Past intrusion of Circumpolar Deep Water in the Ross Sea: Impacts on the ancient Ross Ice Shelf

The Ross Ice Shelf, Antarctica's largest by area, may face increased instability under future warming, threatening the Antarctic Ice Sheet. Understanding its past response to climate change is critical for anticipating future sea-level rise. We present a multi-proxy reconstruction of ocean and cryosphere conditions in the Ross Sea over the past 40,000 years. Our data show that warm Circumpolar Deep Water reached the JOIDES Trough in the western Ross Sea shortly after the Last Glacial Maximum, coinciding with the retreat of an ancestral ice shelf. This oceanic warming aligns with a southward shift of both the westerly and easterly wind belts, indicating a large-scale atmospheric mechanism driving regional ocean changes. The timing and nature of these processes reveal the tight coupling between atmospheric circulation, ocean heat transport, and ice shelf dynamics. These interactions led to reduced ice shelf extent, highlighting the role of ocean-atmosphere coupling in the Pacific sector of the Southern Ocean during deglaciation.

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Publication Details

Journal
Science Advances
Published
2025-06-27
DOI
https://doi.org/10.1126/sciadv.adt7075
Citations
2
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
2.60
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article

Past intrusion of Circumpolar Deep Water in the Ross Sea: Impacts on the ancient Ross Ice Shelf

Mathia Sabino, Federico Giglio, Francesca Battaglia, Simon T. Belt et al.
2 citations
Science Advances
Geology and Paleoclimatology Research
2.60
article

Past intrusion of Circumpolar Deep Water in the Ross Sea: Impacts on the ancient Ross Ice Shelf

Mathia Sabino, Federico Giglio, Francesca Battaglia, Simon T. Belt, Tommaso Tesi, Alessio Di Roberto, Andrea Geniram, Fiorenza Torricella, Jens Hefter, Enrico Pochini, Alessio Nogarotto, Francesco Muschitiello, Lucilla Capotondi, G. Giorgetti, Ester Colizza, Gesine Mollenhauer, Chiara Pambianco
article en
2 citations

Abstract

The Ross Ice Shelf, Antarctica's largest by area, may face increased instability under future warming, threatening the Antarctic Ice Sheet. Understanding its past response to climate change is critical for anticipating future sea-level rise. We present a multi-proxy reconstruction of ocean and cryosphere conditions in the Ross Sea over the past 40,000 years. Our data show that warm Circumpolar Deep Water reached the JOIDES Trough in the western Ross Sea shortly after the Last Glacial Maximum, coinciding with the retreat of an ancestral ice shelf. This oceanic warming aligns with a southward shift of both the westerly and easterly wind belts, indicating a large-scale atmospheric mechanism driving regional ocean changes. The timing and nature of these processes reveal the tight coupling between atmospheric circulation, ocean heat transport, and ice shelf dynamics. These interactions led to reduced ice shelf extent, highlighting the role of ocean-atmosphere coupling in the Pacific sector of the Southern Ocean during deglaciation.

Science AdvancesVol. 11(26)
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Université Libre de Bruxelles (BE), University of Trieste (IT), Ca' Foscari University of Venice (IT), University of Alberta (CA), University of Bremen (DE), University of Cambridge (GB), Istituto Nazionale di Geofisica e Vulcanologia (IT), Institute of Atmospheric Sciences and Climate (IT), National Research Council (RO), National Research Council (IT), University of Florence (IT), University of Plymouth (GB)
Life below water
Openalex Percentile: Top 11%
Geology and Paleoclimatology Research
2.60
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