The electrical activity of Saharan dust as perceived from surface electric field observations
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Published:2021-01-25
Issue:2
Volume:21
Page:927-949
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Daskalopoulou VasilikiORCID, Mallios Sotirios A.ORCID, Ulanowski ZbigniewORCID, Hloupis George, Gialitaki AnnaORCID, Tsikoudi IoannaORCID, Tassis KonstantinosORCID, Amiridis VassilisORCID
Abstract
Abstract. We report on the electric field variations during Saharan
dust advection over two atmospheric remote stations in Greece, using
synergistic observations of the vertical atmospheric electric field strength
(Ez) at ground level and the lidar-derived particle
backscatter coefficient profiles. Both parameters were monitored for the
first time with the simultaneous deployment of a ground-based field mill
electrometer and a multi-wavelength polarization lidar. The field mill
time series are processed to extract the diurnal variations of the global
electric circuit and remove fast field perturbations due to peak lightning
activity. In order to identify the influence of the elevated dust layers on
the ground Ez, we extract a localized reference
electric field from the time series that reflects the local fair-weather
activity. Then, we compare it with the reconstructed daily average behaviour
of the electric field and the Saharan dust layers' evolution, as depicted by
the lidar. The observed enhancement of the vertical electric field (up to
∼100 V m−1), for detached pure dust layers, suggests the
presence of in-layer electric charges. Although higher dust loads are
expected to result in such an electric field enhancement, episodic cases
that reduce the electric field are also observed (up to ∼60 V m−1). To quantitatively approach our results, we examine the dependency of
Ez against theoretical assumptions for the
distribution of separated charges within the electrified dust layer.
Electrically neutral dust is approximated by atmospheric conductivity
reduction, while charge separation areas within electrically active dust
layers are approximated as finite-extent cylinders. This physical
approximation constitutes a more realistic description of the distribution
of charges, as opposed to infinite-extent geometries, and allows for
analytical solutions of the electric field strength so that observed
variations during the monitored dust outbreaks can be explained.
Funder
European Social Fund H2020 European Research Council
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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