论文标题

Wavescan:重力波数据的多解析回归

Wavescan: multiresolution regression of gravitational-wave data

论文作者

Klimenko, Sergey

论文摘要

识别嵌入非平稳噪声的瞬态重力波信号需要分析所得时间序列中时间依赖的光谱成分。信号功率的时频分布可以用Gabor原子或小波来估计,通过窗口函数在时间和频率上进行定位。这种分析受到海森堡 - 盖布尔的不确定性的限制,这种不确定性不允许在时间和频率上同时使用单个小波进行高分辨率定位。结果,时间和光谱泄漏会影响时频分布,从而限制了功率谱中尖锐特征的识别。本文提出了一种时频回归方法,其中用不同窗口的小波堆栈跨越了各种分辨率,用于在每个时间频率的位置扫描功率。这样的小波扫描(称为WaveScan中的纸张)扩展了传统的多分辨率分析,以捕获瞬态信号并由于时间和光谱泄漏而删除局部功率变化。在每个时间频率位置从堆栈中选择一个最小影响泄漏的小波,以获得功率的高分辨率定位。本文介绍了多分辨率WAVESCAN回归的所有阶段,包括时间变化频谱的估计,时间频率域中瞬态信号的识别以及相应的时域波形的重建。为了证明该方法的性能,将WAVESCAN回归应用于Ligo探测器的重力波数据。

Identification of a transient gravitational-wave signal embedded into non-stationary noise requires the analysis of time-dependent spectral components in the resulting time series. The time-frequency distribution of the signal power can be estimated with Gabor atoms, or wavelets, localized in time and frequency by a window function. Such analysis is limited by the Heisenberg-Gabor uncertainty, which does not allow a high-resolution localization of power with individual wavelets simultaneously in time and frequency. As a result, the temporal and spectral leakage affects the time-frequency distribution, limiting the identification of sharp features in the power spectrum. This paper presents a time-frequency regression method where instead of a single window, a stack of wavelets with different windows spanning a wide range of resolutions is used to scan power at each time-frequency location. Such a wavelet scan (dubbed in the paper as wavescan) extends the conventional multiresolution analysis to capture transient signals and remove the local power variations due to the temporal and spectral leakage. A wavelet, least affected by the leakage, is selected from the stack at each time-frequency location to obtain the high-resolution localization of power. The paper presents all stages of the multiresolution wavescan regression, including the estimation of the time-varying spectrum, identification of transient signals in the time-frequency domain, and reconstruction of the corresponding time-domain waveforms. To demonstrate the performance of the method, the wavescan regression is applied to the gravitational wave data from the LIGO detectors.

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