Kadri Usama, Crivelli Davide, Parsons Wade, Colbourne Bruce, Ryan Amanda
Cardiff University, School of Mathematics, Cardiff, CF24 4AG, UK.
Massachusetts Institute of Technology, Department of Mathematics, Cambridge, 02139, MA, USA.
Sci Rep. 2017 Oct 24;7(1):13949. doi: 10.1038/s41598-017-14177-3.
Analysis of data, recorded on March 8th 2014 at the Comprehensive Nuclear-Test-Ban Treaty Organisation's hydroacoustic stations off Cape Leeuwin Western Australia, and at Diego Garcia, reveal unique pressure signatures that could be associated with objects impacting at the sea surface, such as falling meteorites, or the missing Malaysian Aeroplane MH370. To examine the recorded signatures, we carried out experiments with spheres impacting at the surface of a water tank, where we observed almost identical pressure signature structures. While the pressure structure is unique to impacting objects, the evolution of the radiated acoustic waves carries information on the source. Employing acoustic-gravity wave theory we present an analytical inverse method to retrieve the impact time and location. The solution was validated using field observations of recent earthquakes, where we were able to calculate the eruption time and location to a satisfactory degree of accuracy. Moreover, numerical validations confirm an error below 0.02% for events at relatively large distances of over 1000 km. The method can be developed to calculate other essential properties such as impact duration and geometry. Besides impacting objects and earthquakes, the method could help in identifying the location of underwater explosions and landslides.
对2014年3月8日在位于西澳大利亚州卢因角附近的全面禁止核试验条约组织水声监测站以及迪戈加西亚记录的数据进行分析后发现,存在一些独特的压力特征,这些特征可能与物体撞击海面有关,比如坠落的陨石,或者失踪的马来西亚航空公司MH370航班。为了研究记录下来的这些特征,我们用水箱中的球体撞击水面进行了实验,在实验中我们观察到了几乎相同的压力特征结构。虽然压力结构对于撞击物体来说是独特的,但辐射声波的演变携带着有关声源的信息。我们运用声重力波理论提出了一种解析反演方法来获取撞击时间和位置。利用近期地震的现场观测对该解决方案进行了验证,我们能够将地震爆发时间和位置计算到令人满意的精确程度。此外,数值验证证实,对于距离超过1000千米的相对远距离事件,误差低于0.02%。该方法可以进一步拓展以计算其他重要特性,比如撞击持续时间和几何形状。除了撞击物体和地震之外,该方法还能帮助确定水下爆炸和山体滑坡的位置。