首页> 外文期刊>Journal of Volcanology and Geothermal Research2012V243-244NOCT,15 >Volcanic plume characteristics determined using an infrared imaging camera
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Volcanic plume characteristics determined using an infrared imaging camera

机译:使用红外热像仪确定的火山羽特征

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摘要

Measurements of volcanic emissions (ash and SO2) from small-sized eruptions at three geographically dispersed volcanoes are presented from a novel, multichannel, uncooled imaging infrared camera. Infrared instruments and cameras have been used previously at volcanoes to study lava bodies and to assess plume dynamics using high temperature sources. Here we use spectrally resolved narrowband (similar to 0.5-1 mu m bandwidth) imagery to retrieve SO2 and ash slant column densities (g m(-2)) and emission rates or fluxes from infrared thermal imagery at close to ambient atmospheric temperatures. The relatively fast sampling (0.1-0.5 Hz) of the multispectral imagery and the fast sampling (similar to 1 Hz) of single channel temperature data permit analysis of some aspects of plume dynamics. Estimations of SO2 and ash mass fluxes, and total slant column densities of SO2 and fine ash in individual small explosions from Stromboli (Italy) and Karymsky (Russia), and total SO2 slant column densities and fluxes from Lascar (Chile) volcanoes, are provided. We evaluate the temporal evolution of fine ash particle sizes in ash-rich explosions at Stromboli and Karymsky and use these observations to infer the presence of at least two distinct fine ash modes, with mean radii of <10 mu m and >10 mu m. The camera and techniques detailed here provide a tool to quickly and remotely estimate fluxes of fine ash and SO2 gas and characterize eruption size. (C) 2015 Elsevier B.V. All rights reserved.
机译:使用新型的多通道非冷却成像红外热像仪,可以测量在三个地理上分散的火山的小型火山喷发产生的火山灰排放量(灰分和二氧化硫)。以前,在火山中使用红外仪器和照相机来研究熔岩体并使用高温源评估羽流动力学。在这里,我们使用光谱分辨的窄带(类似于0.5-1μm带宽)图像来检索SO2和灰倾斜列密度(g m(-2))以及在接近环境大气温度下红外热成像的发射率或通量。多光谱图像的相对快速采样(0.1-0.5 Hz)和单通道温度数据的快速采样(类似于1 Hz)允许对羽流动力学的某些方面进行分析。提供了来自斯特隆博利(意大利)和卡林斯基(俄罗斯)的单个小爆炸中SO2和灰质通量的估算值,以及SO2和细灰的总斜柱密度以及Lascar(智利)火山的SO2斜柱总密度和通量的估算。我们评估了Stromboli和Karymsky富灰爆炸中细灰粒度的时间演变,并利用这些观察结果推断出至少两种不同的细灰模式的存在,平均半径分别为<10μm和> 10μm。此处详细介绍的照相机和技术提供了一种工具,可以快速,远程地估算细灰和SO2气体的通量并确定喷发的大小。 (C)2015 Elsevier B.V.保留所有权利。

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