Articles | Volume 13, issue 5
https://doi.org/10.5194/cp-13-437-2017
https://doi.org/10.5194/cp-13-437-2017
Research article
 | 
09 May 2017
Research article |  | 09 May 2017

A glaciochemical study of the 120 m ice core from Mill Island, East Antarctica

Mana Inoue, Mark A. J. Curran, Andrew D. Moy, Tas D. van Ommen, Alexander D. Fraser, Helen E. Phillips, and Ian D. Goodwin

Viewed

Total article views: 3,001 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,686 1,111 204 3,001 336 139 215
  • HTML: 1,686
  • PDF: 1,111
  • XML: 204
  • Total: 3,001
  • Supplement: 336
  • BibTeX: 139
  • EndNote: 215
Views and downloads (calculated since 15 Sep 2016)
Cumulative views and downloads (calculated since 15 Sep 2016)

Viewed (geographical distribution)

Total article views: 3,001 (including HTML, PDF, and XML) Thereof 2,907 with geography defined and 94 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (preprint)

Latest update: 26 Jul 2024
Download
Short summary
A 120 m ice core from Mill Island, East Antarctica, was studied its chemical components. The Mill Island ice core contains 97 years of climate record (1913–2009) and has a mean snow accumulation of 1.35 m yr−1 (ice equivalent). Trace ion concentrations were generally higher than other Antarctic ice core sites. Nearby sea ice concentration was found to influence the annual mean sea salt record. The Mill Island ice core records are unexpectedly complex, with strong modulation of the trace chemistry.