为两种厄尔尼诺预测探索整个太平洋的敏感区域及其对目标观测的影响

Qianqian Qi, Wansuo Duan, Xia Liu, Hui Xu
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摘要

根据最有可能影响两种厄尔尼诺现象预测的整个太平洋的初始误差,利用地球物理流体动力实验室的 CM2P1(一种完全耦合的全球气候模式)确定了从 1 月开始整个太平洋的海洋温度对厄尔尼诺预测的敏感区域。误差增长分析和数值试验表明,北太平洋维多利亚模式(VM)区域的初始海洋温度将影响 CP-El Niño 的强度预测,而赤道西太平洋次表层和东南太平洋表层的初始海洋温度将调节 CP-El Niño 的空间结构预测。但对于 EP-El Niño 来说,前者加上赤道中东太平洋表层将对该事件的空间结构预测产生影响,而后者则对该事件的强度预测更为有效。此外,如果在整个太平洋的敏感区域进行有针对性的观测,那么厄尔尼诺的预测能力,包括强度和空间结构的预测,都会大大提高。在预报厄尔尼诺现象的特殊味道和强度时,不能排除亚热带太平洋敏感区和热带太平洋敏感区作为准确的指标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Exploring sensitive area in the whole pacific for two types of El Niño predictions and their implication for targeted observations
Based on the initial errors in the whole Pacific that are most likely to affect the predictions of two types of El Niño events, the sensitive area of ocean temperature in the whole Pacific for El Niño prediction starting from January is identified by using the Geophysical Fluid Dynamic Laboratory CM2P1, a fully coupled global climate model. The error growth analysis and the numerical experiments illustrated that, the initial ocean temperature in the Victoria mode (VM) region in the North Pacific will affect the intensity predictions of the CP-El Niño while that in the subsurface layer of the west equatorial Pacific and the surface layer of southeast Pacific will modulate the spatial structure predictions of CP-El Niño. But for EP-El Niño, the former plus the surface layer of the equatorial central eastern pacific will modulate the spatial structure predictions of the event while the latter is shown to be more effective in predictions of the intensity of the event. Furthermore, if targeted observations are conducted in the sensitive area of the whole Pacific, the El Niño prediction skills, including intensity and spatial structure predictions, could be greatly improved for both EP- and CP-El Niño events. Neither the sensitive area of subtropical Pacific nor the tropical Pacific can be precluded as accurate indicators when forecasting particular flavors and the intensity of El Niño events.
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