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Detection and characterization of volcanic ash plumes over Lille during the Eyjafjallaj?kull eruption

机译:Eyjafjallaj?kull喷发期间里尔上空的火山灰羽流的检测和表征

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Routine sun-photometer and micro-lidar measurements were performed in Lille,northern France, in April and May 2010 during the Eyjafjallaj?kullvolcanic eruption. The impact of such an eruption emphasized significance ofhazards for human activities and importance of observations of the volcanicaerosol particles. This paper presents the main results of a jointmicro-lidar/sun-photometer analysis performed in Lille, where volcanic ashplumes were observed during at least 22 days, whenever weather conditionspermitted. Aerosol properties retrieved from automatic sun-photometermeasurements (AERONET) were strongly changed during the volcanic aerosolplumes transport over Lille. In most cases, the aerosol optical depth (AOD)increased, whereas ?ngstr?m exponent decreased, thus indicatingcoarse-mode dominance in the volume size distribution. Moreover, the non-sphericalfraction retrieved by AERONET significantly increased. The real part of thecomplex refractive index was up to 1.55 at 440 nm during the eruption,compared to background data of about 1.46 before the eruption. Collocatedlidar data revealed that several aerosol layers were present between 2 and5 km, all originating from the Iceland region as confirmed bybackward trajectories. The volcanic ash AOD was derived from lidarextinction profiles and sun-photometer AOD, and its maximum was estimatedaround 0.37 at 532 nm on 18 April 2010. This value was observed at analtitude of 1700 m and corresponds to an ash mass concentration (AMC)slightly higher than 1000 μg m?3 (±50%). An effective lidarratio of ash particles of 48 sr was retrieved at 532 nm for 17 April duringthe early stages of the eruption, a value which agrees with several otherstudies carried out on this topic. Even though the accuracy of theretrievals is not as high as that obtained from reference multiwavelengthlidar systems, this study demonstrates the opportunity of micro-lidar andsun-photometer joint data processing for deriving volcanic AMC. It alsooutlines the fact that a network of combined micro-lidars andsun photometers can be a powerful tool for routine monitoring of aerosols,especially in the case of such hazardous volcanic events.
机译:在法国北部的里尔,于2010年4月至5月进行的常规Eyjafjallaj?kull火山喷发中,进行了常规日光光度计和微激光雷达测量。这种喷发的影响强调了对人类活动的危害的重要性以及对火山气溶胶颗粒观测的重要性。本文介绍了在里尔进行的微激光/太阳光度计联合分析的主要结果,只要天气条件允许,在至少22天之内观察到火山灰烬。在里尔的火山气溶胶运输过程中,从自动太阳光度计测量(AERONET)检索到的气溶胶特性发生了很大变化。在大多数情况下,气溶胶光学深度(AOD)会增加,而弹力指数会减小,因此表明体积尺寸分布中的粗模式占优势。而且,AERONET检索到的非球形分数显着增加。喷发期间,复折射率的实部在440 nm处高达1.55,而喷发前的背景数据约为1.46。并列的激光雷达数据显示,在2至5公里之间存在数个气溶胶层,所有气溶胶层均来自冰岛地区,并通过向后的轨迹证实。火山灰的AOD来源于激光消光剖面和太阳光度计的AOD,2010年4月18日在532 nm处的最大值估计为0.37左右。该值在1700 m的海拔高度处观察到,与灰分质量浓度(AMC)略高大于1000μgm ?3 (±50%)。在喷发的早期阶段,于4月17日在532 nm处回收了48 sr灰烬颗粒的有效激光雷达比,该值与对该主题进行的其他研究一致。即使逆流技术的精度不如参考多波长激光雷达系统获得的精度高,但这项研究证明了微激光雷达和太阳光度计联合数据处理方法有可能推导火山AMC。它还概述了一个事实,那就是微激光和太阳光度计相结合的网络可以成为常规监测气溶胶的有力工具,尤其是在此类危险的火山事件中。

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