The ash dispersion over Europe during the Eyjafjallajokull eruption - Comparison of CMAQ simulations to remote sensing and air-borne in-situ observations

被引:30
作者
Matthias, Volker [1 ]
Aulinger, Armin [1 ]
Bieser, Johannes [1 ]
Cuesta, Juan [2 ,3 ]
Geyer, Beate [1 ]
Langmann, Baerbel [5 ]
Serikov, Ilya [6 ]
Mattis, Ina [7 ]
Minikin, Andreas [8 ]
Mona, Lucia [4 ]
Quante, Markus [1 ]
Schumann, Ulrich [8 ]
Weinzierl, Bernadett [8 ]
机构
[1] Helmholtz Zentrum Geesthacht, Inst Coastal Res, Max Planck Str 1, D-21502 Geesthacht, Germany
[2] UPEC, LISA, F-94010 Creteil, France
[3] Lab Atmospheres Milieux Observat Spatiales LATMOS, F-75252 Paris, France
[4] CNR, IMAA, I-85050 Potenza, Italy
[5] Univ Hamburg, Inst Geophys, D-20146 Hamburg, Germany
[6] Max Planck Inst Meteorol, D-20146 Hamburg, Germany
[7] Leibniz Inst Tropospher Res, D-04318 Leipzig, Germany
[8] Deutsch Zentrum Luft & Raumfahrt DLR, Inst Phys Atmosphare, D-82230 Oberpfaffenhofen, Germany
关键词
Volcanic eruption; Ash dispersion; Chemistry transport model; Lidar; Sun photometer; Ash concentration; VOLCANIC ASH; LIDAR MEASUREMENTS; OPTICAL DEPTH; AEROSOL; MODEL; CLOUD; EXTINCTION; EMISSIONS; TRANSPORT; AERONET;
D O I
10.1016/j.atmosenv.2011.06.077
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The dispersion of volcanic ash over Europe after the outbreak of the Eyjafjallajokull on Iceland on 14 April 2010 has been simulated with a conventional three-dimensional Eulerian chemistry transport model system, the Community Multiscale Air Quality (CMAQ) model. Four different emission scenarios representing the lower and upper bounds of the emission height and intensity were considered. The atmospheric ash concentrations turned out to be highly variable in time and space. The model results were compared to three different kinds of observations: Aeronet aerosol optical depth (AOD) measurements, Earlinet aerosol extinction profiles and in-situ observations of the ash concentration by means of optical particle counters aboard the DLR Falcon aircraft. The model was able to reproduce observed AOD values and atmospheric ash concentrations. Best agreement was achieved for lower emission heights and a fraction of 2% transportable ash in the total volcanic emissions. The complex vertical structure of the volcanic ash layers in the free troposphere could not be simulated. Compared to the observations, the model tends to show vertically more extended, homogeneous aerosol layers. This is caused by a poor vertical resolution of the model at higher altitudes and a lack of information about the vertical distribution of the volcanic emissions. Only a combination of quickly available observations of the volcanic ash cloud and atmospheric transport models can give a comprehensive picture of ash concentrations in the atmosphere. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:184 / 194
页数:11
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