Articles | Volume 19, issue 10
https://doi.org/10.5194/tc-19-5231-2025
https://doi.org/10.5194/tc-19-5231-2025
Research article
 | 
30 Oct 2025
Research article |  | 30 Oct 2025

Seasonal variability of ocean heat transport and ice-shelf basal melt around Antarctica

Fabio Boeira Dias, Matthew H. England, Adele K. Morrison, and Benjamin K. Galton-Fenzi

Viewed

Total article views: 3,765 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,221 474 70 3,765 52 79
  • HTML: 3,221
  • PDF: 474
  • XML: 70
  • Total: 3,765
  • BibTeX: 52
  • EndNote: 79
Views and downloads (calculated since 13 Feb 2025)
Cumulative views and downloads (calculated since 13 Feb 2025)

Viewed (geographical distribution)

Total article views: 3,765 (including HTML, PDF, and XML) Thereof 3,622 with geography defined and 143 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 12 Feb 2026
Download
Short summary
The Antarctic Ice Sheet melting dominates the sea-level projection uncertainties. Much uncertainty arises from our limited understanding of how ice shelves melt from below. Using a detailed ocean–ice-shelf model, we found that East Antarctic ice shelves experience seasonal melting driven by ocean heat transport variability. In contrast, West Antarctic ice shelves show consistent melting due to a steady supply of warm, deep water, indicating a potentially distinct response due to a warming climate.
Share