Footprint of sustained poleward warm water flow within East Antarctic submarine canyons

Abstract The intrusion of relatively warm water onto the continental shelf is widely recognized as a threat to Antarctic ice shelves and glaciers grounded below sea level, as enhanced ocean heat increases their basal melt. While the circulation of warm water has been documented on the East Antarctic...

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Autors principals:	Federica Donda, Michele Rebesco, Vedrana Kovacevic, Alessandro Silvano, Manuel Bensi, Laura De Santis, Yair Rosenthal, Fiorenza Torricella, Luca Baradello, Davide Gei, Amy Leventer, Alix Post, German Leitchenkov, Taryn Noble, Fabrizio Zgur, Andrea Cova, Philip O’Brien, Roberto Romeo
Format:	Artigo
Idioma:	Inglês
Publicat:	Nature Portfolio 2024-07-01
Col·lecció:	Nature Communications
Accés en línia:	https://doi.org/10.1038/s41467-024-50160-z
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