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LAVA FLOW MAPPING AND CHANGE DETECTION IN THE MT. ETNA VOLCANO BETWEEN 2009-2012 USING HYPERION HYPERSPECTRAL IMAGERY

机译:熔岩流动映射和MT中的变化检测。 2009 - 2012年间使用Hyperion高光谱图像之间的etna火山

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Mt. Etna is a young composite strato-volcano and one of the most active volcanoes in the world. Eruptions occur almost every year with a persistent degassing activity at the summit craters. In the last 100 years it has produced in average 107m~3 of new lava per year. The main goal of our work is to detect land cover changes, including different lava flows, over the volcano that occurred between 2009 and 2012 using hyperspectral imagery (EO-1 Hyperion). For this purpose, we separated the volcano into three main land cover types: dense vegetation, urban and semi-urban areas and bare lava areas. For each area, a change detection map was produced. For the bare lava areas, two classification maps were produced based on (i) reflectance differences and (ii) chronology as proposed in bibliography. Results have shown changes in all three land cover types. In particular, for the bare lava areas, the most significant lava changes are observed in the northern and central part of the volcano, where several lava flows occurred during the 3-year study period.
机译:Mt. etna是一个年轻的复合转移火山和世界上最活跃的火山之一。爆发几乎每年都发生在山顶陨石坑上的持续脱气活动。在过去的100年里,每年平均每年生产107米〜3。我们工作的主要目标是检测到2009年至2012年在2009年至2012年之间发生的火山中的土地覆盖变化,包括不同的熔岩流量,它使用高光谱图像(EO-1 Hyperion)。为此目的,我们将火山分为三种主要土地覆盖类型:密集植被,城市和半城区和裸露的熔岩地区。对于每个区域,产生改变检测图。对于裸露的熔岩区域,基于(i)反射差异和(ii)按照参考书目提出的第(ii)的年表产生了两个分类地图。结果显示了所有三种覆盖类型的变化。特别是对于裸露的熔岩区域,在火山的北部和中央部分观察到最重要的熔岩变化,其中几个熔岩流动在3年的研究期间发生。

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