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Adaptive filtering techniques for gravitational wave interferometric data: Removing long-term sinusoidal disturbances and oscillatory transients

机译:重力波干涉数据的自适应滤波技术:消除长期正弦波干扰和振荡瞬变

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摘要

It is known by the experience gained from the gravitational wave detector prototypes that the interferometric output signal will be corrupted by a significant amount of non-Gaussian noise, a large part of it being essentially composed of long-term sinusoids with a slowly varying envelope (such as violin resonances in the suspensions, or main power harmonics) and short-term ringdown noise (which may emanate from servo control systems, electronics in a nonlinear state, etc.). Since non-Gaussian noise components make the detection and estimation of the gravitational wave signature more difficult, a denoising algorithm based on adaptive filtering techniques (LMS methods) is proposed to separate and extract them from the stationary and Gaussian background noise. The strength of the method is that it does not require any precise model on the observed data: the signals are distinguished on the basis of their autocorrelation time. We believe that the robustness and simplicity of this method make it useful for data preparation and for the understanding of the first interferometric data. We present the detailed structure of the algorithm and its application to both simulated data and real data from the LIGO 40 m prototype.
机译:从重力波检测器原型获得的经验得知,干涉测量输出信号将被大量的非高斯噪声破坏,其中很大一部分基本上是由具有缓慢变化包络的长期正弦波组成的(例如悬浮液中的小提琴共振或主电源谐波)和短期振铃噪声(可能来自伺服控制系统,处于非线性状态的电子设备等)。由于非高斯噪声分量使重力波签名的检测和估计更加困难,因此提出了一种基于自适应滤波技术(LMS方法)的去噪算法,以将其从平稳和高斯背景噪声中分离出来。该方法的优势在于,它不需要对观察到的数据建立任何精确的模型:信号是根据其自相关时间来区分的。我们相信,这种方法的鲁棒性和简便性使其可用于数据准备和理解第一个干涉测量数据。我们介绍了该算法的详细结构及其在LIGO 40 m原型中的模拟数据和实际数据中的应用。

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