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首页> 外文期刊>測地学会誌 >ALOSデータを用いたInSAR解析により捉えられた2010年Eyjafjallajokull火山噴火に伴う地殻変動
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ALOSデータを用いたInSAR解析により捉えられた2010年Eyjafjallajokull火山噴火に伴う地殻変動

机译:使用ALOS数据通过InSAR分析捕获的与2010年Eyjafjallajokull火山喷发相关的地壳运动

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On 20 March 2010, Eyjafjallajokull volcano in Iceland began to erupt after about 190 years of inactivity. A steam explosion on 22 March generated a steam plume that rose to an altitude of 8 km (26,200 ft.) a.s.l., and many residents evacuated. Afterward, the volcano continued to be active with small eruptions. Then, a large eruption on 14 April 2010 propelled volcanic ash to an altitude exceeding 8 km. Volcanic ash from this eruption circulated in the atmosphere, greatly disrupting air transport services in Europe. In this study, we used Interferometric Synthetic Aperture Radar (InSAR) data from the Advanced Land Observing Satellite (ALOS) to analyze the ground deformation associated with the eruptive activity. In addition, we compared pairs of Phased Array type L-Band SAR (PALSAR) amplitude images and Advanced Visible and Near Infrared Radiometer type 2 (AVNIR-2) images acquired before and after the eruption. We obtained a good interference result from several pairs of PALSAR images, and clearly detected an interference fringe due to volcanic activity in paired images acquired before the eruption of,14 April. In composite color images generated from PALSAR amplitude images acquired before and after the volcanic eruption, eruption points could be identified by their intense red color. In addition, we estimated the pressure sources during the eruptive activity using an elevation-modified Mogi model and an Okada model. When a Mogi-type point source was assumed, the estimated volume inflation was 4.5 – 6.5 X 10~7 m~3 about 6 km east of the mountaintop at 4-6 km depth, and when an Okada-type opening source was assumed, a volume inflation of about 4.0 X 10~7 m~3 was estimated 4-5 km east of the mountaintop at 5-6 km depth. The two models thus yielded similar results, although the opening displacement predicted by the Okada model on 1 April was 0.67 m, and it dramatically increased by 13 April to 1.41 m. This result is consistent with the greater size of the eruption of 14 April.
机译:2010年3月20日,经过约190年的不活动之后,冰岛的Eyjafjallajokull火山开始爆发。 3月22日发生的蒸汽爆炸产生的蒸汽羽流升至海拔8公里(26,200英尺)a.s.l.,许多居民被疏散。此后,火山继续活跃,小喷发。然后,2010年4月14日的一次大喷发将火山灰推到了超过8公里的高度。火山喷发产生的火山灰在大气中循环传播,极大地破坏了欧洲的航空运输服务。在这项研究中,我们使用了来自高级陆地观测卫星(ALOS)的干涉合成孔径雷达(InSAR)数据来分析与喷发活动相关的地面变形。此外,我们比较了喷发前后相控阵型L波段SAR(PALSAR)振幅图像和高级可见和近红外辐射计2型(AVNIR-2)图像对。我们从几对PALSAR图像中获得了良好的干涉结果,并在4月14日喷发之前获取的成对图像中清楚地检测到由于火山活动引起的干涉条纹。在由火山喷发前后采集的PALSAR振幅图像生成的合成彩色图像中,喷发点可以通过深红色识别。此外,我们使用高程修正的Mogi模型和Okada模型估算了喷发活动期间的压力源。假设使用Mogi型点源,则在4-6 km深度的山顶以东约6 km处,估计的体积膨胀为4.5 – 6.5 X 10〜7 m〜3,而假设使用Okada型开放源,在5-6 km深度的山顶以东4-5 km处估计约有4.0 X 10〜7 m〜3的体积膨胀。因此,尽管冈田模型在4月1日预测的张开位移为0.67 m,但到4月13日急剧增加至1.41 m,这两个模型得出的结果相似。这一结果与4月14日喷发的更大规模相吻合。

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