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首页> 外文期刊>Journal of Applied Meteorology and Climatology >Wind-Blown Dust Modeling Using a Backward-Lagrangian Particle Dispersion Model
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Wind-Blown Dust Modeling Using a Backward-Lagrangian Particle Dispersion Model

机译:使用后拉拉格兰粒子分散模型的风吹粉尘建模

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Presented here is a new dust modeling framework that uses a backward-Lagrangian particle dispersion model coupled with a dust emission model, both driven by meteorological data from the Weather Research and Forecasting (WRF) Model. This new modeling framework was tested for the spring of 2010 at multiple sites across northern Utah. Initial model results for March-April 2010 showed that the model was able to replicate the 27-28 April 2010 dust event; however, it was unable to reproduce a significant wind-blown dust event on 30 March 2010. During this event, the model significantly underestimated PM2.5 concentrations (4.7 vs 38.7 mu g m(-3)) along the Wasatch Front. The backward-Lagrangian approach presented here allowed for the easy identification of dust source regions with misrepresented land cover and soil types, which required an update to WRF. In addition, changes were also applied to the dust emission model to better account for dust emitted from dry lake basins. These updates significantly improved dust model simulations, with the modeled PM2.5 comparing much more favorably to observations (average of 30.3 mu g m(-3)). In addition, these updates also improved the timing of the frontal passage within WRF. The dust model was also applied in a forecasting setting, with the model able to replicate the magnitude of a large dust event, albeit with a 2-h lag. These results suggest that the dust modeling framework presented here has potential to replicate past dust events, identify source regions of dust, and be used for short-term forecasting applications.
机译:这里提出的是一种新的粉尘建模框架,它使用了由来自天气研究和预测(WRF)模型的气象数据驱动的灰尘发射模型的后向拉格朗日粒子分散模型。这一新的建模框架在犹他州北部的多个地点进行了测试。 2010年3月至4月的初始模型结果表明,该模型能够复制2010年4月27日至28日尘埃事件;但是,它无法在2010年3月30日恢复了一个重要的风吹尘埃事件。在此活动期间,该模型沿着播种机前面明显低估了PM2.5浓度(4.7 Vs 38.7 mu g m(-3))。这里展示的后向拉格朗日方法允许容易地识别具有歪曲的陆地覆盖和土壤类型的灰尘源区,这需要更新到WRF。此外,还将变化应用于粉尘发射模型,以更好地解释从干燥的湖泊盆地排放的灰尘。这些更新显着改善了粉尘模型模拟,模拟的PM2.5对观察更有利的比较(平均为30.3μgm(-3))。此外,这些更新还改善了WRF内部通道的定时。粉尘模型也应用于预测环境,模型能够复制大型尘埃事件的大小,尽管具有2-H滞后。这些结果表明,这里呈现的粉尘建模框架具有复制过去的粉尘事件,识别灰尘源区,并用于短期预测应用。

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