The Cryosphere
The Cryosphere
TC
Articles | Volume 15, issue 3
Articles | Volume 15, issue 3
https://doi.org/10.5194/tc-15-1383-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-1383-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 15, issue 3
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: 2,958 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,019 824 115 2,958 317 122 139
  • HTML: 2,019
  • PDF: 824
  • XML: 115
  • Total: 2,958
  • Supplement: 317
  • BibTeX: 122
  • EndNote: 139
Views and downloads (calculated since 08 Apr 2020)
Cumulative views and downloads (calculated since 08 Apr 2020)

Viewed (geographical distribution)

Total article views: 2,958 (including HTML, PDF, and XML) Thereof 2,797 with geography defined and 161 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jul 2025
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.
Read more
Share