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Detailed Mapping of Pyroclastic Flows and Lahars for an Active Volcano Using RADARSAT SAR and ASTER Image Data

机译:使用RADARSAT SAR和ASTER图像数据的活火山的火山碎屑流和Lahars的详细映射

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Merapi eruption is characterized by the persistent growth of a summit dome and partial or total collapse of the dome to generate hot pyroclastic flows. In this paper, we aim at detecting the latest pyroclastic flows deposit and assessing its possibility to generate lahars during and after rainy season. We used RADARSAT SAR scenes and ASTER images acquired on the dates soon after the eruption. The analysis of two type image data proved the high capability of detecting the small-scale volcanic flows in spite of the bad atmospheric condition. The RADARSAT SAR scattering intensity changes through beta nought calculation for SIX product before and after the eruption, and the n classifications using NDVI threshold methods were applied to delineate the pyroclastic flows and lahars distribution. Moving image calculation was also adopted to simulate vector of lahars flow direction. The results deduced that the coverage of lahars deposit changed from parental pyroclastic deposits was about 5.5 km2. The lahars commonly flowed towards the SE-SW direction and elongated more than 10 km. The lahars flow from the nearest height topography to the lower part with gathering and filling the river banks. This study can be effective for environment and hazard assessments associated with pyroclastic flows and lahars after the eruption.
机译:默拉皮火山喷发的特征是山顶穹顶的持续增长和穹顶的部分或全部塌陷,从而产生热的火山碎屑流。在本文中,我们旨在检测最新的火山碎屑流沉积物,并评估其在雨季期间和雨季之后产生拉哈斯的可能性。我们使用了在喷发后不久获取的RADARSAT SAR场景和ASTER图像。两种图像数据的分析证明,即使在恶劣的大气条件下,仍具有较高的探测小规模火山流的能力。通过在喷发之前和之后通过β零值计算得出SARD SAR SAR散射强度的变化,并使用NDVI阈值方法对n种分类进行了描述,描述了火山碎屑流和拉哈斯分布。还采用运动图像计算来模拟拉哈斯流向的矢量。结果推论,拉哈斯沉积物的覆盖范围由父母的火山碎屑沉积物改变为约5.5 km2。泻湖通常流向SE-SW方向,并拉长了10多公里。 har流从最接近的高度地形流向下部,聚集并填满河岸。这项研究对于喷发后火山碎屑流和火山爆发的环境和危害评估可能是有效的。

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