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首页> 外文期刊>Atmospheric Measurement Techniques Discussions >Improved optical flow velocity analysis in SOsub2/sub camera images of volcanic plumes – implications for emission-rate retrievals investigated at Mt Etna, Italy and Guallatiri, Chile
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Improved optical flow velocity analysis in SOsub2/sub camera images of volcanic plumes – implications for emission-rate retrievals investigated at Mt Etna, Italy and Guallatiri, Chile

机译:改进的SO 2 火山羽相机图像中的光流速度分析–对意大利埃特纳火山和智利瓜拉提里研究的排放速率取回的意义

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摘要

Accurate gas velocity measurements in emission plumes are highly desirable for various atmospheric remote sensing applications. The imaging technique of UV SOsub2/sub cameras is commonly used to monitor SOsub2/sub emissions from volcanoes and anthropogenic sources (e.g. power plants, ships). The camera systems capture the emission plumes at high spatial and temporal resolution. This allows the gas velocities in the plume to be retrieved directly from the images. The latter can be measured at a pixel level using optical flow (OF) algorithms. This is particularly advantageous under turbulent plume conditions. However, OF algorithms intrinsically rely on contrast in the images and often fail to detect motion in low-contrast image areas. We present a new method to identify ill-constrained OF motion vectors and replace them using the local average velocity vector. The latter is derived based on histograms of the retrieved OF motion fields. The new method is applied to two example data sets recorded at Mt Etna (Italy) and Guallatiri (Chile). We show that in many cases, the uncorrected OF yields significantly underestimated SOsub2/sub?emission rates. We further show that our proposed correction can account for this and that it significantly improves the reliability of optical-flow-based gas velocity retrievals. In the case of Mt Etna, the SOsub2/sub emissions of the north-eastern crater are investigated. The corrected SOsub2/sub?emission rates range between 4.8 and 10.7 kg?ssup?1/sup (average of 7.1 ± 1.3?kg?ssup?1/sup) and are in good agreement with previously reported values. For the Guallatiri data, the emissions of the central crater and a fumarolic field are investigated. The retrieved SOsub2/sub?emission rates are between 0.5 and 2.9 kg?ssup?1/sup (average of 1.3 ± 0.5?kg?ssup?1/sup) and provide the first report of SOsub2/sub emissions from this remotely located and inaccessible volcano.
机译:对于各种大气遥感应用,非常需要在排放羽流中进行准确的气体速度测量。 UV SO 2 相机的成像技术通常用于监视火山和人为来源(例如发电厂,轮船)的SO 2 排放。摄像机系统以高空间和时间分辨率捕获排放羽流。这允许直接从图像中检索羽流中的气体速度。后者可以使用光流(OF)算法在像素级别进行测量。这在湍流羽流条件下特别有利。但是,OF算法本质上依赖于图像中的对比度,并且通常无法检测到低对比度图像区域中的运动。我们提出了一种新的方法来识别约束不正确的OF运动矢量,并使用局部平均速度矢量替换它们。后者是基于检索到的OF运动场的直方图得出的。将该新方法应用于在埃特纳火山(意大利)和瓜拉蒂里(智利)记录的两个示例数据集。我们表明,在许多情况下,未经校正的OF产量会大大低估SO 2 的排放率。我们进一步表明,我们提出的校正可以解决这个问题,并且可以显着提高基于光流的气体速度检索的可靠性。以埃特纳火山为例,研究了东北火山口的SO 2 排放。校正后的SO 2 ?排放速率介于4.8和10.7 kg?s ?1 之间(平均值为7.1±1.3?kg?s ?1 ),并且与先前报告的值高度吻合。对于Guallatiri数据,研究了中央火山口和富马场的排放。回收的SO 2 ?排放速率介于0.5和2.9 kg?s ?1 之间(平均值为1.3±0.5?kg?s ?1 ),并提供此偏远且难以接近的火山SO 2 排放的第一份报告。

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