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Volume 13, issue 7 | Copyright

Special issue: Observations and modeling of aerosol and cloud properties...

Atmos. Chem. Phys., 13, 3705-3720, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 04 Apr 2013

Research article | 04 Apr 2013

Detection and characterization of volcanic ash plumes over Lille during the Eyjafjallajökull eruption

A. Mortier1, P. Goloub1, T. Podvin1, C. Deroo1, A. Chaikovsky2, N. Ajtai3, L. Blarel1, D. Tanre1, and Y. Derimian1 A. Mortier et al.
  • 1Laboratoire d'Optique Atmosphérique, CNRS, UMR8518, Université Lille 1, Villeneuve d'Ascq, France
  • 2Laboratory of Optics of Scattering Media, Stepanov Institute, Academy of Science of Belarus, Minsk, Belarus
  • 3Research Center for Disaster Management, Faculty of Environmental Science and Engineering, Babeş-Bolyaï University, Cluj-Napoca, Romania

Abstract. Routine sun-photometer and micro-lidar measurements were performed in Lille, northern France, in April and May 2010 during the Eyjafjallajökull volcanic eruption. The impact of such an eruption emphasized significance of hazards for human activities and importance of observations of the volcanic aerosol particles. This paper presents the main results of a joint micro-lidar/sun-photometer analysis performed in Lille, where volcanic ash plumes were observed during at least 22 days, whenever weather conditions permitted. Aerosol properties retrieved from automatic sun-photometer measurements (AERONET) were strongly changed during the volcanic aerosol plumes transport over Lille. In most cases, the aerosol optical depth (AOD) increased, whereas Ångström exponent decreased, thus indicating coarse-mode dominance in the volume size distribution. Moreover, the non-spherical fraction retrieved by AERONET significantly increased. The real part of the complex refractive index was up to 1.55 at 440 nm during the eruption, compared to background data of about 1.46 before the eruption. Collocated lidar data revealed that several aerosol layers were present between 2 and 5 km, all originating from the Iceland region as confirmed by backward trajectories. The volcanic ash AOD was derived from lidar extinction profiles and sun-photometer AOD, and its maximum was estimated around 0.37 at 532 nm on 18 April 2010. This value was observed at an altitude of 1700 m and corresponds to an ash mass concentration (AMC) slightly higher than 1000 μg m−3 (±50%). An effective lidar ratio of ash particles of 48 sr was retrieved at 532 nm for 17 April during the early stages of the eruption, a value which agrees with several other studies carried out on this topic. Even though the accuracy of the retrievals is not as high as that obtained from reference multiwavelength lidar systems, this study demonstrates the opportunity of micro-lidar and sun-photometer joint data processing for deriving volcanic AMC. It also outlines the fact that a network of combined micro-lidars and sun photometers can be a powerful tool for routine monitoring of aerosols, especially in the case of such hazardous volcanic events.

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