Articles | Volume 15, issue 3
https://doi.org/10.5194/tc-15-1627-2021
https://doi.org/10.5194/tc-15-1627-2021
Research article
 | 
01 Apr 2021
Research article |  | 01 Apr 2021

Heterogeneous CO2 and CH4 content of glacial meltwater from the Greenland Ice Sheet and implications for subglacial carbon processes

Andrea J. Pain, Jonathan B. Martin, Ellen E. Martin, Åsa K. Rennermalm, and Shaily Rahman

Viewed

Total article views: 3,070 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,126 835 109 3,070 157 96 109
  • HTML: 2,126
  • PDF: 835
  • XML: 109
  • Total: 3,070
  • Supplement: 157
  • BibTeX: 96
  • EndNote: 109
Views and downloads (calculated since 03 Jul 2020)
Cumulative views and downloads (calculated since 03 Jul 2020)

Viewed (geographical distribution)

Total article views: 3,070 (including HTML, PDF, and XML) Thereof 2,906 with geography defined and 164 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 22 Nov 2024
Download
Short summary
The greenhouse gases (GHGs) methane and carbon dioxide can be produced or consumed by geochemical processes under the Greenland Ice Sheet (GrIS). Chemical signatures and concentrations of GHGs in GrIS discharge show that organic matter remineralization produces GHGs in some locations, but mineral weathering dominates and consumes CO2 in other locations. Local processes will therefore determine whether melting of the GrIS is a positive or negative feedback on climate change driven by GHG forcing.