Articles | Volume 16, issue 7
https://doi.org/10.5194/tc-16-2985-2022
https://doi.org/10.5194/tc-16-2985-2022
Research article
 | 
27 Jul 2022
Research article |  | 27 Jul 2022

Development of crystal orientation fabric in the Dome Fuji ice core in East Antarctica: implications for the deformation regime in ice sheets

Tomotaka Saruya, Shuji Fujita, Yoshinori Iizuka, Atsushi Miyamoto, Hiroshi Ohno, Akira Hori, Wataru Shigeyama, Motohiro Hirabayashi, and Kumiko Goto-Azuma

Viewed

Total article views: 2,054 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,584 426 44 2,054 38 43
  • HTML: 1,584
  • PDF: 426
  • XML: 44
  • Total: 2,054
  • BibTeX: 38
  • EndNote: 43
Views and downloads (calculated since 30 Nov 2021)
Cumulative views and downloads (calculated since 30 Nov 2021)

Viewed (geographical distribution)

Total article views: 2,054 (including HTML, PDF, and XML) Thereof 1,967 with geography defined and 87 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Apr 2024
Short summary
Crystal orientation fabrics (COF) of the Dome Fuji ice core were investigated with an innovative method with unprecedentedly high statistical significance and dense depth coverage. The COF profile and its fluctuation were found to be highly dependent on concentrations of chloride ion and dust. The data suggest deformation of ice at the deepest zone is highly influenced by COF fluctuations that progressively develop from the near-surface firn toward the deepest zone within ice sheets.