Streamflow from northern Eurasia into the Arctic Ocean has been increasing since the 1930s. Research shows that increased poleward moisture transport is responsible for additional water in the region.
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Troy, T. Wetting the Arctic. Nature Clim Change 3, 17–18 (2013). https://doi.org/10.1038/nclimate1790
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DOI: https://doi.org/10.1038/nclimate1790