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Volcanic dust characterization by EARLINET during Etna's eruptions in 2001-2002

机译:EARLINET在2001-2002年埃特纳火山爆发期间对火山灰的特征

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Lidar measurements were performed in the framework of the EARLINET project during the last eruptions (July-August 2001 and November 2002) of the Etna volcano. Both aerosol backscattering and extinction coefficients show the presence of remarkable aerosol layers in central and especially in southern Europe during the Etna eruptions periods. The aerosol layer altitudes ranged from 1 to 6 km. Back-trajectory, lidar ratio and backscatter related Angstrom coefficient analyses show that most of the aerosol layers originated from the Etna eruption and were made of sulfates and small absorbing volcanic ash. Thanks to the EARLINET network, the space and temporal distributions of volcanic aerosol have been studied over continental scale.
机译:在Etna火山的最后一次喷发(2001年7月至8月和2002年11月)期间,在EARLINET项目的框架内进行了激光雷达测量。气溶胶的反向散射系数和消光系数都表明,在埃特纳火山爆发期间,中欧,特别是南欧存在着明显的气溶胶层。气溶胶层高度范围为1至6 km。反向轨迹,激光雷达比率和反向散射相关的埃斯特伦系数分析表明,大多数气溶胶层起源于埃特纳火山喷发,由硫酸盐和少量吸收性火山灰组成。得益于EARLINET网络,已经在大陆范围内研究了火山气溶胶的时空分布。

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