Winter thermohaline evolution along and below the Ross Ice Shelf

The Ross Ice Shelf floats above the southern sector of the Ross Sea and creates a cavity where critical ocean-ice interactions take place. Crucial processes occurring in this cavity include the formation of Ice Shelf Water, the coldest ocean water, and the intrusion of Antarctic Surface Water, the main driver of frontal and basal melting. During the winter, a polynya forms along the Ross Ice Shelf edge, producing a precursor to Antarctic Bottom Water known as High Salinity Shelf Water. Due to the difficulty of direct exploration of the Ross Ice Shelf in the winter, processes occurring there have been only hypothesized to date. Here we show thermohaline observations collected along the Ross Ice Shelf front from 2020 to 2023 using unconventionally programmed Argo floats. These measurements provide year-round observations of water column changes in and around the Ross Ice Shelf cavity, allowing to quantify production of High Salinity Shelf Water, ocean heat content and basal melt rates.

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Publication Details

Journal
Nature Communications
Published
2024-12-04
DOI
https://doi.org/10.1038/s41467-024-54751-8
Citations
2
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
0.75

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article

Winter thermohaline evolution along and below the Ross Ice Shelf

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2 citations
Nature Communications
Cryospheric studies and observations
0.75
article

Winter thermohaline evolution along and below the Ross Ice Shelf

Elena Mauri, Daniela Flocco, Pierpaolo Falco, Yuri Cotroneo, Giorgio Budillon, Naomi Krauzig, Cosimo Solidoro, Riccardo Martellucci, Massimo Pacciaroni, Milena Menna, Annunziata Pirro, Angela Garzia, Pasquale Castagno, Enrico Zambianchi, Francesco Memmola, Giulio Notarstefano
article en
2 citations

Abstract

The Ross Ice Shelf floats above the southern sector of the Ross Sea and creates a cavity where critical ocean-ice interactions take place. Crucial processes occurring in this cavity include the formation of Ice Shelf Water, the coldest ocean water, and the intrusion of Antarctic Surface Water, the main driver of frontal and basal melting. During the winter, a polynya forms along the Ross Ice Shelf edge, producing a precursor to Antarctic Bottom Water known as High Salinity Shelf Water. Due to the difficulty of direct exploration of the Ross Ice Shelf in the winter, processes occurring there have been only hypothesized to date. Here we show thermohaline observations collected along the Ross Ice Shelf front from 2020 to 2023 using unconventionally programmed Argo floats. These measurements provide year-round observations of water column changes in and around the Ross Ice Shelf cavity, allowing to quantify production of High Salinity Shelf Water, ocean heat content and basal melt rates.

Nature CommunicationsVol. 15(1)
University of Messina (IT), Marche Polytechnic University (IT), Parthenope University of Naples (IT), CoNISMa (IT), National Institute of Oceanography and Applied Geophysics (IT), University of Naples Federico II (IT), Sapienza University of Rome (IT)
Deutsches Zentrum für Luft- und Raumfahrt
Life below water
Openalex Percentile: Top 29%
Cryospheric studies and observations
0.75
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