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Ocean Science An interactive open-access journal of the European Geosciences Union

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doi:10.5194/os-2016-95
© Author(s) 2016. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
16 Dec 2016
Review status
A revision of this discussion paper is under review for the journal Ocean Science (OS).
Shelf–Basin interaction along the Laptev – East Siberian Seas
Leif G. Anderson1, Göran Björk1, Ola Holby2, Sara Jutterström3, Carl Magnus Mörth4, Matt O'Regan4, Christof Pearce4,5, Igor Semiletov6,7,8, Christian Stranne4,10, Tim Stöven1,9, Toste Tanhua9, Adam Ulfsbo1,11, and Martin Jakobsson4 1Department of Marine Sciences, University of Gothenburg, 412 96 Gothenburg, Sweden
2Department of Environmental and Energy Systems, Karlstad University, 651 88 Karlstad, Sweden
3IVL Swedish Environmental Research Institute, Box 530 21, 400 14 Gothenburg, Sweden
4Department of Geological Sciences, Stockholm University, 106 91 Stockholm, Sweden
5Department of Geoscience, Aarhus University, Aarhus, Denmark
6International Arctic Research Center, University Alaska Fairbanks, Fairbanks, AK 99775, USA
7Pacific Oceanological Institute, Russian Academy of Sciences Far Eastern Branch, Vladivostok 690041, Russia
8The National Research Tomsk Polytechnic University, Tomsk, Russia
9Helmholtz Centre for Ocean Research Kiel, GEOMAR, Kiel, Germany
10Center for Coastal and Ocean Mapping/Joint Hydrographic Center, 03824 Durham, NH, USA
11Division of Earth and Ocean Sciences, Nicholas School of the Environment, Duke University, Durham, NC 27704, USA
Abstract. Extensive biogeochemical transformation of organic matter takes place in the shallow continental shelf seas of Siberia. This, in combination with brine production from sea-ice formation, results in cold bottom waters with relatively high salinity and nutrient concentrations, as well as low oxygen and pH levels. Data from the SWERUS-C3 expedition with icebreaker Oden, July to September 2014, show the distribution of such nutrient rich cold bottom waters along the continental margin from about 140 to 180° E. The water with maximum nutrient concentration, classically named the upper halocline, is absent over the Lomonosov Ridge at 140° E while it appears in the Makarov Basin at 150° E to intensify further eastwards. At the intercept between the Mendeleev Ridge and the East Siberian continental shelf slope, the nutrient maximum is still intense, but distributed across a larger depth interval. The nutrient rich water is found at salinities up to ~ 34.5. East of 170° E transient tracers show significantly less ventilated waters below about 150 m water depth. This likely results from a local isolation of waters over the Chukchi Abyssal Plain as the boundary current from the west is steered away from this area by the bathymetry of the Mendeleev Ridge. The water with salinities of ~ 34.5 has high nutrients and low oxygen concentrations as well as low pH, typically indicating decay of organic matter. A deficit in nitrate relative to phosphate suggests that this process partly occurs under hypoxia. We conclude that the high nutrient water with salinity ~ 34.5 are formed on the shelf slope in the Mendeleev Ridge region from interior basin water that is trapped for enough time to achieve its signature.

Citation: Anderson, L. G., Björk, G., Holby, O., Jutterström, S., Mörth, C. M., O'Regan, M., Pearce, C., Semiletov, I., Stranne, C., Stöven, T., Tanhua, T., Ulfsbo, A., and Jakobsson, M.: Shelf–Basin interaction along the Laptev – East Siberian Seas, Ocean Sci. Discuss., doi:10.5194/os-2016-95, in review, 2016.
Leif G. Anderson et al.
Leif G. Anderson et al.
Leif G. Anderson et al.

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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 reach 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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