Many Antarctic glaciers are hemorrhaging ice. This one is healing its cracks

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Many Antarctic glaciers are hemorrhaging ice. This one is healing its cracks
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Scientists have explored the recesses of an Antarctic glacier that is currently stable, helping improve predictions of the continent’s fate.

Understanding what is happening at Kamb will help scientists predict how large parts of the Antarctic coastline that are not currently vulnerable might respond as the world continues to warm due to human-caused climate change. Here’s what’s different about Kamb.In December 2019, two teams of researchers from New Zealand and the United States visited the Kamb Ice Stream — a type of glacier that consists of a channel of faster-moving ice surrounded by slower ice.

The new finding at Kamb makes sense, says New Zealand team member Christina Hulbe, of the University of Otago, because the seabed at Kamb is relatively shallow. So it is not exposed to the deep, warm ocean currents that are hitting Thwaites. The globes were greenish — a hue often seen in winter ice that forms on the surface of the ocean. This color makes Lawrence and his colleagues think that the globes form from the ultracold mixture of seawater and meltwater that circulates up into a crack and refreezes, gradually filling in the crack, from the top down, over many decades. They think that this is happening in all of the crevasses they observed. “These crevasses are effectively healing themselves,” he says.

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