Articles | Volume 14, issue 1
https://doi.org/10.5194/essd-14-65-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-14-65-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data description paper
| 
12 Jan 2022
Data description paper |
| 12 Jan 2022
| 12 Jan 2022
Water masses distribution offshore the Sabrina Coast (East Antarctica)
National Institute of Oceanography and Applied Geophysics (OGS), Trieste, 34010, Italy
Vedrana Kovačević
National Institute of Oceanography and Applied Geophysics (OGS), Trieste, 34010, Italy
Federica Donda
National Institute of Oceanography and Applied Geophysics (OGS), Trieste, 34010, Italy
Philip Edward O'Brien
Department of Environmental Sciences, Macquarie University, Sydney, Australia
Linda Armbrecht
Institute for Marine and Antarctic Studies, University of Tasmania, Battery Point, TAS 7004, Australia
Leanne Kay Armand
Research School of Earth Sciences, Australian National University, Canberra, Australia
deceased, Leanne Kay Armand on 4 January 2022
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Short summary
The Totten Glacier (Sabrina Coast, East Antarctica) has undergone significant retreat in recent years, underlining its sensitivity to climate change and its potential contribution to global sea-level rise. The melting process is strongly influenced by ocean dynamics and the spatial distribution of water masses appears to be linked to the complex morpho-bathymetry of the area, supporting the hypothesis that downwelling processes contribute to shaping the architecture of the continental margin.
The Totten Glacier (Sabrina Coast, East Antarctica) has undergone significant retreat in recent...
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