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Linking volcanic tremor, degassing, and eruption dynamics via SO _2 imaging

机译:通过SO _2成像将火山震颤,除气和喷发动力学联系起来

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摘要

Recently developed UV cameras offer improvement in remote sensing of volcanic SO_2, with temporal resolutions of ~1 Hz and synoptic plume views. Integrated UV camera and seismic measurements recorded in January 2009 at Fuego volcano, Guatemala, provide new insight into the system's shallow conduit processes. High temporal resolution SO_2 data reveal patterns of SO_2 emission rate relative to explosions and seismic tremor that indicate tremor and degassing share a common source process. Progressive decreases in emission rate appear to represent inhibition of gas loss from magma as a result of rheological stiffening in the upper conduit. Measurements of emission rate from two closely-spaced vents, made possible by the high spatial resolution of the camera (1024 × 1024 pixels), help constrain this model. This inter-disciplinary approach illuminates eruptive processes at Fuego and holds promise for gaining similar understanding at other volcanic systems.
机译:最近开发的紫外线照相机可改善火山SO_2的遥感,其时间分辨率约为1 Hz,并具有天气羽状视图。 2009年1月在危地马拉的Fuego火山上记录的集成式紫外线摄像机和地震测量结果为系统的浅层管道过程提供了新的见解。较高的时间分辨率SO_2数据揭示了与爆炸和地震震颤有关的SO_2排放速率模式,表明震颤和脱气共享一个共同的源过程。排放速率的逐渐降低似乎表示由于上导管的流变变硬而抑制了岩浆产生的气体损失。摄像机的高空间分辨率(1024×1024像素)使得测量两个紧密间隔的通风口的发射率成为可能,从而限制了该模型。这种跨学科的方法阐明了Fuego的喷发过程,并有望在其他火山系统上获得类似的理解。

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