库页岛Poronaisk附近海域地震激发特征

D. Kovalev, P. Kovalev, A. Borisov, V. S. Zarochintsev, K. Kirillov
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引用次数: 2

摘要

本文介绍了2008-2009年在库页岛Poronaisk附近海域利用自然测量资料研究地震激发能潜在来源的结果。两个自动海平面记录仪以1秒采样率收集了持续时间约为3个月的时间序列数据。时间序列的频谱分析可以得出这样的结论:周期为2至7小时的波过程可以归类为波场。用数值方法计算出的可能的淤塞周期与在特尔佩尼亚湾探测到的淤塞周期非常接近。计算的波浪过程包络线显示,周期为7 h的巨浪峰值与风浪有很好的重合,证实了大气扰动向7 h巨浪的能量转移。潮汐周期为3.5小时,与潮汐谐波周期4M - hz相等。因此,考虑到3.5 h时海水q因子为11.9的高值,揭示了能量从潮谐向潮涌传递的共振通道。日潮最大值后6-8天(24.68小时)出现2.7小时的最高潮期,接近月潮调和周期M1。对周期为2 h的地震激发因子的分析表明,地震激发能至少有一部分是由大气扰动提供的。因此,洪水高度的增加发生在特尔佩尼亚湾的南风期间。
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Features of seiсhe excitation in the water area near Poronaisk (Sakhalin Island)
The results of studying potential sources of seiche excitation energy in the water area near Poronaisk (Sakhalin Island) using natural measurement data in 2008–2009 are presented. Time series data with a duration of about three months were collected by two autonomous sea-level recorders at one-second sample rate. Spectral analyses of time series made possible to conclude that wave processes with periods from 2 to 7 hours can be classified as seiches. Possible seiche periods calculated by numerical methods are very close to the periods of seiches detected in the Terpeniya Bay. The calculated envelopes of wave processes showed a good coincidence of the peaks of seiches with a period of 7 hours and wind waves, which confirms the transfer of energy from atmospheric disturbances to the seven-hour seiche. Seiche period of 3.5 hours is shown to be equal to the period of tidal harmonic 4M7. Thus, the resonance pass of energy transmission from tidal harmonic to seiche was revealed taking into account high for marine waters q-factor equal to 11.9 at the period of 3.5 hours. The highest seiches at a period of 2.7 hours are observed on the 6-8 day after maximum of daily tide with a period of 24.68 hours, which is close to the period of lunar tide harmonic M1. The analyses of excitation factors of seiches with 2-hour period showed that the excitation energy, or at least a part of it, is provided by atmospheric disturbances. Thus, the increasing of seiche height occurs during the winds of southern directions in the Terpeniya Bay.
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