阐述了阿拉木图预报试验场地磁动态观测时间序列中异常识别方法应用的主要成果。以往所利用稳定地磁场中异常探索的方法,在北天山条件下按构造磁效应未能得到积极的结果。在许多情况下,地磁场谱特性的相关函数、子波分析及异常和噪音的分位量纲计算都能识别作为地震前兆的中、短期异常。 The main results of the application of the method of anomaly identification in the time series of magnetic dynamic observation in the Almaty prediction test site are described. In the past, the method of anomaly exploration in a stable geomagnetic field failed to obtain a positive result according to the magnetic effect in the North Tianshan Mountains. In many cases, correlation functions of geomagnetic field spectral characteristics, wavelet analysis, and quantile dimension calculations of anomalies and noises can be identified as medium- and short-term anomalies that are precursors to earthquakes.