Articles | Volume 14, issue 5
https://doi.org/10.5194/tc-14-1537-2020
https://doi.org/10.5194/tc-14-1537-2020
Research article
 | 
12 May 2020
Research article |  | 12 May 2020

Refractory black carbon (rBC) variability in a 47-year West Antarctic snow and firn core

Luciano Marquetto, Susan Kaspari, and Jefferson Cardia Simões

Viewed

Total article views: 3,369 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,570 730 69 3,369 54 50
  • HTML: 2,570
  • PDF: 730
  • XML: 69
  • Total: 3,369
  • BibTeX: 54
  • EndNote: 50
Views and downloads (calculated since 06 Nov 2019)
Cumulative views and downloads (calculated since 06 Nov 2019)

Viewed (geographical distribution)

Total article views: 3,369 (including HTML, PDF, and XML) Thereof 2,673 with geography defined and 696 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 28 Mar 2024
Download
Short summary
Black carbon, commonly known as soot, is a particle originating from the incomplete combustion of fossil fuels and biomass burning that plays an important role in the climatic system. In this work, we analyzed black carbon from an Antarctic ice core spanning 1968–2015 and observed very low concentrations of this particle in the snow, lower than previous works in West Antarctica. We suggest that black carbon transport to East Antarctica is different from its transport to West Antarctica.