van der Does, Michélle; Korte, Laura F; Munday, Chris I; Brummer, Geert-Jan A; Stuut, Jan-Berend W (2016): Particle size of Saharan dust in the Atlantic Ocean, from October 2012 to November 2013. PANGAEA, https://doi.org/10.1594/PANGAEA.863030, Supplement to: van der Does, M et al. (2016): Particle size traces modern Saharan dust transport and deposition across the equatorial North Atlantic. Atmospheric Chemistry and Physics, 16(21), 13697-13710, https://doi.org/10.5194/acp-16-13697-2016
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Mineral dust has a large impact on regional and global climate, depending on its particle size. Especially in the Atlantic Ocean downwind of the Sahara, the largest dust source on earth, the effects can be substantial but are poorly understood. This study focuses on seasonal and spatial variations in particle size of Saharan dust deposition across the Atlantic Ocean, using an array of submarine sediment traps moored along a transect at 12° N. We show that the particle size decreases downwind with increased distance from the Saharan source, due to higher gravitational settling velocities of coarse particles in the atmosphere. Modal grain sizes vary between 4 and 33 µm throughout the different seasons and at five locations along the transect. This is much coarser than previously suggested and incorporated into climate models. In addition, seasonal changes are prominent, with coarser dust in summer, and finer dust in winter and spring. Such seasonal changes are caused by transport at higher altitudes and at greater wind velocities during summer than in winter. Also the latitudinal migration of the dust cloud, associated with the Intertropical Convergence Zone, causes seasonal differences in deposition as the summer dust cloud is located more to the north, and more directly above the sampled transect. Furthermore, increased precipitation and more frequent dust storms in summer coincide with coarser dust deposition. Our findings contribute to understanding Saharan dust transport and deposition relevant for the interpretation of sedimentary records for climate reconstructions, as well as for global and regional models for improved prediction of future climate.
Stuut, Jan-Berend W; Boersen, Barry; Brück, Matthias; Hansen, Akio; Koster, Bob; van der Does, Michélle; Witte, Yvo (2014): TRAFFIC: Transatlantic fluxes of Saharan dust - Cruise No. M89 - October 3 - October 25, 2012 - Las Palmas de Gran Canaria (Spain) - Cristobal (Panama). METEOR-Berichte, DFG-Senatskommission für Ozeanographie, M89, 30 pp, https://doi.org/10.2312/cr_m89
Stuut, Jan-Berend W; Brummer, Geert-Jan A; van der Does, Michélle; Friese, Carmen A; Geerken, Esmee; van der Heide, Roald; Korte, Laura F; Koster, Bob; Metcalfe, Brett; Munday, Chris I; van Ooijen, Jan C; Siccha, Michael; Veldhuizen, Ronald; de Visser, Jan-Dirk; Witte, Yvo; Wuis, Leon (2014): Cruise Report and preliminary results - TRAFFIC II: Transatlantic fluxes of Saharan dust - Cruise No. 64PE378 - 9 November – 6 December 2013 - Las Palmas de Gran Canaria (Spain) – St Maarten. Royal Netherlands Institute for Sea Research, 50 pp, hdl:10013/epic.48173.d001
Median Latitude: 12.381000 * Median Longitude: -34.166000 * South-bound Latitude: 12.000000 * West-bound Longitude: -57.040000 * North-bound Latitude: 13.810000 * East-bound Longitude: -23.000000
Date/Time Start: 2012-10-07T12:18:00 * Date/Time End: 2013-10-30T12:00:00
Saharan dust from sediment-trap samples, moored along a transect in the Atlantic Ocean at 12° N. Samples collected between October 2012 and November 2013. Part of the TRAFFIC (NWO) and DUSTTRAFFIC (ERC) projects.