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Statistical detection of meteor showers using data from the Swedish infrasound network Ludwik Liszka Swedish Institute of Space Physics SLU 901 83 Umea, Sweden
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Swedish Infrasound Network Present stations: Kiruna Jamton Lycksele Uppsala
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Search for small and medium meteor events – objectives: To search for meteor events below the infrasonic background level To establish a set of indicators which can be used to discriminate a single event To develop techniques for extraction of events from combined multi-station data
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Meteor on 2002-12-30 in Morjärv, Northern Sweden
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Morjärv Meteor
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Angle-of-arrival = 208º Vp = 350 m/s
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Morjärv Meteor
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How to optimize the indicators? Principal Component Analysis (PCA) of multiple indicator data Indicators are distributions of variables: Angle-of-arrival Phase velocity Crosscorrelation Spectral slope
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Principal component analysis Purpose: to find a direction where maximum variance may be found in multivariate data
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PCA Direction of maximum variance
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Angle-of-arrival Entropy = -1.18 (Emax=0, Emin=-2.42)
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Phase velocity Vp
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Cross-correlation
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Spectral slope
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Parameters of the analysis 1 window = 128 data points (7.11 sec) The window is moved in 32p steps (overlap) Distributions are created for each sample of 50 positions of the window 16 samples / 30 minutes
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Discrimination of meteor impacts Selection of data to find proper combination of indicators: Concorde vs. North Sea Meteor Another approach is to apply PCA without pre-selecting transformation coefficients
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Comparison of indicators
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Plot of component loadings
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High cross-correlation counts
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Meteor discrimination
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Bavarian Meteor 2002-04-06 5th principal component
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Discriminant function based on 5 th PC
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Small meteors – meteor showers Leonids – 2002-11-18
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Small meteors – meteor showers Leonids – 2001-11-18
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Combination of information from 2 stations (North Sea Meteor) Lycksele - Jamton
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Combination of information from 2 stations (North Sea Meteor) Lycksele - Kiruna
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Combination of information from 2 stations (Leonids 2002-11-18) Lycksele - Jamton
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Conclusions PCA may be used to discriminate events with a specific signature, like meteor impacts The method may be applied to events below the noise level, for example, meteor showers
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