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      Retreat of the cold halocline layer in the Arctic Ocean

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      Journal of Geophysical Research: Oceans
      American Geophysical Union (AGU)

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          Some results from a time-dependent thermodynamic model of sea ice

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            On the halocline of the Arctic Ocean

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              Two circulation regimes of the wind-driven Arctic Ocean

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                Author and article information

                Journal
                Journal of Geophysical Research: Oceans
                J. Geophys. Res.
                American Geophysical Union (AGU)
                01480227
                May 15 1998
                May 15 1998
                : 103
                : C5
                : 10419-10435
                Article
                10.1029/98JC00580
                29540372-c3a7-44c7-adb5-e28c07bee64a
                © 1998

                http://doi.wiley.com/10.1002/tdm_license_1.1

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