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首页> 外文期刊>TAO: Terrastrial, atmospheric, and oceanic sciences >Baekdusan Volcano Time-Series Analysis from 1992 to 1998 Using Multi-Interferogram InSAR Processing
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Baekdusan Volcano Time-Series Analysis from 1992 to 1998 Using Multi-Interferogram InSAR Processing

机译:使用多干涉图InSAR处理的Baekdusan火山1992年至1998年的时间序列分析

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A multi-temporal SAR interferometry (InSAR) method was applied to a time-series analysis of the period from 1992 - 1998 to detect precursor volcanic activity at Baekdusan volcano, located on the border between China and North Korea. Permanent scatterers were selected for stable signal processing to monitor ground motion using the permanent scatterer InSAR (PSInSAR) technique, which generated a time-series surface deformation map using the refined small baseline subset (SBAS) InSAR method. The time-series analysis results were verified using a multi-track comparison technique for two different tracks (88/230 and 89/230). The time-series analysis of the two tracks represents an unaltered phase signal (mm scale) with time, except for periods with insufficient interferograms to make a precise time-series surface deformation map due to factors including atmospheric phase delay and other error effects (i.e., those that display a maximum value of the phase difference from -2.14 to +2.64 cm). These phase signals also have the Root Mean Square Error (RMSE) range from 0.32 - 2.56 cm. No surface deformation was detected from the Japanese Earth Resources Satellites (JERS-1) synthetic aperture radar (SAR) data collected between 1992 - 1998 at the Baekdusan volcano, as monitored using volcanic surface movements with dynamic magma activity. No volcanic eruption precursor signals were demonstrated during the inactive period (1992 - 1998) prior to the active period (2002 - 2006) of this volcano.
机译:将多时相SAR干涉法(InSAR)方法用于1992年至1998年的时间序列分析,以检测位于中朝边界的白头山火山的前驱火山活动。选择永久散射体进行稳定的信号处理,以使用永久散射体InSAR(PSInSAR)技术监视地面运动,该技术使用改进的小基线子集(SBAS)InSAR方法生成时间序列表面变形图。使用多轨比较技术对两个不同的轨道(88/230和89/230)验证了时间序列分析结果。两条轨迹的时间序列分析表示随时间变化的相位信号(毫米标度),但由于大气相位延迟和其他误差影响(例如,由于干涉图不足而无法形成精确的时间序列表面变形图的周期除外) ,即那些显示从-2.14到+2.64 cm的相位差最大值的传感器。这些相位信号的均方根误差(RMSE)范围为0.32-2.56 cm。 1992年至1998年在白头山火山收集的日本地球资源卫星(JERS-1)合成孔径雷达(SAR)数据中未检测到表面变形,该数据是使用具有动态岩浆活动的火山表面运动进行监测的。在该火山的活跃期(2002年至2006年)之前的非活跃期(1992年至1998年)没有显示出火山喷发前兆信号。

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