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A Total Station Plan Combined with “D/V Chikyu” and DONET:Simultaneous Observation from Seafloor to Atmosphere

机译:结合“ D / V Chikyu”和DONET的全站仪计划:从海底到大气的同时观测

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DONET (Dense Oceanfloor Network system for Earthquakes and Tsunamis) has been developed and installed around Nankai Trough, which is motivated by the 2004 Sumatra-Andaman Earthquake. DONET contains pressure gauges as well as seismometers, which is expected to detect crustal deformations driven by peeling off subduction plate coupling process. From our simulation results, leveling changes are different sense among at the DONET points even in the same science node. On the other hand, oceanic fluctuations such as melting ice masses through the global warming has so large scale as to cause ocean bottom pressure change coherently for all of DONET points especially in the same node. This difference suggests the possibility of extracting crustal deformations component from ocean bottom pressure data by differential of stacking data. However, this operation cannot be applied to local-scale fluctuations related to ocean mesoscale eddies and current fluctuations, which affect ocean bottom pressure through water density changes in the water column (from the sea surface to the bottom). Recently, Kuroshio current path has been changed drastically, which significantly affect ocean bottom pressures at DONET station points. Therefore, we need integral analysis by combining seismology, ocean physics and tsunami engineering so as to decompose into crustal deformation, oceanic fluctuations and instrumental drift, which will bring about high precision data enough to find geophysical phenomena. Since DONET has been and will be connected to long-term borehole observatories constructed in the Nankai Trough under the Integrated Ocean Drilling Program (IODP) by using the deep-sea drilling vessel Chikyu, we have to discuss the best way to do simultaneous observation from seafloor to atmosphere by taking advantage of this chance.
机译:DONET(用于地震和海啸的密集海底网络系统)是在2004年苏门答腊-安达曼大地震的推动下,在南海海槽附近开发并安装的。 DONET包含压力计和地震仪,有望检测由于剥离俯冲板耦合过程而引起的地壳变形。从我们的模拟结果来看,即使在同一科学节点中,在DONET点之间的水平变化也有不同的含义。另一方面,诸如全球融化过程中融化的冰块之类的海洋波动的规模如此之大,以致于所有DONET点(尤其是同一节点)的海底压力连贯地变化。这种差异表明有可能通过叠加数据的差异从海底压力数据中提取地壳变形分量。但是,此操作无法应用于与海洋中尺度涡旋和洋流波动有关的局部尺度波动,这些波动会通过水柱中水密度的变化(从海面到海底)影响海洋底部压力。最近,黑潮的电流路径发生了巨大变化,这极大地影响了DONET站点的海底压力。因此,我们需要将地震学,海洋物理学和海啸工程相结合进行整体分析,以分解为地壳变形,海洋波动和仪器漂移,这将带来足够的高精度数据来寻找地球物理现象。由于DONET已经并且将与深海钻探船Chikyu根据综合海洋钻探计划(IODP)在南海海槽建造的长期井眼观测站相连,因此,我们必须讨论从中进行同步观测的最佳方法利用这次机会将海底空气带入大气层。

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