dorsal/arxiv
View SchemaAn Automatic Method for Determination of Lg Arrival Times Using Wavelet Transforms
| Authors | Ileana M. Tibuleac, E. T. Herrin |
|---|---|
| Categories | |
| ArXiv ID | physics/9806041 |
| URL | https://arxiv.org/abs/physics/9806041 |
Abstract
The regional phase Lg is used to estimate location and magnitude for sources closer than 1500 km. The complexity of Lg waveforms makes it difficult to consistently determine Lg arrival time, thus affecting source location with a single station or array. This study tests an automatic method for timing Lg arrivals using wavelet transforms to decompose the Lg signal into its components localized both in time and scale. A Continuous Wavelet Transform (CWT) using a Daubechies order two (db2) wavelet is applied to 10 seconds of raw data, containing the start of Lg. Initial positioning of the window is obtained using the standard Lg travel time tables. The coefficients at scale 8 from the db2 decomposition are squared and the resulting time series is represented by an approximation of the 4'th level Discrete Wavelet Transform (DWT) using a Haar wavelet. A threshold detector is then applied to the resulting time series to determine the Lg arrival time. The method was tested using well located earthquakes (USGS) and explosions from known mines (mb less than 4.0), recorded on the vertical components at TXAR (Lajitas, Texas) and PDAR (Pinedale, Wyoming) arrays. The Lg arrival time was automatically picked with a standard deviation of less than 1.5 seconds (less than 10 km location error) for well known locations. Location errors are larger with the increase in distance and smaller with the increase in signal to noise ratio of events.
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"abstract": "The regional phase Lg is used to estimate location and magnitude for sources\ncloser than 1500 km. The complexity of Lg waveforms makes it difficult to\nconsistently determine Lg arrival time, thus affecting source location with a\nsingle station or array. This study tests an automatic method for timing Lg\narrivals using wavelet transforms to decompose the Lg signal into its\ncomponents localized both in time and scale. A Continuous Wavelet Transform\n(CWT) using a Daubechies order two (db2) wavelet is applied to 10 seconds of\nraw data, containing the start of Lg. Initial positioning of the window is\nobtained using the standard Lg travel time tables. The coefficients at scale 8\nfrom the db2 decomposition are squared and the resulting time series is\nrepresented by an approximation of the 4\u0027th level Discrete Wavelet Transform\n(DWT) using a Haar wavelet. A threshold detector is then applied to the\nresulting time series to determine the Lg arrival time. The method was tested\nusing well located earthquakes (USGS) and explosions from known mines (mb less\nthan 4.0), recorded on the vertical components at TXAR (Lajitas, Texas) and\nPDAR (Pinedale, Wyoming) arrays. The Lg arrival time was automatically picked\nwith a standard deviation of less than 1.5 seconds (less than 10 km location\nerror) for well known locations. Location errors are larger with the increase\nin distance and smaller with the increase in signal to noise ratio of events.",
"arxiv_id": "physics/9806041",
"authors": [
"Ileana M. Tibuleac",
"E. T. Herrin"
],
"categories": [
"physics.geo-ph"
],
"title": "An Automatic Method for Determination of Lg Arrival Times Using Wavelet Transforms",
"url": "https://arxiv.org/abs/physics/9806041"
},
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