Northern Pacific Ocean’s heat flow is accelerating Arctic warming

The movement of warm, moist air from the North Pacific to the Arctic is driving low-cloud formation and accelerating warming in the Arctic, new research suggests. Photo by NASA/Carnegie

Aug. 8 (UPI) — New research suggests heat flow in the northern Pacific Ocean is having a greater impact on climate change in the Arctic than expected.

The Arctic is warming at accelerated rates and losing ice at a faster clip than predicted by models. The phenomenon is known as Arctic amplification.

Previous studies have detailed a variety of positive feedback mechanisms in the Arctic driving warming and melting, but until now, oceanic heat flow hasn’t been well understood.

Paleoclimate records show rapid climate change in the Arctic isn’t uncommon. During the last deglaciation period, Greenland experienced two periods of sudden warming, each featuring temperature increases of 27 degrees Fahrenheit over the course of a few decades.

Records suggest each of the two episodes were correlated with accelerated warming in the mid-latitude North Pacific and North Atlantic oceans.

Using historic data, scientists designed new models to predict how heat flow in the North Pacific and North Atlantic oceans is driving Arctic amplification.

“Since there appeared to be coupling between abrupt Arctic temperature changes and sea surface temperature changes in both the North Atlantic and North Pacific in the past, we thought it was important to untangle how each region may affect the Arctic differently in order to provide insight into recent and future Arctic changes,” Summer Praetorius, a former postdoctoral fellow at the Carnegie Institution for Science, said in a news release.

The models showed both warming and cooling trends in the North Pacific had a larger impact on Arctic temperatures than changes in the North Atlantic.

Scientists believe the North Pacific’s influence is driven by the movement of moist, warm air, which seeds low-lying clouds, trapping warm air closer to the surface in the Arctic. The phenomenon likely amplifies other ice-melting, air-warming positive feedback mechanisms.

Researchers detailed their work this week in the journal Nature Communications.


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