On-shelf circulation of warm water toward the Totten Ice Shelf in East Antarctica

• Published in: Nature communications Vol. 14; no. 1; p. 4955
• Main Authors: Hirano, Daisuke, Tamura, Takeshi, Kusahara, Kazuya, Fujii, Masakazu, Yamazaki, Kaihe, Nakayama, Yoshihiro, Ono, Kazuya, Itaki, Takuya, Aoyama, Yuichi, Simizu, Daisuke, Mizobata, Kohei, Ohshima, Kay I., Nogi, Yoshifumi, Rintoul, Stephen R., van Wijk, Esmee, Greenbaum, Jamin S., Blankenship, Donald D., Saito, Koji, Aoki, Shigeru
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 17.08.2023; Nature Publishing Group; Nature Portfolio
• Subjects: 704/106/829; 704/829/2737; Bathymetry; Continental shelves; Geologic depressions; Glaciers; Heat transport; Humanities and Social Sciences; Ice shelves; Land ice; multidisciplinary; Science; Science (multidisciplinary); Sea level; Warm water; Water circulation; Antarctica
• ISSN: 2041-1723; 2041-1723
• DOI: 10.1038/s41467-023-39764-z

The Totten Glacier in East Antarctica, with an ice volume equivalent to >3.5 m of global sea-level rise, is grounded below sea level and, therefore, vulnerable to ocean forcing. Here, we use bathymetric and oceanographic observations from previously unsampled parts of the Totten continental shelf to reveal on-shelf warm water pathways defined by deep topographic features. Access of warm water to the Totten Ice Shelf (TIS) cavity is facilitated by a deep shelf break, a broad and deep depression on the shelf, a cyclonic circulation that carries warm water to the inner shelf, and deep troughs that provide direct access to the TIS cavity. The temperature of the warmest water reaching the TIS cavity varies by ~0.8 °C on an interannual timescale. Numerical simulations constrained by the updated bathymetry demonstrate that the deep troughs play a critical role in regulating ocean heat transport to the TIS cavity and the subsequent basal melt of the ice shelf. The Totten Glacier in East Antarctica is grounded below sea level and vulnerable to ocean forcing. Observations and simulations demonstrate warm water access from offshore to the glacier, facilitated by deep topography off the Sabrina Coast.