Koffi Justin Kouame, F. D. B. Bouo, Y. Tchétché, D. Gbè, P. Assamoi
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引用次数: 0
Abstract
In this paper, a sensitivity study of convection schemes and cloud microphysics is performed using the Weather Research and Forecasting (WRF) model. It concerns the mesoscale simulation of the squall line observed during the African Monsoon Multidisciplinary Analysis campaign on September 22nd, 2006. Four convection schemes (Kain-Fritsch, Grell-Devenyi, Tietke and New Simplified Arakawa-Schubert) and five microphysics schemes (WRF Single-Moment 3-class (WSM3), WRF Single-Moment 5-class (WSM5), WRF Single-Moment 6-class (WSM6), Thompson and NSSL2-moment) are used. Each microphysics scheme is associated with a convection scheme, giving twenty combinations. The goal is to find the combination able to provide a realistic representation of the meteorological fields associated to the studied squall line, especially those of precipitation. The New Simplified Arakawa-Schubert convection scheme combined either with the WSM6 microphysics scheme, either with the WSM5 microphysics scheme or Thompson scheme was found to give a result closer to observation. The study also confirms that convection schemes have much more influence than microphysics on precipitation heights.
本文利用天气研究与预报(WRF)模式对对流方案和云微物理进行了敏感性研究。对2006年9月22日非洲季风多学科分析活动观测到的飑线进行了中尺度模拟。采用了4种对流格式(Kain-Fritsch、Grell-Devenyi、Tietke和New Simplified Arakawa-Schubert)和5种微物理格式(WRF single -矩3类(WSM3)、WRF single -矩5类(WSM5)、WRF single -矩6类(WSM6)、Thompson和nssl2 -矩)。每个微物理方案都与一个对流方案相关联,有20种组合。目标是找到能够提供与所研究的飑线有关的气象场,特别是降水的气象场的真实表示的组合。新简化Arakawa-Schubert对流格式与WSM6微物理格式、WSM5微物理格式或Thompson格式结合后得到的结果更接近观测值。研究还证实对流方案比微物理方案对降水高度的影响要大得多。