Articles | Volume 20, issue 5
https://doi.org/10.5194/os-20-1267-2024
https://doi.org/10.5194/os-20-1267-2024
Research article
 | 
18 Oct 2024
Research article |  | 18 Oct 2024

Subsurface floats in the Filchner Trough provide the first direct under-ice tracks of the circulation on shelf

Jean-Baptiste Sallée, Lucie Vignes, Audrey Minière, Nadine Steiger, Etienne Pauthenet, Antonio Lourenco, Kevin Speer, Peter Lazarevich, and Keith W. Nicholls

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Cited articles

Arndt, J. E., Schenke, H. W., Jakobsson, M., Nitsche, F. O., Buys, G., Goleby, B., Rebesco, M., Bohoyo, F., Hong, J., Black, J., Greku, R., Udintsev, G., Barrios, F., Reynoso-Peralta, W., Taisei, M., and Wigley, R.: The international bathymetric chart of the Southern Ocean (IBCSO) version 1.0 – A new bathymetric compilation covering circum-Antarctic waters, Geophys. Res. Lett., 40, 3111–3117, https://doi.org/10.1002/grl.50413, 2013. a
Årthun, M., Nicholls, K. W., Makinson, K., Fedak, M. A., and Boehme, L.: Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica, Geophys. Res. Lett., 39, L17601, https://doi.org/10.1029/2012GL052856, 2012. a, b, c, d
Daae, K., Hattermann, T., Darelius, E., and Fer, I.: On the effect of topography and wind on warm water inflow – An idealized study of the southern Weddell Sea continental shelf system, J. Geophys. Res.-Oceans, 122, 2622–2641, 2017. a, b, c
Daae, K., Hattermann, T., Darelius, E., Mueller, R., Naughten, K., Timmermann, R., and Hellmer, H.: Necessary conditions for warm inflow toward the Filchner Ice Shelf, Weddell Sea, Geophys. Res. Lett., 47, 1–11, 2020. a
Darelius, E. and Sallée, J.-B.: Seasonal outflow of ice shelf water across the front of the Filchner ice shelf, Weddell Sea, Antarctica, Geophys. Res. Lett., 45, 3577–3585, 2018. a, b
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Short summary
In the Weddell Sea, we investigated how warm deep currents and cold waters containing freshwater released from the Antarctic are connected. We used autonomous observation devices that have never been used in this region previously and that allow us to track the movement and characteristics of water masses under the sea ice. Our findings show a dynamic interaction between warm masses, providing key insights to understand climate-related changes in the region.