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The end of the Arctic as we know it

  • ‘Hot, sour and out of breath,’ the northern ocean is ailing faster than expected, with potentially catastrophic consequences for all of us

Reading Time:9 minutes
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The Greenpeace ship Arctic Sunrise takes scientists to test sea ice in the Fram Strait between the Norwegian archipelago of Svalbard and Greenland. Picture: Denis Sinyakov / Greenpeace

The demise of an entire ocean is almost too much to grasp, but as the expedition sails deeper into the Arctic, the colossal processes of breakdown are increasingly evident.

The first fragment of ice appears off the starboard bow a few kilometres before the 79th parallel in the Fram Strait, which lies between Greenland and the Norwegian archipelago of Svalbard. The solitary floe is soon followed by another, then another, then clusters, then swarms, then entire fields of white crazy paving that stretch to the horizon.

From deck level it is a stunning sight. But from high above, drones and helicopters capture the bigger, more alarming picture: a slow-motion blast pattern of frozen shrapnel radiating from the high Arctic southwards through this strait, which is the interchange of 80 per cent of the water between the ice cap and the world’s oceans.
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This is where ice floes come to die, and the cemetery is filling faster each year, according to the leader of this scientific expedition, Till Wagner, of the University of North Carolina at Wilmington (UNCW), in the United States. One of the objectives of the expedition is to investigate why the collapse of Arctic ice is happening faster than climate computer models predict and to understand what this augurs for the rest of the planet.

The melt is not simply a seasonal process. The natural thaw that starts with spring’s warm weather is being amplified by man-made global heating. The Arctic has warmed by 2 degrees Celsius above pre-industrial temperatures, twice the global average. Some hot spots, including parts of the Fram Strait, have heated up by 4 degrees. There are variations from year to year, but the trend is clear and accelerating.

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Sea ice is melting earlier in the spring and freezing later in the autumn. Each summer it thins more and recedes further, leaving greater expanses of the ocean exposed to 24-hour sunlight. This is driving back the frontiers of ice and fragmenting one of the planet’s most important climate regulators. It is also creating a series of feedbacks that are accelerating the Arctic melt. Several are only partially understood.

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