Shake to the Beat: Exploring the Seismic Signals and Stadium Response of Concerts and Music Fans

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Seismological Research Letters Pub Date : 2024-03-13 DOI:10.1785/0220230385
G. Tepp, I. Stubailo, Monica Kohler, Richard Guy, Yousef Bozorgnia
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Abstract

Large music festivals and stadium concerts are known to produce unique vibration signals that resemble harmonic tremor, particularly at frequencies around 1–10 Hz. This study investigates the seismic signals of a Taylor Swift concert performed on 5 August 2023 (UTC) as part of a series at SoFi Stadium in Inglewood, California, with an audience of ∼70,000. Signals were recorded on regional seismic network stations located within ∼9 km of the stadium, as well as on strong-motion sensors placed near and inside the stadium prior to the concert series. We automatically identified the seismic signals from spectrograms using a Hough transform approach and characterized their start times, durations, frequency content, particle motions, radiated energy, and equivalent magnitudes. These characteristics allowed us to associate the signals with individual songs and explore the nature of the seismic source. The signal frequencies matched the song beat rates well, whereas the signal and song durations were less similar. Radiated energy was determined to be a more physically relevant measure of strength than magnitude, given the tremor-like nature of the signals. The structural response of the stadium showed nearly equal shaking intensities in the vertical and horizontal directions at frequencies that match the seismic signals recorded outside the stadium. In addition, we conducted a brief experiment to further evaluate whether the harmonic tremor signals could be generated by the speaker system and instruments, audience motions, or something else. All evidence considered, we interpret the signal source as primarily crowd motion in response to the music. The particle motions of the strongest harmonics are consistent with Rayleigh waves influenced by scattered body waves and likely reflect how the crowd is moving. Results from three other musical performances at SoFi in summer 2023 were similar, although differences in the signals may relate to the musical genre and variations in audience motions.
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跟着节拍摇摆探索音乐会和乐迷的地震信号和体育场反应
众所周知,大型音乐节和体育场音乐会会产生类似谐震的独特振动信号,尤其是在 1-10 赫兹左右的频率。本研究调查了泰勒-斯威夫特于 2023 年 8 月 5 日(协调世界时)在加利福尼亚州英格尔伍德 SoFi 体育场举行的系列演唱会的地震信号,该演唱会的观众人数为 7 万人。信号由位于体育场 9 千米范围内的区域地震网络台站记录,以及在系列音乐会之前放置在体育场附近和内部的强运动传感器记录。我们使用 Hough 变换方法从频谱图中自动识别地震信号,并对其起始时间、持续时间、频率含量、质点运动、辐射能量和等效震级进行特征描述。这些特征使我们能够将信号与单个歌曲联系起来,并探索震源的性质。信号频率与歌声节拍非常吻合,而信号和歌声持续时间则不太相似。鉴于信号的震颤性质,辐射能量被认为是比震级更贴近物理的强度衡量标准。体育场的结构响应显示,在垂直和水平方向上的震动强度几乎相等,其频率与体育场外记录到的地震信号相吻合。此外,我们还做了一个简短的实验,以进一步评估谐波震颤信号是否可能由扬声器系统和乐器、观众动作或其他因素产生。考虑到所有证据,我们认为信号源主要是观众对音乐的反应。最强谐波的粒子运动与受散射体波影响的瑞利波一致,很可能反映了人群的运动方式。2023 年夏季在 SoFi 进行的另外三场音乐表演的结果与此类似,但信号的差异可能与音乐类型和观众运动的变化有关。
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来源期刊
Seismological Research Letters
Seismological Research Letters 地学-地球化学与地球物理
CiteScore
6.60
自引率
12.10%
发文量
239
审稿时长
3 months
期刊介绍: Information not localized
期刊最新文献
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