The discovery of the Slims River diversion away from the Bering Sea into another watershed that empties into the Pacific Ocean was published yesterday in the journal Nature Geoscience.
Gerard Roe, co-author of the study and a professor at the University of Washington in Seattle in the US state of Washington, told AFP today that the Slims riverbed had dried up in only four days.
"The habitat was altered," he said in a telephone interview. "The chemistry and biology of the water changed dramatically."
They traced its mysterious disappearance to the Slims River's headwaters, where they found a glacial barrier that once routed its flow northward into the Bering Sea had been breached in the spring.
This "abruptly and radically" altered drainage from the Kaskawulsh Glacier spring melt, according to the study, sent the river in the opposite direction into the Pacific Ocean, 1,300 kilometers away from where the mouth of the river used to be.
Such changes, they warned in the study, can have "profound downstream impacts" on ecosystems and communities that rely on the discharge.
Last summer, for example, Kluane Lake, which was fed by the Slims River, dropped a full meter below its lowest recorded level for that time of year.
Another research team member, John Clague of Simon Fraser University in Vancouver, said the discovery highlights that while people view climate change as a gradual process, its effects may not be.
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