首页> 外文期刊>Journal of Glaciology >Seismic signals from large, tabular icebergs drifting along the Dronning Maud Land coast, Antarctica, and their significance for iceberg monitoring
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Seismic signals from large, tabular icebergs drifting along the Dronning Maud Land coast, Antarctica, and their significance for iceberg monitoring

机译:沿南极德龙宁莫德海岸漂流的大型板状冰山的地震信号及其对冰山监测的意义

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In this study, we analyze a large dataset of seismic signals, recorded by station TROLL in Dronning Maud Land, Antarctica. The signals, recorded in April-December 2012, came from sources near the edge of the ice shelves, at distances of 230-500 km from TROLL. The sources, which moved westward with time, could be associated with four large, tabular icebergs, drifting between 15 degrees E and 8 degrees W. Combining the seismological data with information from satellite remote sensing, we find that one-third of the signals can be attributed to individual icebergs. The trajectories of three of the associated icebergs are known through iceberg-tracking databases, whereas the fourth, a fragment of one of the other three, is untracked, and only scarce information is available from satellite imagery. The observed seismic signals exhibit a wide variety of frequency characteristics, from unstructured episodes to occurrences of iceberg harmonic tremor. Although we are not able to determine the exact cause of the signals, we classify them into five classes on a phenomenological basis. This study demonstrates the potential of regional seismic networks for iceberg monitoring as supplementary resources to information obtained with remote-sensing technologies.
机译:在这项研究中,我们分析了南极Dronning Maud Land TROLL台站记录的大量地震信号。 2012年4月至12月记录的信号来自冰架边缘附近的信号源,距TROLL 230-500公里。这些随时间向西移动的震源可能与四个大型的板状冰山有关,它们在东15度到西8度之间漂移。结合地震数据和来自卫星遥感的信息,我们发现三分之一的信号可以归因于个别的冰山。可通过冰山跟踪数据库了解三个相关冰山的轨迹,而未跟踪第四冰山(其他三个冰山之一)的片段,并且卫星图像中仅提供了很少的信息。从非结构性事件到冰山谐波震颤的发生,观测到的地震信号具有多种频率特性。尽管我们无法确定信号的确切原因,但我们根据现象学将其分为五类。这项研究证明了冰山监测的区域地震网络作为遥感技术获得的信息的补充资源的潜力。

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