Articles | Volume 15, issue 2
https://doi.org/10.5194/tc-15-1087-2021
https://doi.org/10.5194/tc-15-1087-2021
Research article
 | 
01 Mar 2021
Research article |  | 01 Mar 2021

Brief communication: Spatial and temporal variations in surface snow chemistry along a traverse from coastal East Antarctica to the ice sheet summit (Dome A)

Guitao Shi, Hongmei Ma, Zhengyi Hu, Zhenlou Chen, Chunlei An, Su Jiang, Yuansheng Li, Tianming Ma, Jinhai Yu, Danhe Wang, Siyu Lu, Bo Sun, and Meredith G. Hastings

Viewed

Total article views: 1,530 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,001 488 41 1,530 210 27 30
  • HTML: 1,001
  • PDF: 488
  • XML: 41
  • Total: 1,530
  • Supplement: 210
  • BibTeX: 27
  • EndNote: 30
Views and downloads (calculated since 25 Sep 2020)
Cumulative views and downloads (calculated since 25 Sep 2020)

Viewed (geographical distribution)

Total article views: 1,530 (including HTML, PDF, and XML) Thereof 1,451 with geography defined and 79 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 24 Feb 2024
Download
Short summary
It is important to understand atmospheric chemistry over Antarctica under a changing climate. Thus snow collected on a traverse from the coast to Dome A was used to investigate variations in snow chemistry. The non-sea-salt fractions of K+, Mg2+, and Ca2+ are associated with terrestrial inputs, and nssCl is from HCl. In general, proportions of non-sea-salt fractions of ions to the totals are higher in the interior areas than on the coast, and the proportions are higher in summer than in winter.