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Evaluation of ENSO simulations in CMIP5 models: A new perspective based on percolation phase transition in complex networks

机译:CMIP5模型中的ENSO仿真评估:基于复杂网络中渗流相变的新观点

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摘要

In this study, the performance of CMIP5 models in simulating the El Niño-Southern Oscillation (ENSO) is evaluated by using a new metric based on percolation theory. The surface air temperatures (SATs) over the tropical Pacific Ocean are constructed as a SAT network, and the nodes within the network are linked if they are highly connected (e.g., high correlations). It has been confirmed from reanalysis datasets that the SAT network undergoes an abrupt percolation phase transition when the influences of the sea surface temperature anomalies (SSTAs) below are strong enough. However, from simulations of the CMIP5 models, most models are found incapable of capturing the observed phase transition at a proper critical point Pc. For the 15 considered models, four even miss the phase transition, indicating that the simulated SAT network is too stable to be significantly changed by the SSTA below. Only four models can be considered cautiously with some skills in simulating the observed phase transition of the SAT network. By comparing the simulated SSTA patterns with the node vulnerabilities, which is the chance of each node being isolated during a ENSO event, we find that the improperly simulated sea-air interactions are responsible for the missing of the observed percolation phase transition. Accordingly, a careful study of the sea-air couplers, as well as the atmospheric components of the CMIP5 models is suggested. Since the percolation phase transition of the SAT network is a useful phenomenon to indicate whether the ENSO impacts can be transferred remotely, it deserves more attention for future model development.
机译:在这项研究中,使用基于渗流理论的新指标评估了CMIP5模型在模拟厄尔尼诺-南方涛动(ENSO)中的性能。热带太平洋上的地表空气温度(SAT)被构造为SAT网络,并且如果网络中的节点之间具有很高的连通性(例如,高相关性),则它们之间是链接的。从重新分析数据集中已经证实,当下面的海表温度异常(SSTA)的影响足够强时,SAT网络将经历突然的渗流相变。但是,通过对CMIP5模型的仿真,发现大多数模型都无法捕获在适当的临界点Pc处观察到的相变。对于15个考虑的模型,有四个甚至错过了相变,表明模拟的SAT网络太稳定而不能被下面的SSTA显着改变。在模拟观察到的SAT网络的相变时,只有一些技巧可以谨慎地考虑四个模型。通过将模拟的SSTA模式与节点脆弱性(这是ENSO事件期间每个节点被隔离的机会)进行比较,我们发现模拟海洋与空气相互作用不当是造成观测到的渗流相变缺失的原因。因此,建议仔细研究海气耦合器以及CMIP5模型的大气成分。由于SAT网络的渗透阶段过渡是一个有用的现象,它表明ENSO的影响是否可以远程转移,因此在以后的模型开发中应引起更多关注。

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