利用小波方法处理2004年苏门答腊大地震后的超导重力数据检测低于1.5mHz自由振荡信号的耦合和分裂
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摘要
新型超导重力仪已被证实在频率低于1 mHz的情况下优于最好的地震仪STS-1,因而新型超导重力仪可作为极低噪音的地震仪,观测长周期地球自由振荡.具有良好窄带频率响应的小波滤波器非常有助于消除大气压波动对重力变化的影响.用小波滤波器处理2004年12月26日苏门答腊大地震后的超导重力仪的观测数据,清楚地检测到了1.5 mHz以下,除0T5,0T7,1T1外所有的环形自由振荡的耦合现象,并检测到了环形自由振荡1T2,1T3的耦合现象.此外,还利用单台超导重力仪的观测数据清楚地检测到了球形自由振荡2S1的3个分裂谱峰.
引文
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