Articles | Volume 11, issue 4
https://doi.org/10.5194/tc-11-1537-2017
https://doi.org/10.5194/tc-11-1537-2017
Research article
 | 
04 Jul 2017
Research article |  | 04 Jul 2017

A 125-year record of climate and chemistry variability at the Pine Island Glacier ice divide, Antarctica

Franciele Schwanck, Jefferson C. Simões, Michael Handley, Paul A. Mayewski, Jeffrey D. Auger, Ronaldo T. Bernardo, and Francisco E. Aquino

Viewed

Total article views: 3,042 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,732 1,138 172 3,042 380 101 156
  • HTML: 1,732
  • PDF: 1,138
  • XML: 172
  • Total: 3,042
  • Supplement: 380
  • BibTeX: 101
  • EndNote: 156
Views and downloads (calculated since 07 Nov 2016)
Cumulative views and downloads (calculated since 07 Nov 2016)

Viewed (geographical distribution)

Total article views: 3,042 (including HTML, PDF, and XML) Thereof 2,834 with geography defined and 208 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (preprint)

Latest update: 29 Nov 2023
Download
Short summary
The West Antarctic Ice Sheet (WAIS) is more susceptible to marine influences than the East Antarctica Ice Sheet (EAIS). During recent decades, rapid changes have occurred in the WAIS sector, including flow velocity acceleration, retraction of ice streams, and mass loss. In this study, we use an ice core located near the Pine Island Glacier ice divide to reconstruct mineral dust and marine aerosol transport and the influence of climate variables on the elemental concentration.