Preprints
https://doi.org/10.5194/egusphere-2025-3577
https://doi.org/10.5194/egusphere-2025-3577
29 Aug 2025
 | 29 Aug 2025
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Saharan and Arabian dust optical properties registered by sun photometry during A-LIFE field experiment in Cyprus

David Mateos, Carlos Toledano, Abel Calle, Roberto Román, Marcos Herreras-Giralda, Ramiro González, Sara Herrero-Anta, Daniel González-Fernández, Celia Herrero-del Barrio, Argyro Nisantzi, Silke Gross, Victoria E. Cachorro, Ángel M. de Frutos, and Bernadett Weinzierl

Abstract. The A-LIFE (Absorbing aerosol layers in a changing climate: aging, lifetime, and dynamics) field experiment in Cyprus (April 2017) employed a wide range of ground-based and airborne instruments, including passive/active remote sensing and in-situ techniques. This study presents the columnar records obtained by sun photometry. Two sun/sky/lunar photometers, belonging to AERONET network, were strategically placed at two different sites: Pafos and Limassol, 40 km apart. Aerosol optical and microphysical properties derived from direct sun and sky radiance measurements are analysed to determine an inventory of aerosol event days during the whole experiment, with mineral dust being predominant. Obtained Ångström exponent values in the near-infrared range (0.5 for Saharan dust and 0.34 for Arabian dust) can served as a classification criterion. Dust sources are the key point for a well understanding of the size distribution and absorption power. Saharan dust exhibited smaller and less absorbing particles than Arabian dust. The columnar volume efficiency factor (linear fit between aerosol optical depth and total volume concentration) was proved as a reliable proxy for the identification of dust origin since Arabian and Saharan dusts exhibit different slopes: 1.28 and 1.68 μm2/μm3, respectively. Mixtures of mineral dust were mainly dominated by Arabian dust, while mixtures of fine and coarse aerosols showed no clear prevalence of dust origin. No significant presence of black carbon-rich aerosols was detected in the atmospheric column, as absorption Ångström exponent values ranged from 1.6 to 3 across aerosol types identified in the inventory of A-LIFE experiment.

Competing interests: Silke Gross is member of the editorial board of ACP journal.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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David Mateos, Carlos Toledano, Abel Calle, Roberto Román, Marcos Herreras-Giralda, Ramiro González, Sara Herrero-Anta, Daniel González-Fernández, Celia Herrero-del Barrio, Argyro Nisantzi, Silke Gross, Victoria E. Cachorro, Ángel M. de Frutos, and Bernadett Weinzierl

Status: open (until 10 Oct 2025)

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David Mateos, Carlos Toledano, Abel Calle, Roberto Román, Marcos Herreras-Giralda, Ramiro González, Sara Herrero-Anta, Daniel González-Fernández, Celia Herrero-del Barrio, Argyro Nisantzi, Silke Gross, Victoria E. Cachorro, Ángel M. de Frutos, and Bernadett Weinzierl
David Mateos, Carlos Toledano, Abel Calle, Roberto Román, Marcos Herreras-Giralda, Ramiro González, Sara Herrero-Anta, Daniel González-Fernández, Celia Herrero-del Barrio, Argyro Nisantzi, Silke Gross, Victoria E. Cachorro, Ángel M. de Frutos, and Bernadett Weinzierl

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Short summary
The A-LIFE experiment deployed in Cyprus included two sun photometers of AERONET network in two different sites. Mineral dust was predominant during the experiment, with Saharan and Arabian dust showing distinct optical properties, in particular, the Angstrom Exponent in the near-infrarred range and Volume Efficiency factor. Both magnitudes can served as a reliable proxy for mineral dust typing. No significant black carbon presence was detected.
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