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首页> 外文期刊>Journal of hydrometeorology >Impact of Urbanization on Heavy Convective Precipitation under Strong Large-Scale Forcing: A Case Study over the Milwaukee-Lake Michigan Region
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Impact of Urbanization on Heavy Convective Precipitation under Strong Large-Scale Forcing: A Case Study over the Milwaukee-Lake Michigan Region

机译:强力大强迫下城市化对强对流降水的影响:以密尔沃基-密歇根湖为例

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In this study, observational and numericalmodeling analyses based on theWeather Research and Forecasting Model (WRF) are used to investigate the impact of urbanization on heavy rainfall over the Milwaukee- LakeMichigan region. The authors examine urban modification of rainfall for a stormsystemwith continentalscale moisture transport, strong large-scale forcing, and extreme rainfall over a large area of the upper Midwest of the United States. WRF simulations were carried out to examine the sensitivity of the rainfall distribution in and around the urban area to different urban land surface model representations and urban land-use scenarios. Simulation results suggest that urbanization plays an important role in precipitation distribution, even in settings characterized by strong large-scale forcing. For the Milwaukee-Lake Michigan region, the thermodynamic perturbations produced by urbanization on the temperature and surface pressure fields enhance the intrusion of the lake breeze and facilitate the formation of a convergence zone, which create favorable conditions for deep convection over the city. Analyses of model and observed vertical profiles of reflectivity using contoured frequency by altitude displays (CFADs) suggest that cloud dynamics over the city do not change significantly with urbanization. Simulation results also suggest that the large-scale rainfall pattern is not sensitive to different urban representations in the model. Both urban representations, the Noah land surface model with urban land categories and the single-layer urban canopy model, adequately capture the dominant features of this storm over the urban region.
机译:在这项研究中,基于天气研究和预报模型(WRF)的观测和数值模型分析被用于调查密尔沃基-密歇根湖地区城市化对强降雨的影响。作者研究了美国大陆中部大片地区具有大陆性水汽输送,强大的大规模强迫和极端降雨的暴风雨系统的城市降雨修正。进行了WRF模拟,以检验市区内及周边地区降雨分布对不同城市地表模型表示和城市土地利用情景的敏感性。模拟结果表明,即使在以强大的大规模强迫为特征的环境中,城市化在降水分布中也起着重要作用。对于密尔沃基-密歇根湖地区,城市化对温度和表面压力场​​产生的热力学扰动加剧了湖风的侵入,并促进了汇聚区的形成,为整个城市的深度对流创造了有利条件。使用海拔显示(CFAD)的轮廓频率对模型的反射率和观测到的反射率垂直剖面进行的分析表明,城市化过程中的云动态不会随着城市化而发生显着变化。模拟结果还表明,大规模降雨模式对模型中的不同城市表示不敏感。两种城市表示形式,具有城市土地类别的诺亚地表模型和单层城市冠层模型都充分捕捉了这场风暴在城市地区的主导特征。

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