Articles | Volume 18, issue 21
https://doi.org/10.5194/acp-18-15859-2018
https://doi.org/10.5194/acp-18-15859-2018
Research article
 | 
06 Nov 2018
Research article |  | 06 Nov 2018

Long-range transport of volcanic aerosol from the 2010 Merapi tropical eruption to Antarctica

Xue Wu, Sabine Griessbach, and Lars Hoffmann

Viewed

Total article views: 3,012 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,073 865 74 3,012 73 82
  • HTML: 2,073
  • PDF: 865
  • XML: 74
  • Total: 3,012
  • BibTeX: 73
  • EndNote: 82
Views and downloads (calculated since 22 May 2018)
Cumulative views and downloads (calculated since 22 May 2018)

Viewed (geographical distribution)

Total article views: 3,012 (including HTML, PDF, and XML) Thereof 2,998 with geography defined and 14 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
Volcanic aerosol is an important source of sulfur for Antarctica, where local sources of sulfur are rare. Midlatitude and high-latitude volcanism can directly influence the aerosol budget of the polar stratosphere, but tropical volcanic eruptions can also enhance polar aerosols by transport. Our study investigates pathway and transport processes of volcanic aerosol from the tropics to the lower stratosphere over Antarctica by combining Lagrangian transport simulation and satellite observations.
Altmetrics
Final-revised paper
Preprint