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Volume 13, issue 2
Ocean Sci., 13, 349–363, 2017
https://doi.org/10.5194/os-13-349-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Climate–carbon–cryosphere interactions in the...

Ocean Sci., 13, 349–363, 2017
https://doi.org/10.5194/os-13-349-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 Apr 2017

Research article | 27 Apr 2017

Shelf–Basin interaction along the East Siberian Sea

Leif G. Anderson et al.
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR by Leif Anderson on behalf of the Authors (25 Mar 2017)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (31 Mar 2017) by Tommaso Tesi
AR by Leif Anderson on behalf of the Authors (02 Apr 2017)  Author's response    Manuscript
ED: Publish as is (03 Apr 2017) by Tommaso Tesi
Publications Copernicus
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Short summary
We use data collected in 2014 to show that the outflow of nutrient-rich water occurs much further to the west than has been reported in the past. We suggest that this is due to much less summer sea-ice coverage in the northwestern East Siberian Sea than in the past decades. Further, our data support a more complicated flow pattern in the region where the Mendeleev Ridge reaches the shelf compared to the general cyclonic circulation within the individual basins as suggested historically.
We use data collected in 2014 to show that the outflow of nutrient-rich water occurs much...
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