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

<table>(Top) Panorama from the south of the Monte Rosa Massif showing the location of the ice core site (Colle Gnifetti glacier, CG) and the Grenz Glacier. (Bottom) Geographical map showing the 315-hour backward trajectories arriving at Jungfraujoch (JFJ), reconstructed using the NOAA HYSPLIT model (<a href="http://ready.arl.noaa.gov/HYSPLIT.php">http://ready.arl.noaa.gov/HYSPLIT.php</a>).</table>

Advances in Meteorology

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Figure 1

Figure 1: Characterization of Modern and Fossil Mineral Dust Transported to High Altitude in the Western Alps: Saharan Sources and Transport Patterns 

Figure 1 | Characterization of Modern and Fossil Mineral Dust Transported to High Altitude in the Western Alps: Saharan Sources and Transport Patterns 