Weber Philipp, Wang Fengzhong, Vodenska-Chitkushev Irena, Havlin Shlomo, Stanley H Eugene
Center for Polymer Studies and Department of Physics, Boston University, Boston, Massachusetts 02215, USA.
Phys Rev E Stat Nonlin Soft Matter Phys. 2007 Jul;76(1 Pt 2):016109. doi: 10.1103/PhysRevE.76.016109. Epub 2007 Jul 24.
We analyze the memory in volatility by studying volatility return intervals, defined as the time between two consecutive fluctuations larger than a given threshold, in time periods following stock market crashes. Such an aftercrash period is characterized by the Omori law, which describes the decay in the rate of aftershocks of a given size with time t by a power law with exponent close to 1. A shock followed by such a power law decay in the rate is here called Omori process. We find self-similar features in the volatility. Specifically, within the aftercrash period there are smaller shocks that themselves constitute Omori processes on smaller scales, similar to the Omori process after the large crash. We call these smaller shocks subcrashes, which are followed by their own aftershocks. We also show that the Omori law holds not only after significant market crashes as shown by Lillo and Mantegna [Phys. Rev. E 68, 016119 (2003)], but also after "intermediate shocks." By appropriate detrending we remove the influence of the crashes and subcrashes from the data, and find that this procedure significantly reduces the memory in the records. Moreover, when studying long-term correlated fractional Brownian motion and autoregressive fractionally integrated moving average artificial models for volatilities, we find Omori-type behavior after high volatilities. Thus, our results support the hypothesis that the memory in the volatility is related to the Omori processes present on different time scales.
我们通过研究波动回报间隔来分析波动中的记忆性,波动回报间隔定义为股市崩盘后的时间段内,两个连续大于给定阈值的波动之间的时间。这样的崩盘后时期具有大森定律的特征,该定律描述了给定规模余震的发生率随时间t以指数接近1的幂律衰减。在此,随后发生率呈这种幂律衰减的冲击被称为大森过程。我们在波动中发现了自相似特征。具体而言,在崩盘后时期内存在较小的冲击,这些冲击本身在较小尺度上构成大森过程,类似于大崩盘后的大森过程。我们将这些较小的冲击称为子崩盘,随后是它们自己的余震。我们还表明,大森定律不仅在如利洛和曼泰尼亚[《物理评论E》68, 016119 (2003)]所展示的重大市场崩盘后成立,而且在“中等冲击”后也成立。通过适当的去趋势处理,我们从数据中消除了崩盘和子崩盘的影响,发现这一过程显著降低了记录中的记忆性。此外,在研究长期相关的分数布朗运动和自回归分数整合移动平均波动率人工模型时,我们在高波动率后发现了大森型行为。因此,我们的结果支持了波动中的记忆性与不同时间尺度上存在的大森过程相关这一假设。