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Dynamical regimes and transitions in Plio-Pleistocene Asian monsoon

机译:亚洲上新世-上新世季风的动力机制和过渡

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We propose a novel approach based on the fluctuation of similarity to identify regimes of distinct dynamical complexity in short time series. A statistical test is developed to estimate the significance of the identified transitions. Our method is verified by uncovering bifurcation structures in several paradigmatic models, providing more complex transitions compared with traditional Lyapunov exponents. In a real-world situation, we apply this method to identify millennial-scale dynamical transitions in Plio-Pleistocene proxy records of the South Asian summer monsoon system. We infer that many of these transitions are induced by the external forcing of the solar insolation and are also affected by internal forcing on Monsoonal dynamics, i.e., the glaciation cycles of the Northern Hemisphere and the onset of the Walker circulation.
机译:我们提出了一种基于相似度波动的新颖方法,以识别短时间序列中不同动态复杂度的机制。开发了统计测试以估计已识别转换的重要性。我们的方法通过在几个范例模型中发现分叉结构而得到验证,与传统的Lyapunov指数相比,它提供了更复杂的过渡。在现实世界中,我们应用此方法来确定南亚夏季风系统的上新世更新记录中的千年尺度动力学转变。我们推断,这些过渡中的许多是由日照的外在强迫引起的,并且还受季风动力学的内在强迫影响,即北半球的冰川周期和沃克环流的开始。

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