 25, 2019

The shade of a single tree can provide welcome relief from the hot summer sun. But when that single tree is part of a small forest, it creates a profound cooling effect. According to a study published today in the Proceedings ...


Adjust slider to filter visible comments by rank

Display comments: newest first

3 / 5 (4) Nov 19, 2018
As glaciers melt in Alaska, the land, relieved of the weight, rises faster than the sea level. The net effect is sea levels in parts of Alaska are falling.
5 / 5 (2) Nov 19, 2018
As glaciers melt in Alaska, the land, relieved of the weight, rises faster than the sea level. The net effect is sea levels in parts of Alaska are falling.

This well known effect is also quite slow because of the viscosity of the mantle rock. The effects of more water from glacier melt and thermal expansion is very fast, at least an order of magnitude faster. Expecting sea levels to fall because of rebound effects isn't practical or reasonable.
1 / 5 (3) Nov 19, 2018
Why Most Published Research Findings Are False
DOI: 10.1371/journal.pmed.0020124
5 / 5 (1) Nov 20, 2018
As glaciers melt in Alaska, the land, relieved of the weight, rises faster than the sea level. The net effect is sea levels in parts of Alaska are falling.

Is there any reason you thought this was relevant to the article? Perhaps you can comment on something with equal relevancy such as the airspeed of an unladen swallow?
5 / 5 (1) Nov 20, 2018
Why Most Published Research Findings Are False
DOI: 10.1371/journal.pmed.0020124

There's a reason these articles about problems with published research are always about the softer sciences, like biology and "social science", and never about papers like this one which are based on physics.
not rated yet Nov 21, 2018
well z5, as you insist that your brain is so simple that physics can explain such simplicity?

The rest of us live in a world of ever changing, constantly fermenting, evolving, mutating biology, psychology, societies and cultures that physics is incompetent to even begin to explain.

You obviously resent that there are no simple answers in reality. And Time refuses to halt at your command.

Please sign in to add a comment. Registration is free, and takes less than a minute. Read more

Click here to reset your password.
Sign in to get notified via email when new comments are made.