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Infrasonic ambient noise interferometry from correlationsof microbaroms

机译:次微环境相关的次声环境噪声干涉法

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We show that microbaroms, continuous infrasoundfluctuations resulting from the interaction of the ocean withthe atmosphere, have long-range correlation properties thatmake it possible to estimate the impulse response betweentwo microphones from passive recordings. The processingis analogous to methods employed in the emerging field ofambient noise seismology, where the random noise source isthe ocean coupling with the solid Earth (microseisms)instead of the atmosphere (microbaroms). We find that time-dependent temperature fields and temperature inversionsdetermine the character of infrasonic impulse responses atFourpeaked Volcano in Alaska. Applications includeimaging and monitoring the gross structure of the Earth'satmospheric boundary layer. Citation: Haney, M. M. (2009),Infrasonic ambient noise interferometry from correlations ofmicrobaroms.
机译:我们表明,由于海洋与大气相互作用而产生的连续不断的次声涨落所产生的微气压,具有远距离的相关特性,这使得可以从被动录音中估计两个麦克风之间的脉冲响应。该处理类似于在环境噪声地震学的新兴领域中使用的方法,在该领域中,随机噪声源是与固体地球耦合的海洋(微地震),而不是大气(微气压)。我们发现随时间变化的温度场和温度反演确定了阿拉斯加四峰火山次声脉冲响应的特征。应用包括对地球大气边界层的总体结构进行成像和监测。引文:Haney,M. M.(2009),《基于微压力相关的次声环境噪声干涉法》。

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