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Estimating observing locations for advancing beyond the winter predictability barrier of Indian Ocean dipole event predictions

机译:估计超出印度洋偶极子事件预测的冬季可预测性障碍的观测地点

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摘要

In this paper, we explored potential observing locations (i.e., the sensitive areas) of positive Indian Ocean dipole (IOD) events to advance beyond the winter predictability barrier (WPB) using the geophysical fluid dynamics laboratory climate model version 2p1 (GFDL CM2p1). The sensitivity analysis is conducted through perfect model predictability experiments, in which the model is assumed to be perfect and so any prediction errors are caused by initial errors. The results show that the initial errors with an east-west dipole pattern are more likely to result in a significant WPB than spatially correlated noises; the areas where the large values of the dipole pattern initial errors are located have great effects on prediction uncertainties in winter and provide useful information regarding the sensitive areas. Further, the prediction uncertainties in winter are more sensitive to the initial errors in the subsurface large value areas than to those in the surface large value areas. The results indicate that the subsurface large value areas are sensitive areas for advancing beyond the WPB of IOD predictions and if we carry out intensive observations across these areas, the prediction errors in winter may be largely reduced. This will lead to large improvements in the skill of wintertime IOD event forecasts.
机译:在本文中,我们使用地球物理流体动力学实验室气候模型版本2p1(GFDL CM2p1)探索了正印度洋偶极子(IOD)事件可能超越冬季可预测性壁垒(WPB)的潜在观测地点(即敏感区域)。敏感性分析是通过理想的模型可预测性实验进行的,其中假定模型是理想的,因此任何预测误差都是由初始误差引起的。结果表明,与空间相关噪声相比,东西向偶极子模式的初始误差更可能导致明显的WPB。偶极子图形初始误差大的区域对冬季的预测不确定性有很大影响,并提供有关敏感区域的有用信息。此外,冬季的预测不确定性对地下大价值区的初始误差比对地面大价值区的初始误差更为敏感。结果表明,地下大价值区域是超越IOD预报工作量的敏感区域,如果我们在这些区域进行深入观察,冬季的预报误差可能会大大减少。这将大大提高冬季IOD事件预测的技巧。

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