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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >A sensitivity study of the Kelvin wave and the Madden-Julian Oscillation in aquaplanet simulations by the Naval Research Laboratory Spectral Element Atmospheric Model
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A sensitivity study of the Kelvin wave and the Madden-Julian Oscillation in aquaplanet simulations by the Naval Research Laboratory Spectral Element Atmospheric Model

机译:开尔文波和敏感性研究在aquaplanet Madden-Julian振荡海军研究实验室的模拟光谱元素大气模型

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摘要

The dynamical core of the Naval Research Laboratory (NRL) Spectral Element Atmospheric Model (NSEAM) is coupled with full physics and used to investigate the organization and propagation of equatorial atmospheric waves under the aquaplanet conditions. The sensitivity of the model simulation to the amount of horizontal viscosity, distribution of the vertical levels, and selected details of the precipitation physics is examined and discussed mainly utilizing simulated convective precipitation with the aid of time-longitude plots and the spectral diagrams designed by Wheeler and Kiladis (1999). It is shown that the simulation of the Kelvin wave and Madden-Julian Oscillation depends strongly on the details of the vertical level distribution and the choice of parameters in the convective parameterization. Efforts are made to calibrate the new model to capture the essential interaction between the dynamics and physics of the atmosphere. The speed and spectrum of the eastward propagating Kelvin waves and the signature of the Madden-Julian Oscillation simulated by the new model reveal main features similar to those predicted by the simplified theory and found in limited observations. This study attempts to understand the significant variability found among the aquaplanet simulations by various global atmospheric models and highlights the uncertainties concerning convective processes and their coupling to large-scale wave motion in large-scale models of the atmosphere.
机译:海军研究的动力核心实验室(海军)大气光谱元素模型(NSEAM)与完整的物理和耦合调查组织和使用赤道下大气波的传播aquaplanet条件。模型模拟的水平粘度、垂直分布的水平,和选择的细节降水物理检查和讨论主要利用吗模拟对流降水与援助time-longitude的情节和光谱图设计的惠勒和Kiladis(1999)。开尔文波的模拟和显示Madden-Julian振动强烈依赖细节的垂直分布和水平对流参数的选择参数化。新模型来捕获必不可少的动力学和物理之间的相互作用大气中。向东传播开尔文波和Madden-Julian振荡的签名新模型的模拟显示主要特征类似预测的简化理论和有限的观察中发现。研究试图理解的重要可变性aquaplanet中发现通过各种全球大气模型模拟并强调不确定性有关对流过程及其耦合大规模的波动在大规模的模型大气中。

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