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Volume 7, issue 3
Ocean Sci., 7, 305-316, 2011
https://doi.org/10.5194/os-7-305-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Synoptic Antarctic Shelf-Slope Interactions (SASSI)

Ocean Sci., 7, 305-316, 2011
https://doi.org/10.5194/os-7-305-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 May 2011

Research article | 06 May 2011

On the freshening of the northwestern Weddell Sea continental shelf

H. H. Hellmer1, O. Huhn2, D. Gomis3, and R. Timmermann1 H. H. Hellmer et al.
  • 1Alfred Wegener Institut für Polar und Meeresforschung, Bremerhaven, Germany
  • 2Institut für Umweltphysik, Universität Bremen, Bremen, Germany
  • 3IMEDEA, Universitat de les Illes Balears – CSIC, Mallorca, Spain

Abstract. We analyzed hydrographic data from the northwestern Weddell Sea continental shelf of the three austral winters 1989, 1997, and 2006 and two summers following the last winter cruise. During summer a thermal front exists at ~64° S separating cold southern waters from warm northern waters that have similar characteristics as the deep waters of the central basin of the Bransfield Strait. In winter, the whole continental shelf exhibits southern characteristics with high Neon (Ne) concentrations, indicating a significant input of glacial melt water. The comparison of the winter data from the shallow shelf off the tip of the Antarctic Peninsula, spanning a period of 17 yr, shows a salinity decrease of 0.09 for the whole water column, which has a residence time of <1 yr. We interpret this freshening as being caused by a combination of reduced salt input due to a southward sea ice retreat and higher precipitation during the late 20th century on the western Weddell Sea continental shelf. However, less salinification might also result from a delicate interplay between enhanced salt input due to sea ice formation in coastal areas formerly occupied by Larsen A and B ice shelves and increased Larsen C ice loss.

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