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Multi-nested WRF simulations for studying planetary boundary layer processes on the turbulence-permitting scale in a realistic mesoscale environment

机译:用于研究行星边界层过程的多套合WRF模拟,湍流允许在逼真的Mescle环境中的湍流尺度

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The Weather Research and Forecasting (WRF) model was applied in a nested configuration from a 2.7?km convection-permitting domain via grey-zone resolutions of 900?m and 300?m down to the 100?m turbulence-permitting scale. Based on sensitivity studies, this approach was optimized to investigate the evolution of small-scale processes in the PBL for a clear sky case during the HOPE experiment in western Germany on 24 April 2013. The results were compared with theoretical and experimental findings from literature and high-resolution lidar observations collected during the campaign. Simulations with parameterized turbulence were able to capture the temporal evolution of the PBL height, but almost no internal structure was simulated in the boundary layer. Only the turbulence-permitting simulations were capable of reproducing the morning transition from the stable nighttime to the daytime convective boundary layer and the following break-up into turbulent eddies. Comparisons with lidar data showed that the turbulence-permitting simulations reproduced the observed turbulence statistics. Nevertheless, the potential temperature in the boundary layer was 1?K cooler than observed, caused by a lower surface temperature mixed upward by the turbulent eddies. The simulated PBL height was underestimated by 200?m, reflected in a well-captured profile of specific humidity up to a height of 900?m and an overly strong decrease of moisture above. The general shape of the variance profiles of potential temperature and specific humidity were captured by the model. However, the simulated variability throughout the boundary layer was lower and the different heights of the variance peaks indicated that the model may not fully capture the turbulent processes at the top of the boundary layer. Identifying those systematic differences between nested simulations and observations demonstrated the value of this model approach for process studies and parameterization tests.
机译:天气研究和预测(WRF)模型应用于从2.7 km对流允许的域通过900?m和300?m的灰色区域分辨率到达100?m绕动概况。基于敏感性研究,经过优化,这种方法是在2013年4月24日在希望在德国希望实验期间探讨PBL的小规模过程的演变。结果与文学的理论和实验结果进行了比较。结果和实验结果在活动期间收集的高分辨率激光雷达观察结果。具有参数化湍流的模拟能够捕获PBL高度的时间演变,但在边界层中几乎没有模拟内部结构。只有湍流允许的仿真能够从稳定的夜间转换到白天对流边界层,并且在湍流涡流中的分解中再现。利用LIDAR数据的比较表明,湍流允许仿真再现观察到的湍流统计。然而,边界层中的潜在温度比观察到的1Ω·k冷却,由湍流漩涡向上混合的较低表面温度引起。模拟PBL高度被200μm低估,在特定湿度的良好捕获的曲线上反映至高度为900Ωm的高度,并且上面的水分过度降低。模型捕获了潜在温度和特定湿度的方差轮廓的一般形状。然而,整个边界层的模拟可变性较低,方差峰的不同高度表明,该模型可能无法完全捕获边界层顶部的湍流过程。识别嵌套模拟与观察之间的系统差异表明了该模型方法进行过程研究和参数化测试的值。

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