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      Variability and extreme of Mackenzie River daily discharge during 1973–2011

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      Quaternary International
      Elsevier BV

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          The role of sea ice and other fresh water in the Arctic circulation

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            Accelerated decline in the Arctic sea ice cover

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              Increasing river discharge to the Arctic Ocean.

              Synthesis of river-monitoring data reveals that the average annual discharge of fresh water from the six largest Eurasian rivers to the Arctic Ocean increased by 7% from 1936 to 1999. The average annual rate of increase was 2.0 +/- 0.7 cubic kilometers per year. Consequently, average annual discharge from the six rivers is now about 128 cubic kilometers per year greater than it was when routine measurements of discharge began. Discharge was correlated with changes in both the North Atlantic Oscillation and global mean surface air temperature. The observed large-scale change in freshwater flux has potentially important implications for ocean circulation and climate.
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                Author and article information

                Journal
                Quaternary International
                Quaternary International
                Elsevier BV
                10406182
                September 2015
                September 2015
                : 380-381
                :
                : 159-168
                Article
                10.1016/j.quaint.2014.09.023
                601c8bb3-28c3-4810-b164-e8728db58f68
                © 2015
                History

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