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CORRECTION article

Front. Mar. Sci., 17 March 2021

Sec. Global Change and the Future Ocean

Volume 8 - 2021 | https://doi.org/10.3389/fmars.2021.667007

Corrigendum: Borealization of the Arctic Ocean in Response to Anomalous Advection From Sub-Arctic Seas

  • 1. International Arctic Research Center and College of Natural Science and Mathematics, University of Alaska Fairbanks, Fairbanks, AK, United States

  • 2. Finnish Meteorological Institute, Helsinki, Finland

  • 3. Polar Science Center, Applied Physics Lab and School of Oceanography, University of Washington, Seattle, WA, United States

  • 4. Department of Arctic and Marine Biology UiT - the Arctic University of Norway, Tromsø, Norway

  • 5. Institute of Ocean Sciences, Fisheries and Oceans Canada, Sidney, BC, Canada

  • 6. Institute of Marine Research, Fram Centre, Tromsø, Norway

  • 7. College of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, AK, United States

  • 8. SINTEF Ocean AS, Trondheim, Norway

  • 9. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia

  • 10. Chalmers University of Technology, Gothenburg, Sweden

  • 11. Institute of Marine Research, Bergen, Norway

  • 12. International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, United States

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In the original article, there was an error. The description of the method used to calculate the depth of the lower boundary of the halocline is not complete. “This algorithm is used in Figures 12, 13. The depth of the 0°C isotherm defines the total halocline base depth; it is used in all other figures where the depth of the halocline base is required (Figures 7, 8, 14, 15 and Supplementary Figure 7).” was missing from the original description.

A correction has been made to Methods, Sub-section a. Methods in physical observations, Sub-section Halocline Base Depth:

“For each CTD and ITP profile the lower halocline boundary is defined following Bourgain and Gascard (2011) who show that the density ratio Rρ = (α∂θ/∂z)/(β∂S/z) = 0.05 (α is the thermal expansion coefficient and β is the haline contraction coefficient, θ is potential temperature and S is salinity) may be used to identify the cold halocline base depth. This algorithm is used in Figures 12, 13. The depth of the 0°C isotherm defines the total halocline base depth; it is used in all other figures where the depth of the halocline base is required (Figures 7, 8, 14, 15 and Supplementary Figure 7).”

The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.

References

  • 1

    Bourgain P. Gascard J.-C. (2011). The Arctic Ocean halocline and its interannual variability from 1997 to 2008. Deep Sea Res. I58, 745756. 10.1016/j.dsr.2011.05.001

Summary

Keywords

Arctic ocean, climate change, atlantification and pacification, multidisciplinary changes, future projections

Citation

Polyakov IV, Alkire MB, Bluhm BA, Brown KA, Carmack EC, Chierici M, Danielson SL, Ellingsen I, Ershova EA, Gårdfeldt K, Ingvaldsen RB, Pnyushkov AV, Slagstad D and Wassmann P (2021) Corrigendum: Borealization of the Arctic Ocean in Response to Anomalous Advection From Sub-Arctic Seas. Front. Mar. Sci. 8:667007. doi: 10.3389/fmars.2021.667007

Received

12 February 2021

Accepted

15 February 2021

Published

17 March 2021

Volume

8 - 2021

Edited and reviewed by

Dorte Krause-Jensen, Aarhus University, Denmark

Updates

Copyright

*Correspondence: Igor V. Polyakov

This article was submitted to Global Change and the Future Ocean, a section of the journal Frontiers in Marine Science

Disclaimer

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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