Rising surface salinity and declining sea ice: A new Southern Ocean state revealed by satellites

For decades, the surface of the polar Southern Ocean (south of 50°S) has been freshening-an expected response to a warming climate. This freshening enhanced upper-ocean stratification, reducing the upward transport of subsurface heat and possibly contributing to sea ice expansion. It also limited the formation of open-ocean polynyas. Using satellite observations, we reveal a marked increase in surface salinity across the circumpolar Southern Ocean since 2015. This shift has weakened upper-ocean stratification, coinciding with a dramatic decline in Antarctic sea ice coverage. Additionally, rising salinity facilitated the reemergence of the Maud Rise polynya in the Weddell Sea, a phenomenon last observed in the mid-1970s. Crucially, we demonstrate that satellites can now monitor these changes in real time, providing essential evidence of the Southern Ocean's potential transition toward persistently reduced sea ice coverage.

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Publication Details

Journal
Proceedings of the National Academy of Sciences
Published
2025-06-30
DOI
https://doi.org/10.1073/pnas.2500440122
Citations
14
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
18.21

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article

Rising surface salinity and declining sea ice: A new Southern Ocean state revealed by satellites

Alberto C. Naveira Garabato, Aditya Narayanan, Matthew R. Mazloff, Rafael Catany et al.
14 citations
Proceedings of the National Academy of Sciences
Arctic and Antarctic ice dynamics
18.21
article

Rising surface salinity and declining sea ice: A new Southern Ocean state revealed by satellites

Alberto C. Naveira Garabato, Aditya Narayanan, Matthew R. Mazloff, Rafael Catany, Verónica González‐Gambau, Alessandro Silvano, F. Alexander Haumann, Theo Spira, Estrella Olmedo, Antonio Turiel, Roberto Sabia
article en
14 citations

Abstract

For decades, the surface of the polar Southern Ocean (south of 50°S) has been freshening-an expected response to a warming climate. This freshening enhanced upper-ocean stratification, reducing the upward transport of subsurface heat and possibly contributing to sea ice expansion. It also limited the formation of open-ocean polynyas. Using satellite observations, we reveal a marked increase in surface salinity across the circumpolar Southern Ocean since 2015. This shift has weakened upper-ocean stratification, coinciding with a dramatic decline in Antarctic sea ice coverage. Additionally, rising salinity facilitated the reemergence of the Maud Rise polynya in the Weddell Sea, a phenomenon last observed in the mid-1970s. Crucially, we demonstrate that satellites can now monitor these changes in real time, providing essential evidence of the Southern Ocean's potential transition toward persistently reduced sea ice coverage.

Proceedings of the National Academy of SciencesVol. 122(27)
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Consejo Superior de Investigaciones Científicas (ES), Scripps Institution of Oceanography (US), National Oceanography Centre (GB), European Space Agency (FR), Institut Català de Ciències del Clima (ES), Argans (United Kingdom) (GB), Institut de Ciències del Mar (ES), European Space Research Institute (IT), University of Southampton (GB), Ludwig-Maximilians-Universität München (DE), University of Gothenburg (SE)
National Science Foundation, National Aeronautics and Space Administration, European Space Agency, Ministerio de Ciencia e Innovación, Natural Environment Research Council, European Research Council
Life below water
Openalex Percentile: Top 0%
Arctic and Antarctic ice dynamics
18.21
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