初始条件对大气环流模式的影响

Y. Guan, W. Lu, G. Zhou
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摘要

本文进行了两次连续17年的集合后播数值试验,初始条件为实时预报采用的NCEP-DOE Reanalysis 2数据,第二次试验采用三维变分同化系统(3D-VAR)提供的数据,每次试验有5个单元集合。本文使用的模式是由中国科学院大气物理研究所(IAP9L2x2.5-AGCM)研制的网格点大气环流模式,垂直高度为9个,纬向分辨率为20,纵向分辨率为2.50。应用了相关分析技术。对比结果表明:(1)两种初始条件下热带地区的时间异常系数差异很小,而中高纬度地区,特别是东亚(中国)地区的时间异常系数差异较大;(2)中国大部分地区实验2的时间异常系数大于实验1。(3)利用数据同化后的初始条件(实验2),多个变量的空间异常相关性也有不同程度的改善,即定量地表明初始条件对东亚短期气候预测的作用比全球更重要,且同化后的初始条件在一定程度上优于实时预测。因此,初始条件对大气环流模式的影响是不可忽视的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The effect of initial conditions on Atmospheric General Circulation Model
Two numerical experiments of ensemble hindcasting for 17 years are performed here, initial conditions are NCEP-DOE Reanalysis 2 data (adopted in the real-time prediction) and that in the second are supplied by the system of three-dimensional variational assimilation (3D-VAR), and there are five-member ensembles in each experiment. The model is used here which is a grid-point Atmospheric General Circulation Model with 9 vertical levels and a resolution of 20 in latitudinal and 2.50 in longitudinal direction, developed by the Institute of Atmospheric Physics, the Chinese Academy of Sciences (IAP9L2x2.5-AGCM). The technique of Correlation Analysis is applied. Comparison results show that (1) the difference of temporal anomaly coefficient is very small in the tropics under two different initial conditions, whereas it is large in middle and high latitudes, especially in East Asia (China) region, (2) temporal anomaly coefficient in the experiment 2 is bigger than that in the experiment 1 in most of China region, (3) spatial anomaly correlation of many variables has also different degree improvement by use of the initial conditions after data assimilation(in the experiment 2). That is to say, the results demonstrate quantitatively that the role of initial conditions on short-term climate prediction in East Asia is more important than in the global, what's more, the initial conditions after data assimilation are better than that in the real-time prediction to some extend. So, the effect of initial conditions on atmospheric general circulation model is not neglected.
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