首页> 外文期刊>Journal of Volcanology and Geothermal Research >Infrasonic observations of the June 2009 Sarychev Peak eruption, Kuril Islands: Implications for infrasonic monitoring of remote explosive volcanism
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Infrasonic observations of the June 2009 Sarychev Peak eruption, Kuril Islands: Implications for infrasonic monitoring of remote explosive volcanism

机译:2009年6月千岛群岛Sarychev峰爆发的次声观测:对远距离爆炸性火山的次声监测的意义

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Sarychev Peak (SP), located on Ostrov Matua, Kurils, erupted explosively during 11-16 June 2009. Whereas remote seismic stations did not record the eruption, we report atmospheric infrasound (acoustic wave -0.01-20 Hz) observations of the eruption at seven infrasound arrays located at ranges of -640-6400 km from SP. The infrasound arrays consist of stations of the International Monitoring System global infrasound network and additional stations operated by the Korea Institute of Geoscience and Mineral Resources. Signals at the three closest recording stations IS44 (643 km, Petropavlovsk-Kamchatskiy, Kamchatka Krai, Russia), IS45 (1690 km, Ussuriysk, Russia), and IS30 (1774 km, Isumi, Japan) represent a detailed record of the explosion chronology that correlates well with an eruption chronology based on satellite data (TERRA, NOAA, MTSAT). The eruption chronology inferred from infrasound data has a higher temporal resolution than that obtained with satellite data. Atmosphere-corrected infrasonic source locations determined from backazimuth cross-bearings of first-arrivals have a mean centroid -15 km from the true location of SP. Scatter in source locations of up to ~100 km result from currently unresolved details of atmospheric propagation and source complexity. We observe systematic time-variations in trace-velocity, backazimuth deviation, and signal frequency content at IS44. Preliminary investigation of atmospheric propagation from SP to IS44 indicates that these variations can be attributed to solar tide variability in the thermosphere. It is well known that additional information about active volcanic processes can be learned by deploying infrasonic sensors with seismometers at erupting volcanoes. This study further highlights the significant potential of infrasound arrays for monitoring volcanic regions such as the Kurils that have only sparse seismic network coverage.
机译:2009年6月11日至16日,位于千岛的Ostrov Matua的Sarychev Peak(SP)爆炸性爆发。虽然偏远的地震台没有记录到这次喷发,但我们报告了在2050年的次声的大气次声观测(声波-0.01-20 Hz)。在距SP -640-6400 km范围内的七个次声阵列。次声阵列由国际监测系统全球次声网络台站和韩国地质科学与矿产资源研究所运营的其他台站组成。三个最近的记录站IS44(俄罗斯,堪察加边疆区的Petropavlovsk-Kamchatskiy,643 km),IS45(俄罗斯,乌苏里斯克,1690 km)和IS30(1774 km,Isumi,日本)的信号代表了爆炸年代的详细记录。与基于卫星数据(TERRA,NOAA,MTSAT)的喷发年表有很好的关联。从次声数据推断出的喷发年表比从卫星数据获得的喷发年表具有更高的时间分辨率。根据首次到达的反方位角交叉方位确定的经大气校正的次声源位置与SP的真实位置之间的平均质心为-15 km。由于目前尚未解决的大气传播和源复杂性的细节,导致在约100 km的源位置散布。我们在IS44处观察到迹线速度,后方位角偏差和信号频率内容的系统时变。对从SP到IS44的大气传播的初步研究表明,这些变化可以归因于热层中太阳潮的变化。众所周知,可以通过在喷发的火山处部署带有地震仪的次声传感器来了解有关活动火山过程的其他信息。这项研究进一步强调了次声阵列在监测火山地区(如千岛)(仅具有稀疏地震网络覆盖范围)方面的巨大潜力。

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