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Verification of GRAPES unified global and regional numerical weather prediction model dynamic core

机译:GRAPES全球和区域统一数值天气预报模式动态核心的验证

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摘要

During the past few years, most of the new developed numerical weather prediction models adopt the strategy of multi-scale technique. Therefore, China Meteorological Administration has devoted to developing a new generation of global and regional multi-scale model since 2003. In order to validate the performance of the GRAPES (Global and Regional Assimilation and PrEdiction System) model both for its scientific design and program coding, a suite of idealized tests has been proposed and conducted, which includes the density flow test, three-dimensional mountain wave and the cross-polar flow test. The density flow experiment indicates that the dynamic core has the ability to simulate the fine scale nonlinear flow structures and its transient features. While the three-dimensional mountain wave test shows that the model can reproduce the horizontal and vertical propagation of internal gravity waves quite well. Cross-polar flow test demonstrates the rationality of both for the semi-Lagrangian departure point calculation and the discretization of the model near the poles. The real case forecasts reveal that the model has the ability to predict the large-scale weather regimes in summer such as the subtropical high, and to capture the major synoptic patterns in the mid and high latitudes.
机译:在过去的几年中,大多数新开发的数值天气预报模型都采用了多尺度技术的策略。因此,自2003年以来,中国气象局一直致力于开发新一代的全球和区域多尺度模型。为了验证GRAPES(全球和区域同化和预测系统)模型在科学设计和程序编码方面的性能,提出并进行了一套理想化测试,包括密度流动试验,三维山波和交叉极流动试验。密度流动实验表明,动态岩心具有模拟精细尺度非线性流动结构及其瞬态特征的能力。虽然三维山波测试表明该模型可以很好地再现内部重力波的水平和垂直传播。交叉极点流动测试证明了半拉格朗日出发点计算和模型在极点附近离散化的合理性。实际案例预测表明,该模型具有预测夏季诸如亚热带高压的大规模天气状况的能力,并能够捕获中高纬度地区的主要天气模式。

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