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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Season-dependent dynamics of nonlinear optimal error growth and El Ni?o-Southern Oscillation predictability in a theoretical model
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Season-dependent dynamics of nonlinear optimal error growth and El Ni?o-Southern Oscillation predictability in a theoretical model

机译:理论模型中非线性最优误差增长和厄尔尼诺-南振荡的可预测性的季节相关动力学

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Most state-of-the-art climate models have difficulty in the prediction of El Ni?o-Southern Oscillation (ENSO) starting from preboreal spring seasons. The causes of this spring predictability barrier (SPB) remain elusive. With a theoretical ENSO system model, we investigate this controversial issue by tracing the evolution of conditional nonlinear optimal perturbation (CNOP) and by analyzing the behavior of initial error growth. The CNOPs are the errors in the initial states of ENSO events, which have the biggest impact on the uncertainties at the prediction time under proper physical constraints. We show that the evolution of CNOP-type errors associated with El Ni?o episodes depends remarkably on season with the fastest growth occurring during boreal spring in the onset phase. There also exist other kinds of initial errors, which have either somewhat smaller growth rates or neutral ones during spring. However, for La Ni?a events, even if initial errors are of CNOP-type, the errors grow without significant seasonal dependence. These findings suggest that the SPB in this model results from combined effects of three factors: the annual cycle of the mean state, the structure of El Ni?o, and the pattern of the initial errors. On the basis of the error tendency equations derived from the model, we addressed how the combination of the three factors causes the SPB and proposed a mechanism responsible for the error growth in the model ENSO events. Our results help in clarifying the role of the initial error pattern in SPB, which may provide a clue for explaining why SPB can be eliminated by improving initial conditions. The results also illustrate a theoretical basis for improving data assimilation in ENSO prediction.
机译:从春季前的春季开始,大多数最新的气候模型都难以预测厄尔尼诺-南方涛动(ENSO)。造成这种春天可预测性障碍(SPB)的原因仍然难以捉摸。借助理论ENSO系统模型,我们通过跟踪条件非线性最优摄动(CNOP)的演化并分析初始误差增长的行为来研究这个有争议的问题。 CNOP是ENSO事件初始状态中的错误,在适当的物理约束下,它们对预测时的不确定性影响最大。我们表明,与厄尔尼诺现象有关的CNOP型错误的演变显着取决于季节,在发病初期在北方春季期间生长最快。还存在其他类型的初始误差,这些误差在春季期间具有较小的增长率或中性。但是,对于La Ni?a事件,即使初始误差是CNOP类型的,误差也会在没有明显的季节依赖性的情况下增长。这些发现表明,该模型中的SPB来自三个因素的综合影响:平均状态的年周期,厄尔尼诺现象的结构以及初始误差的模式。基于从模型导出的误差趋势方程式,我们解决了三个因素的组合如何导致SPB的问题,并提出了导致ENSO模型事件中误差增长的机制。我们的结果有助于阐明初始错误模式在SPB中的作用,这可能为解释为什么可以通过改善初始条件而消除SPB提供线索。结果还说明了改善ENSO预测中数据同化的理论基础。

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