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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:与2010年Eyjafjallajokull火山爆发的地壳运动使用ALOS数据捕获

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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,冰岛的Eyjafjallajokull火山在大约190年不活动后开始爆发。 3月22日的蒸汽爆炸产生了一个蒸汽羽流,升至8km(26,200英尺)A.S.L.和许多居民撤离。之后,火山继续积极爆发。然后,2010年4月14日推进火山灰的大型爆发到高度超过8公里的海拔高度。来自这种爆发的火山灰在大气中循环,大大扰乱了欧洲的空运服务。在这项研究中,我们使用了来自先进土地观察卫星(ALOS)的干涉性合成孔径雷达(INSAR)数据来分析与喷发活动相关的地面变形。此外,我们比较了在爆发之前和之后获得的分阶段阵列型L波段SAR(PALSAR)幅度图像和先进的可见和近红外辐射计类型2(AVNIR-2)图像。我们获得了几对波纹图像的良好干扰结果,并且由于在4月14日爆发之前获得的配对图像中的火山活性而明确地检测干涉条纹。在从火山爆发之前和之后获得的波瓦拉幅度图像产生的复合彩色图像中,可以通过它们的强烈红颜色来识别喷发点。此外,我们估计了使用高度修改的Mogi模型和冈田模型的喷发活动期间的压力来源。当假设Mogi型点源时,估计的体积通胀为4.5 - 6.5 x 10〜7 m〜3在山顶以外的4-6公里深度,当假设Okada型开源时,山顶以5-6公里深度估计约4.0×10〜7 m〜3的体积膨胀约4.0×10〜7 m〜3。因此,这两种模型产生了类似的结果,尽管冈田模型在4月1日预测的开口位移为0.67米,但它急剧增加到4月13日至1.41米。该结果与4月14日爆发的大小相一致。

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