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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
https://doi.org/10.5194/acp-2017-131
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
16 Feb 2017
Review status
A revision of this discussion paper was accepted for the journal Atmospheric Chemistry and Physics (ACP) and is expected to appear here in due course.
Seasonal provenance changes of present-day Saharan dust collected on- and offshore Mauritania
Carmen A. Friese1, Hans van Hateren2,a, Christoph Vogt1,3, Gerhard Fischer1, and Jan-Berend W. Stuut1,2 1Marum – Center of Marine Environmental Sciences, University of Bremen, Bremen, 28359, Germany
2NIOZ – Royal Netherlands Ins t itute for Sea Research, Department of Ocean Systems, and Utrecht University, 1790 AB, Den Burg Texel, Netherlands
3ZEKAM, Crystallography, Geosciences, University of Bremen, 28359, Germany
anow at: Vrije Universiteit Amsterdam, Faculty of Earth Sciences, 1081 HV Amsterdam, the Netherlands
Abstract. Saharan dust has a crucial influence on the earth climate system and its emission, transport, and deposition are intimately related to environmental parameters. The alteration in the physical and chemical properties of Saharan dust due to changes in environmental parameters is often used to reconstruct the climate of the past. However, to better interpret possible climate changes the dust source regions need to be known. By analysing the mineralogical composition of transported or deposited dust, potential dust source areas can be inferred. Summer dust transport offshore Northwest Africa occurs in the Saharan air layer (SAL). In contrast, dust transport in continental dust source areas occurs predominantly with the trade winds. Hence, the source regions and related mineralogical tracers differ with season and sampling location. To test this, dust collected in traps onshore and in oceanic sediment traps offshore Mauritania during 2013 to 2015 was analysed. Meteorological data, particle-size distributions, back-trajectory and mineralogical analyses were compared to derive the dust provenance and dispersal. For the onshore dust samples, the source regions varied according to the seasonal changes in trade-wind direction. Gibbsite and dolomite indicated a Western Saharan and local source during summer, while chlorite, serpentine and rutile indicated a source in Mauritania and Mali during winter. In contrast, for the samples that were collected offshore, dust sources varied according to the seasonal change in the dust transporting air layer. In summer, dust was transported in the SAL from Mauritania, Mali and Libya as indicated by ferryglaucophane and zeolite. In winter, dust was transported with the Trades from the Western Sahara as indicated by e.g. sepiolite and fluellite.

Citation: Friese, C. A., van Hateren, H., Vogt, C., Fischer, G., and Stuut, J.-B. W.: Seasonal provenance changes of present-day Saharan dust collected on- and offshore Mauritania, Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2017-131, in review, 2017.
Carmen A. Friese et al.
Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Review', Anonymous Referee #1, 31 Mar 2017 Printer-friendly Version 
 
RC2: 'Review of "Seasonal provenance changes of present-day Saharan dust collected on- and offshore Mauritania"', Anonymous Referee #2, 31 Mar 2017 Printer-friendly Version 
 
AC1: 'Response to reviewer comments', Carmen Friese, 16 Jun 2017 Printer-friendly Version Supplement 
Carmen A. Friese et al.
Carmen A. Friese et al.

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