Mineral Dust Cycle

Mineral Dust Cycle

Mineral dust  aerosols produced  by wind erosion in arid and semi-arid regions contribute for more than 40% of the total annual emissions of tropospheric aerosols. In the atmosphere, these aerosols influence the terrestrial radiative balance and are thus major contributors to climate forcing. Dust deposition is a significant source of nutrients (Fe, P, …) for remote oceanic ecosystems regions, while dust emission contributes to soil loss in source regions. The research activities carried at LISA in this field are mainly focused on the quantification of dust emissions, transport and deposition, in order to assess their radiative and biogeochemical impacts. For this objective, intensive (ground-based and airborne) and longterm field measurements and laboratory experiments are coupled with numerical simulations.


M. Boraiy, M. Korany, Y. Aoun, Stephane Alfaro, M. El-Metwally, M. M. Abdel Wahab, P. Blanc, Y. Eissa, H. Ghedira, Guillaume Siour, K. Hungershoefer, and L. Wald

Including aerosol optical depth improves existing models for the retrieval in cloud-free conditions of the direct normal from the measured global irradiance in Egypt
Meteorologische Zeitschrift

Sunday 24 September 2017
Kangasluoma J., S. Hering2, D. Picard, G. Lewis, J. Enroth, F. Korhonen, M. Kulmala, K. Sellegri, Michell Attoui, T. Petäjä

Characterization of three new condensation particle counters for sub-3 nm particle detection during the Helsinki CPC workshop: the ADI versatile water CPC, TSI 3777 nano enhancer and boosted TSI 3010
Atmos. Meas. Tech.

Monday 19 June 2017
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