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Investigation of the complex dynamics and structure of the 2010 Eyjafjallajökull volcanic ash cloud using multispectral images and numerical simulations
Author(s)
Language
English
Obiettivo Specifico
3V. Dinamiche e scenari eruttivi
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Issue/vol(year)
/118 (2013)
ISSN
0148-0227
Publisher
American Geophysical Union
Pages (printed)
4729–4747
Issued date
2013
Abstract
We investigated the structure and evolution of the 2010 Eyjafjallajökull volcanic cloud
and its dispersal over Iceland and Europe integrating satellite multispectral images and numerical simulations. Data acquired by Medium Resolution Imaging Spectrometer (MERIS)and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) have been analyzed to quantify the cloud extent and composition. The VOL-CALPUFF dispersal code
was applied to reconstruct the transient and 3-D evolution of the cloud. Source parameters estimated on the base of available a posteriori volcanological data sets have been used. Quantitative comparisons between satellite retrievals and modeling results were performed for two selected instants of time during the first and third eruptive phases on a regional scale. Sensitivity of the model to initial volcanological conditions has been analyzed at continental scale. Several complex non intuitive features of cloud dynamics have been highlighted and
strengths and limitations of the adopted methods identified. The main findings are: the level of
quantitative agreement between satellite observations and numerical results depends on ash
cloud composition (particle sizes and concentration) with better agreement for smaller
particles and higher concentrations; the agreement between observations and modeling
outcomes also depends on the temporal stability of volcanological conditions and the
complexity of the meteorological wind field; the irregular dispersion of ash, as reconstructed
from satellite data and numerical modeling, can be well explained by the different response of
particle sizes to strong vertical wind-shear, and by resuspension processes acting at ground level; eruptive source conditions are the main source of uncertainty in modeling, especially during an ongoing crisis and at long-range scales.
and its dispersal over Iceland and Europe integrating satellite multispectral images and numerical simulations. Data acquired by Medium Resolution Imaging Spectrometer (MERIS)and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) have been analyzed to quantify the cloud extent and composition. The VOL-CALPUFF dispersal code
was applied to reconstruct the transient and 3-D evolution of the cloud. Source parameters estimated on the base of available a posteriori volcanological data sets have been used. Quantitative comparisons between satellite retrievals and modeling results were performed for two selected instants of time during the first and third eruptive phases on a regional scale. Sensitivity of the model to initial volcanological conditions has been analyzed at continental scale. Several complex non intuitive features of cloud dynamics have been highlighted and
strengths and limitations of the adopted methods identified. The main findings are: the level of
quantitative agreement between satellite observations and numerical results depends on ash
cloud composition (particle sizes and concentration) with better agreement for smaller
particles and higher concentrations; the agreement between observations and modeling
outcomes also depends on the temporal stability of volcanological conditions and the
complexity of the meteorological wind field; the irregular dispersion of ash, as reconstructed
from satellite data and numerical modeling, can be well explained by the different response of
particle sizes to strong vertical wind-shear, and by resuspension processes acting at ground level; eruptive source conditions are the main source of uncertainty in modeling, especially during an ongoing crisis and at long-range scales.
Type
article
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10.1002_jgrd.50328_published.pdf
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