Will ice floating in the Arctic Sea move faster or slower over the coming decades? The response will tell us whether marine transportation can be expected to become more or less dangerous. It might also have meaningful implications for the rate of arctic ice cover loss, which is hugely consequential for Northern Indigenous communities, ecosystems, and the global climate system.
While observational data suggest the trend has been towards faster sea ice speeds, climate models project that those speeds will slow down during the summer. This contrast has led to some questions about the plausibility of the model projections.
In a new paper published today in The Cryosphere, Lassonde School of Engineering Associate Professor Neil Tandon and Postdoctoral Visitor Jamie Ward found that, while the mechanisms driving the ice slowdown remain plausible, questions remain regarding the timing of the slowdown.
“Understanding how sea ice motion is going to change is clearly of interest. Yet we didn’t know if what the models were projecting was reasonable,” says Tandon. Also with the Centre for Research in Earth and Space Science (CRESS) at York University. We can expect sea ice to continue to speed up for some time. There will be a point in the coming decades when the dynamics will shift.
Floating sea ice presents a particular hazard for marine transportation, says Tandon, pointing to a dramatic example from 2017 when arctic sea ice trapped and sunk two fishing boats around Newfoundland. And the faster the ice, the more hazardous the conditions.
A Spring Analogy of Arctic Sea
To understand why sea ice has been speeding up, Tandon says a spring can be a useful analogy. As temperatures warm and the ice thins, it can expand and contract more readily. Just as a spring made of thinner metal can expand and contract more easily than a thicker metal spring.
“As the thinner sea ice expands and contracts more, it generates more momentum for the sea ice, just like one of those spring-loaded toy cars goes faster the farther back you pull it,” explains Tandon.
However, this is not the only force acting on the ice. When the ice gets thin enough, the internal stresses that produce “springiness” start to fade, and other forces start to dominate.
“As ice enters what they call a free drift state, the internal stress becomes negligible. The external forces of wind and the ocean surface tilt beginning to dominate. The models indicate that changes in the wind and ocean surface tilt will drive a slowdown of the sea ice during the summer season.”
Tandon says that while the models generally agree that this summertime slowdown will occur. They do not agree on when it will start. Some models suggest that the slowdown will start within the next decade. While others suggest it will start toward the end of this century.
Faster ice drifts can create hazardous conditions for marine transport, so in that sense, an ice slowdown could be seen as a positive, but Tandon says there are bigger considerations.
“It does not change the fact that sea ice cover is steadily declining, right? This is a problem because of the impact on ecosystems. These Indigenous populations rely on being able to hunt certain animals, the animal’s ability to survive the changing habitat. The overall effect on the global climate,” says Tandon. “But, I would say it is marginally good news in that the models are telling that some of the most destructive aspects we were expecting about ice cover decline are not being projected.”
