Articles | Volume 17, issue 20
https://doi.org/10.5194/acp-17-12779-2017
https://doi.org/10.5194/acp-17-12779-2017
Research article
 | 
26 Oct 2017
Research article |  | 26 Oct 2017

Do contemporary (1980–2015) emissions determine the elemental carbon deposition trend at Holtedahlfonna glacier, Svalbard?

Meri M. Ruppel, Joana Soares, Jean-Charles Gallet, Elisabeth Isaksson, Tõnu Martma, Jonas Svensson, Jack Kohler, Christina A. Pedersen, Sirkku Manninen, Atte Korhola, and Johan Ström

Viewed

Total article views: 2,955 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,956 851 148 2,955 74 97
  • HTML: 1,956
  • PDF: 851
  • XML: 148
  • Total: 2,955
  • BibTeX: 74
  • EndNote: 97
Views and downloads (calculated since 05 May 2017)
Cumulative views and downloads (calculated since 05 May 2017)

Viewed (geographical distribution)

Total article views: 2,955 (including HTML, PDF, and XML) Thereof 2,923 with geography defined and 32 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 12 Nov 2024
Download
Short summary
Black carbon (BC) deposition enhances Arctic warming and melting. We present Svalbard ice core BC data from 2005 to 2015, comparing the results with chemical transport model data. The ice core and modelled BC deposition trends clearly deviate from measured and observed atmospheric concentration trends, and thus meteorological processes such as precipitation and scavenging efficiency seem to have a stronger influence on the BC deposition trend than BC emission or atmospheric concentration trends.
Altmetrics
Final-revised paper
Preprint