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A Study of ENSO Prediction Using a Hybrid Coupled Model and the Adjoint Method for Data Assimilation

机译:基于混合耦合模型和伴随方法的ENSO数据同化预测研究

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摘要

An experimental ENSO prediction system is presented, based on an ocean general circulation model (GCM) coupled to a statistical atmosphere and the adjoint method of 4D variational data assimilation. The adjoint method is used to initialize the coupled model, and predictions are performed for the period 1980-99. The coupled model is also initialized using two simpler assimilation techniques: forcing the ocean model with observed sea surface temperature and surface fluxes, and a 3D variational data assimilation (3DVAR) method, similar to that used by the National Centers for Environmental Prediction (NCEP) for operational ENSO prediction. The prediction skill of the coupled model initialized by the three assimilation methods is then analyzed and compared. The effect of the assimilation period used in the adjoint method is studied by using 3-, 6-, and 9-month assimilation periods. Finally, the possibility of assimilating only the anomalies with respect to observed climatology in order to circumvent systematic model biases is examined. It is found that the adjoint method does seem to have the potential for improving over simpler assimilation schemes. The improved skill is mainly at prediction intervals of more than 6 months, where the coupled model dynamics start to influence the model solution. At shorter prediction time intervals, the initialization using the forced ocean model or the 3DVAR may result in a better prediction skill. The assimilation of anomalies did not have a substantial effect on the prediction skill of the coupled model. This seems to indicate that in this model the climatology bias, which is compensated for by the anomaly assimilation, is less significant for the predictive skill than the bias in the model variability, which cannot be eliminated using the anomaly assimilation. Changing the optimization period from 6 to 3 to 9 months showed that the period of 6 months seems to be a near-optimal choice for this model.
机译:提出了一个实验性ENSO预测系统,该系统基于与统计大气耦合的海洋总环流模型(GCM)和4D变异数据同化的伴随方法。伴随方法用于初始化耦合模型,并对1980-99年进行预测。耦合模型还使用两种更简单的同化技术进行初始化:用观察到的海面温度和表面通量强迫海洋模型,以及类似于国家环境预测中心(NCEP)所使用的3D变异数据同化(3DVAR)方法。用于ENSO的运行预测。然后对三种同化方法初始化的耦合模型的预测技巧进行了分析和比较。通过使用3个月,6个月和9个月的同化时间,研究了伴随方法中使用的同化时间的影响。最后,研究了仅对观测到的气候进行同化以规避系统模型偏差的可能性。发现伴随方法似乎确实具有改进较简单的同化方案的潜力。技能的提高主要是在6个月以上的预测间隔内进行的,此时耦合的模型动力学开始影响模型解。在较短的预测时间间隔,使用强制海洋模型或3DVAR进行的初始化可能会导致更好的预测技能。异常的同化对耦合模型的预测技巧没有实质性影响。这似乎表明,在该模型中,由异常同化所补偿的气候偏向对于预测技能的重要性不如模型变异性中的偏向,后者无法使用异常同化来消除。将优化期从6个月更改为3到9个月表明,对于该模型,6个月似乎是最佳选择。

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