About this Journal Submit a Manuscript Table of Contents
Advances in Meteorology
Volume 2012 (2012), Article ID 674385, 14 pages
Review Article

Characterization of Modern and Fossil Mineral Dust Transported to High Altitude in the Western Alps: Saharan Sources and Transport Patterns

1Institute F.-A. Forel, University of Geneva, Versoix, Switzerland
2Department of Mineralogy, University of Geneva, Geneva, Switzerland
3Institute of Geology and Palaeontology, University of Lausanne, Lausanne, Switzerland
4Swiss Federal Laboratories for Materials Testing and Research (EMPA), Dübendorf, Switzerland

Received 27 September 2011; Revised 14 December 2011; Accepted 15 January 2012

Academic Editor: Ralph A. Kahn

Copyright © 2012 Florian Thevenon et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


Mineral dust aerosols recently collected at the high-altitude Jungfraujoch research station ( N, E; 3580 m a.s.l.) were compared to mineral dust deposited at the Colle Gnifetti glacier ( N, E; 4455 m a.s.l.) over the last millennium. Radiogenic isotope signatures and backward trajectories analyses indicate that major dust sources are situated in the north-central to north-western part of the Saharan desert. Less radiogenic Sr isotopic compositions of PM10 aerosols and of mineral particles deposited during periods of low dust transfer likely result from the enhancement of the background chemically-weathered Saharan source. Saharan dust mobilization and transport were relatively reduced during the second part of the Little Ice Age (ca. 1690–1870) except within the greatest Saharan dust event deposited around 1770. After ca. 1870, sustained dust deposition suggests that increased mineral dust transport over the Alps during the last century could be due to stronger spring/summer North Atlantic southwesterlies and drier winters in North Africa. On the other hand, increasing carbonaceous particle emissions from fossil fuel combustion combined to a higher lead enrichment factor point to concomitant anthropogenic sources of particulate pollutants reaching high-altitude European glaciers during the last century.