Transport of Saharan dust from the Bodele Depression to the Amazon Basin: a case study

Abstract

Through long-range transport of dust, the Sahara desert supplies essential minerals to the Amazon rain forest. Since Saharan dust reaches South America mostly during the Northern Hemisphere winter, the dust sources active during winter are the main contributors to the forest. Given that the Bodele depression area in Southwestern Chad 5 is the main winter dust source, a close link is expected between the Bod ́ el ́ e emission patterns and volumes and the mineral supply flux to the Amazon. Until now, the particular link between the Bod ́ el ́ e and the Amazon forest was based on sparse satellite measurements and modeling studies. In this study, we combine a detailed analysis of space-borne and ground data with reanalysis model data and 10 surface measurements taken in the Central Amazon during the Amazonian Aerosol Characterization Experiment (AMAZE-08) in order to explore the validity and the nature of the proposed link between the Bodele depression and the Amazon forest. This case study follows the dust events of 11–16 and 18–27 February 2008, from the emission in the Bodele over West Africa, the crossing of the Atlantic Ocean, to the 15 observed e ff ects above the Amazon canopy about 10days after the emission. The dust was lifted by surface winds stronger than 14ms − 1 , usually starting early in the morning. The lofted dust mixed with biomass burning aerosols over Nigeria, was transported over the Atlantic Ocean, and arrived over the South American continent. The top of the aerosol layer reached above 3km, and the bottom merged with the marine boundary 20 layer. The arrival of the dusty air parcel over the Amazon forest increased the average concentration of aerosol crustal elements by an order of magnitude