Stuut, Jan-Berend W; Zabel, Matthias; Ratmeyer, Volker; Helmke, Peer; Schefuß, Enno; Lavik, Gaute; Schneider, Ralph R (2005): Grain size distribution and bulk chemistry of eolian dust. PANGAEA, https://doi.org/10.1594/PANGAEA.739147, Supplement to: Stuut, J-BW et al. (2005): Provenance of present-day eolian dust collected off NW Africa. Journal of Geophysical Research: Atmospheres, 110, D04202, https://doi.org/10.1029/2004JD005161
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Atmospheric dust samples collected along a transect off the West African coast have been investigated for their physical (grain-size distribution), mineralogical, and chemical (major elements) composition. On the basis of these data the samples were grouped into sets of samples that most likely originated from the same source area. In addition, shipboard-collected atmospheric meteorological data, modeled 4-day back trajectories for each sampling day and location, and Total Ozone Mapping Spectrometer aerosol index data for the time period of dust collection (February-March 1998) were combined and used to reconstruct the sources of the groups of dust samples. On the basis of these data we were able to determine the provenance of the various dust samples. It appears that the bulk of the wind-blown sediments that are deposited in the proximal equatorial Atlantic Ocean are transported in the lower level (>~900 hPa) NE trade wind layer, which is a very dominant feature north of the Intertropical Convergence Zone (ITCZ). However, south of the surface expression of the ITCZ, down to 5°S, where surface winds are southwesterly, we still collected sediments that originated from the north and east, carried there by the NE trade wind layer, as well as by easterly winds from higher altitudes. The fact that the size of the wind-blown dust depends not only on the wind strength of the transporting agent but also on the distance to the source hampers a direct comparison of the dust's size distributions and measured wind strengths. However, a comparison between eolian dust and terrigenous sediments collected in three submarine sediment traps off the west coast of NW Africa shows that knowledge of the composition of eolian dust is a prerequisite for the interpretation of paleorecords obtained from sediment cores in the equatorial Atlantic.
Median Latitude: 6.618751 * Median Longitude: -1.765031 * South-bound Latitude: -11.469200 * West-bound Longitude: -17.930000 * North-bound Latitude: 32.417800 * East-bound Longitude: 12.858900
Date/Time Start: 1998-02-15T00:00:00 * Date/Time End: 1998-03-11T00:00:00
M41/1_D1 (D1) * Latitude: 30.440000 * Longitude: -11.720000 * Date/Time: 1998-02-15T00:00:00 * Campaign: M41/1 * Basis: Meteor (1986) * Method/Device: Aeolian dust sample (AEOLD) * Comment: Sampling was conducted with Andersen high-volume particulate matter dust samplers installed on the ship`s tower.
M41/1_D2 * Latitude Start: 28.420800 * Longitude Start: -13.512500 * Latitude End: 24.937500 * Longitude End: -16.886700 * Date/Time Start: 1998-02-15T17:25:00 * Date/Time End: 1998-02-15T22:30:00 * Campaign: M41/1 * Basis: Meteor (1986) * Method/Device: Aeolian dust sample (AEOLD)
M41/1_D3 (D3) * Latitude: 22.890000 * Longitude: -17.440000 * Date/Time: 1998-02-17T00:00:00 * Campaign: M41/1 * Basis: Meteor (1986) * Method/Device: Aeolian dust sample (AEOLD) * Comment: Sampling was conducted with Andersen high-volume particulate matter dust samplers installed on the ship`s tower.
Datasets listed in this publication series
- Stuut, J-BW; Zabel, M; Ratmeyer, V et al. (2005): Bulk chemistry analyses of atmospheric dust samples along a transect off the West African coast. https://doi.org/10.1594/PANGAEA.499740
- Stuut, J-BW; Zabel, M; Ratmeyer, V et al. (2005): Grain-size distributions of atmospheric dust samples along a transect off the West African coast. https://doi.org/10.1594/PANGAEA.496677
- Stuut, J-BW; Zabel, M; Ratmeyer, V et al. (2005): (Table 1) Maximum wind speed, wind direction, altitude, and pressure of dust samples, measured by weather balloons from the Deutsche Wetterdienst onboard FS Meteor during cruise M41/1. https://doi.org/10.1594/PANGAEA.510726