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Analysis of intraseasonal and interannual variability of the Asian summer monsoon using a hidden Markov model.

机译:利用隐马尔可夫模型分析亚洲夏季风的季节内和年际变化。

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Intraseasonal and interannual variability of Asian summer monsoon rainfall in pentad precipitation data is examined using a hidden Markov model (HMM). The spatial patterns of discrete rainfall states derived with the HMM and the associated transition probabilities between the states are shown to represent well the principal Asian summer monsoon intraseasonal oscillation (ISO), propagating eastward and northward with a period of 40-50 days. Stochastic simulations made with the HMM reasonably reproduce the canonical ISO propagation and its observed statistics such as the frequency of ISO events. The interannual modulation of the ISO associated with El Nino-Southern Oscillation (ENSO) is assessed by employing a nonhomogeneous HMM (NHMM) with summer-mean Nino-3.4 index prescribed as an input variable. ENSO influence on the ISO is found to manifest as preferences toward particular ISO phases depending on the ENSO condition, thus adding an asymmetry to the ISO. In the presence of seasonal mean anomalies, it is shown that the El Nino seasonal mean rainfall anomaly pattern is identified by the HMM as a distinct state, in addition to the ISO states, whereas the La Nina seasonal mean rainfall anomaly pattern does not appear distinct from the ISO states.Digital Object Identifier http://dx.doi.org/10.1175/2010JCLI3473.1
机译:使用隐马尔可夫模型(HMM)检查了五单元降水数据中亚洲夏季风的季节内和年际变化。用HMM推导出的离散降雨状态的空间格局以及状态之间的相关过渡概率已很好地代表了主要的亚洲夏季风季内季节内振荡(ISO),向东和向北传播40-50天。用HMM进行的随机模拟合理地再现了规范的ISO传播及其观察到的统计数据,例如ISO事件的发生频率。与厄尔尼诺-南方涛动(ENSO)相关的ISO的年际调制通过采用非均质HMM(NHMM)进行评估,其中夏季平均Nino-3.4指数被指定为输入变量。发现ENSO对ISO的影响表现为对特定ISO阶段的偏爱,具体取决于ENSO条件,从而给ISO增加了不对称性。在存在季节性平均异常的情况下,表明HMM将厄尔尼诺季节性平均降雨异常模式识别为ISO状态之外的一个独特状态,而拉尼娜季节性平均降雨异常模式则没有明显区别。来自ISO国家/地区。数字对象标识符http://dx.doi.org/10.1175/2010JCLI3473.1

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