Climate Change Reroutes a Yukon River in a Geological Instant

Apr 20, 2017

By John Schwartz

In the blink of a geological eye, climate change has helped reverse the flow of water melting from a glacier in Canada’s Yukon, a hijacking that scientists call “river piracy.”

This engaging term refers to one river capturing and diverting the flow of another. It occurred last spring at the Kaskawulsh Glacier, one of Canada’s largest, with a suddenness that startled scientists.

A process that would ordinarily take thousands of years — or more — happened in just a few months in 2016.

Much of the meltwater from the glacier normally flows to the north into the Bering Sea via the Slims and Yukon Rivers. A rapidly retreating and thinning glacier — accelerated by global warming — caused the water to redirect to the south, and into the Pacific Ocean.

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One comment on “Climate Change Reroutes a Yukon River in a Geological Instant”

  • @OP – link Changes in the flow of rivers can have enormous consequences for the landscape and ecosystems of the affected areas, as well as water supplies. When the shift abruptly reduced water levels in Kluane Lake, the Canadian Broadcasting Corporation reported, it left docks for lakeside vacation cabins — which can be reached only by water — high and dry.

    The riverbed of the Slims River basin, now nearly dry, experienced frequent and extensive afternoon dust storms through the spring and summer of last year, the paper stated.

    These sorts of rapid changes can have radical effects on those living in river valleys, who depend on melt-water for irrigation, water supply, or transport by boat, while those in the path of the new diversion can lose land and property to flooding.

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