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https://hdl.handle.net/20.500.14279/14256
Title: | EARLINET observations of the 14-22-May long-range dust transport event during SAMUM 2006: Validation of results from dust transport modelling | Authors: | Müller, Detlef Heinold, Bernd Tesche, Matthias Tegen, Ina Althausen, Dietrich Alados-Arboledas, Lucas Amiridis, Vassilis Amodeo, Aldo Ansmann, Albert Balis, Dimitris S. Comerón, Adolfo D'Amico, Giuseppe Gerasopoulos, Evangelos Guerrero-Rascado, J. L. Freudenthaler, Volker Giannakaki, Elina Heese, Birgit Iarlori, Marco Knippertz, Peter Mamouri, Rodanthi-Elisavet Mona, Lucia Papayannis, Alexandros D. Pappalardo, Gelsomina Perrone, Roberto M. Pisani, Gianluca Rizi, Vincenzo Sicard, Michaël Spinelli, Nicola Tafuro, Anna Maria Wiegner, Matthias |
Major Field of Science: | Engineering and Technology | Field Category: | Environmental Engineering | Keywords: | Aerosol;Dust;Dust aerosols | Issue Date: | 3-Feb-2009 | Source: | Tellus B: Chemical and Physical Meteorology, 2009, vol. 61, no. 1, pp. 325-339 | Volume: | 61 | Issue: | 1 | Start page: | 325 | End page: | 339 | Journal: | Tellus B: Chemical and Physical Meteorology | Abstract: | We observed a long-range transport event of mineral dust from North Africa to South Europe during the Saharan Mineral Dust Experiment (SAMUM) 2006. Geometrical and optical properties of that dust plume were determined with Sun photometer of the Aerosol Robotic Network (AERONET) and Raman lidar near the North African source region, and with Sun photometers of AERONET and lidars of the European Aerosol Research Lidar Network (EARLINET) in the far field in Europe. Extinction-to-backscatter ratios of the dust plume over Morocco and Southern Europe do not differ. Ångström exponents increase with distance from Morocco. We simulated the transport, and geometrical and optical properties of the dust plume with a dust transport model. The model results and the experimental data show similar times regarding the appearance of the dust plume over each EARLINET site. Dust optical depth from the model agrees in most cases to particle optical depth measured with the Sun photometers. The vertical distribution of the mineral dust could be satisfactorily reproduced, if we use as benchmark the extinction profiles measured with lidar. In some cases we find differences. We assume that insufficient vertical resolution of the dust plume in the model calculations is one reason for these deviations. | ISSN: | 16000889 | DOI: | 10.1111/j.1600-0889.2008.00400.x | Rights: | © 2009 The Author(s). | Type: | Article | Affiliation : | Cyprus University of Technology Leibniz Institute for Tropospheric Research University of Granada National Observatory of Athens CNR - National Research Council of Italy Aristotle University of Thessaloniki Universitat Politècnica de Catalunya Ludwig Maximilians University Universitádegli Studi - L'Aquila Johannes Gutenberg University of Mainz National Technical University Of Athens Universitá degli Studi di Lecce Universitá degli Studi di Napoli Federico II Gwangju Institute of Science and Technology |
Publication Type: | Peer Reviewed |
Appears in Collections: | Άρθρα/Articles |
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EARLINET.pdf | Fulltext | 1.41 MB | Adobe PDF | View/Open |
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