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A multi-sensor approach for volcanic ash cloud retrieval and eruption characterization: The 23 November 2013 Etna lava fountain

机译:火山灰云提取和喷发特征的多传感器方法:2013年11月23日Etna熔岩喷泉

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摘要

Volcanic activity is observed worldwide with a variety of ground and space-based\udremote sensing instruments, each with advantages and drawbacks. No single system can give\uda comprehensive description of eruptive activity, and so, a multi-sensor approach is required. This\udwork integrates infrared and microwave volcanic ash retrievals obtained from the geostationary\udMeteosat Second Generation (MSG)-Spinning Enhanced Visible and Infrared Imager (SEVIRI),\udthe polar-orbiting Aqua-MODIS and ground-based weather radar. The expected outcomes are\udimprovements in satellite volcanic ash cloud retrieval (altitude, mass, aerosol optical depth and\udeffective radius), the generation of new satellite products (ash concentration and particle number\uddensity in the thermal infrared) and better characterization of volcanic eruptions (plume altitude,\udtotal ash mass erupted and particle number density from thermal infrared to microwave). This\udapproach is the core of the multi-platform volcanic ash cloud estimation procedure being developed\udwithin the European FP7-APhoRISM project. The Mt. Etna (Sicily, Italy) volcano lava fountaining\udevent of 23 November 2013 was considered as a test case. The results of the integration show the\udpresence of two volcanic cloud layers at different altitudes. The improvement of the volcanic ash\udcloud altitude leads to a mean difference between the SEVIRI ash mass estimations, before and after\udthe integration, of about the 30%. Moreover, the percentage of the airborne “fine” ash retrieved from\udthe satellite is estimated to be about 1%–2% of the total ash emitted during the eruption. Finally,\udall of the estimated parameters (volcanic ash cloud altitude, thickness and total mass) were also\udvalidated with ground-based visible camera measurements, HYSPLIT forward trajectories, Infrared\udAtmospheric Sounding Interferometer (IASI) satellite data and tephra deposits.
机译:全世界都有各种各样的地面和空基\远程遥感仪器观测到火山活动,每种仪器各有利弊。没有单个系统可以全面描述喷发活动,因此,需要使用多传感器方法。这项工作整合了从对地静止\ udMeteosat第二代(MSG)-旋转增强型可见光和红外成像仪(SEVIRI),\极地轨道Aqua-MODIS和地面气象雷达获得的红外和微波火山灰回收。预期的结果是:\\改进了卫星火山灰云的检索(高度,质量,气溶胶光学深度和\有效半径),新卫星产品的产生(灰分浓度和粒子数\热红外中的密度)以及火山的更好表征爆发(尘埃高度,爆发的灰分总量和从热红外到微波的颗粒数密度)。这种\ udappach方法是欧洲FP7-APhoRISM项目中正在开发\ ud的多平台火山灰云估算程序的核心。山。 2013年11月23日的埃特纳火山(意大利西西里岛)火山熔岩喷泉\ udevent被视为测试案例。整合的结果表明在不同高度存在两个火山云层。火山灰\乌云高度的改善导致SEVIRI灰质质量估计在整合前后的平均差约为30%。此外,估计从卫星中回收的机载“细”灰烬的百分比约为喷发过程中排放的总灰烬的1%–2%。最后,所有估计的参数(火山灰云的高度,厚度和总质量)也都通过地面可见相机测量,HYSPLIT前向轨迹,红外/大气探测干涉仪(IASI)卫星数据和特菲拉沉积物进行了验证。

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