Articles | Volume 18, issue 8
https://doi.org/10.5194/tc-18-3685-2024
https://doi.org/10.5194/tc-18-3685-2024
Research article
 | 
20 Aug 2024
Research article |  | 20 Aug 2024

Novel approach to estimate the water isotope diffusion length in deep ice cores with an application to Marine Isotope Stage 19 in the Dome C ice core

Fyntan Shaw, Andrew M. Dolman, Torben Kunz, Vasileios Gkinis, and Thomas Laepple

Viewed

Total article views: 1,051 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
838 162 51 1,051 52 56
  • HTML: 838
  • PDF: 162
  • XML: 51
  • Total: 1,051
  • BibTeX: 52
  • EndNote: 56
Views and downloads (calculated since 07 Dec 2023)
Cumulative views and downloads (calculated since 07 Dec 2023)

Viewed (geographical distribution)

Total article views: 1,051 (including HTML, PDF, and XML) Thereof 1,033 with geography defined and 18 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 13 Dec 2024
Download
Short summary
Fast variability of water isotopes in ice cores is attenuated by diffusion but can be restored if the diffusion length is accurately estimated. Current estimation methods are inadequate for deep ice, mischaracterising millennial-scale climate variability. We address this using variability estimates from shallower ice. The estimated diffusion length of 31 cm for the bottom of the Dome C ice core is 20 cm less than the old method, enabling signal recovery on timescales previously considered lost.