Articles | Volume 19, issue 12
https://doi.org/10.5194/tc-19-6483-2025
https://doi.org/10.5194/tc-19-6483-2025
Brief communication
 | 
03 Dec 2025
Brief communication |  | 03 Dec 2025

Brief communication: Annual variability of the atmospheric circulation at large spatial scale reconstructed from a data assimilation framework cannot explain local East Antarctic ice rises' surface mass balance records

Marie G. P. Cavitte, Hugues Goosse, Quentin Dalaiden, and Nicolas Ghilain

Viewed

Total article views: 1,742 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,322 193 227 1,742 88 57 68
  • HTML: 1,322
  • PDF: 193
  • XML: 227
  • Total: 1,742
  • Supplement: 88
  • BibTeX: 57
  • EndNote: 68
Views and downloads (calculated since 30 Oct 2024)
Cumulative views and downloads (calculated since 30 Oct 2024)

Viewed (geographical distribution)

Total article views: 1,742 (including HTML, PDF, and XML) Thereof 1,721 with geography defined and 21 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 15 Jan 2026
Download
Short summary
Ice cores are influenced by local processes that alter SMB (surface mass balance) records. To evaluate if atmospheric circulation on large spatial scales can explain differing snowfall trends at 8 East Antarctic ice rises, we assimilated their ice core SMB records within a high-resolution downscaled atmospheric model with quantified local errors from radar constraints. The reconstruction captures the SMB records’ variability but may over-fit by introducing unrealistic spatial heterogeneity.
Share