25 research outputs found

    On the behaviour of the bounds of an analysis operator

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    On time-frequency analysis and time-limitedness

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    We study two classical problems, namely the concentration of energy problem and the truncation problem. The first problem deals with time-limited signals that have maximal energy in a certain frequency band. The second problem is about estimating the spectrum of a signal, if this signal is only known at a certain interval. Solutions of the first problem can be used to obtain good solutions for the second one by means of a preprocessing algorithm, called tapering. The truncation problem and the tapering algorithm are also studied for time-scale and time-frequency analysis, using the continuous wavelet transform and the Wigner-Ville representation

    Integral representations of affine transformations in phase space with an application to energy localization problems

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    Applying the fractional Fourier transform and the Wigner distribution on a signal in a cascade fashion is equivalent with a rotation of the time and frequency parameters of the Wigner distribution. This report presents a formula for all unitary operators that are related to energy preserving transformations on the parameters of the Wigner distribution by means of such a cascade of operators. Furthermore, such operators are used to solve certain type of energy localization problems via the Weyl correspondence

    Towards an Online Image-Based Tree Taxonomy

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    Automatic phase detection in seismic data using the discrete wavelet transform

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    Seismic data consist of traces, which contain information about a seismic event, but in some period of time the traces may be just noise. A trace which c ontains seismic information, is called a seismic signal. Seismic signals consist of several typically short energy bursts, called phases, exhibiting several patterns in terms of dominant frequency, amplitude and polarisation. Amongst others, a significant phase is the S-phase. We present a fast algorithm to detect the S-phase in a three-component seismic signal. This new approach is a combination of traditional S-phase detection methods from seismology and the discrete wavele t transform. Stability and correctness of the algorithm will be proved and results will be presented to demonstrate the algorithm
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