Articles | Volume 15, issue 3
https://doi.org/10.5194/tc-15-1383-2021
https://doi.org/10.5194/tc-15-1383-2021
Research article
 | 
16 Mar 2021
Research article |  | 16 Mar 2021

Giant dust particles at Nevado Illimani: a proxy of summertime deep convection over the Bolivian Altiplano

Filipe G. L. Lindau, Jefferson C. Simões, Barbara Delmonte, Patrick Ginot, Giovanni Baccolo, Chiara I. Paleari, Elena Di Stefano, Elena Korotkikh, Douglas S. Introne, Valter Maggi, Eduardo Garzanti, and Sergio Andò

Viewed

Total article views: 2,350 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,566 694 90 2,350 258 82 85
  • HTML: 1,566
  • PDF: 694
  • XML: 90
  • Total: 2,350
  • Supplement: 258
  • BibTeX: 82
  • EndNote: 85
Views and downloads (calculated since 08 Apr 2020)
Cumulative views and downloads (calculated since 08 Apr 2020)

Viewed (geographical distribution)

Total article views: 2,350 (including HTML, PDF, and XML) Thereof 2,207 with geography defined and 143 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Download
Short summary
Information about the past climate variability in tropical South America is stored in the snow layers of the tropical Andean glaciers. Here we show evidence that the presence of very large aeolian mineral dust particles at Nevado Illimani (Bolivia) is strictly controlled by the occurrence of summer storms in the Bolivian Altiplano. Therefore, based on the snow dust content and its composition of stable water isotopes, we propose a new proxy for information on previous summer storms.