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 m...
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| Veröffentlicht in: | Nature communications 2024-12, Vol.15 (1), p.10581-10, Article 10581 |
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| creator | Falco, Pierpaolo Krauzig, Naomi Castagno, Pasquale Garzia, Angela Martellucci, Riccardo Cotroneo, Yuri Flocco, Daniela Menna, Milena Pirro, Annunziata Mauri, Elena Memmola, Francesco Solidoro, Cosimo Pacciaroni, Massimo Notarstefano, Giulio Budillon, Giorgio Zambianchi, Enrico |
| description | 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.
This study presents thermohaline observations collected along the Ross Ice Shelf front from 2020 to 2023 using unconventionally programmed Argo floats that provide year-round observations of water column changes close to the Ross Ice Shelf cavity. |
| doi_str_mv | 10.1038/s41467-024-54751-8 |
| format | Article |
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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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| source | PubMed Central (Open Access); SpringerOpen (Open Access); Alma/SFX Local Collection; EZB Electronic Journals Library; Nature (Open access); Directory of Open Access Journals (Open Access) |
| subjects | 704/106/694 704/829/2737 Bottom water Enthalpy Floats Humanities and Social Sciences Ice formation Ice shelves Land ice multidisciplinary Polynyas Salinity Salinity effects Science Science (multidisciplinary) Seawater Surface water Water circulation Water column Winter |
| title | Winter thermohaline evolution along and below the Ross Ice Shelf |
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