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Assessment of the Weather Research and Forecasting (WRF) model for simulation of extreme rainfall events in the upper Ganga Basin

机译:上甘地盆地极端降雨事件模拟的天气研究和预测(WRF)模型评估

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摘要

Reliable estimates of extreme rainfall events are necessary for an accurate prediction of floods. Most of the global rainfall products are available at a coarse resolution, rendering them less desirable for extreme rainfall analysis. Therefore, regional mesoscale models such as the advanced research version of the Weather Research and Forecasting (WRF) model are often used to provide rainfall estimates at fine grid spacing. Modelling heavy rainfall events is an enduring challenge, as such events depend on multi-scale interactions, and the model configurations such as grid spacing, physical parameterization and initialization. With this background, the WRF model is implemented in this study to investigate the impact of different processes on extreme rainfall simulation, by considering a representative event that occurred during 15-18 June 2013 over the Ganga Basin in India, which is located at the foothills of the Himalayas. This event is simulated with ensembles involving four different microphysics (MP), two cumulus (CU) parameterizations, two planetary boundary layers (PBLs) and two land surface physics options, as well as different resolutions (grid spacing) within the WRF model. The simulated rainfall is evaluated against the observations from 18 rain gauges and the Tropical Rainfall Measuring Mission Multi-Satellite Precipitation Analysis (TMPA) 3B42RT version 7 data. From the analysis, it should be noted that the choice of MP scheme influences the spatial pattern of rainfall, while the choice of PBL and CU parameterizations influences the magnitude of rainfall in the model simulations. Further, the WRF run with Goddard MP, Mellor-Yamada-Janjic PBL and Betts-Miller-Janjic CU scheme is found to perform "best" in simulating this heavy rain event. The selected configuration is evaluated for several heavy to extremely heavy rainfall events that occurred across different months of the monsoon season in the region. The model performance improved through incorporation
机译:对极端降雨事件的可靠估计是准确的洪水预测所必需的。大多数全球降雨产品都以粗糙的分辨率提供,使它们不太理想地用于极端降雨分析。因此,诸如天气研究和预测(WRF)模型的高级研究版等区域Messcale模型通常用于提供细网间距的降雨估计。建模大雨事件是一种持久的挑战,因为此类事件取决于多尺度交互,以及网格间距,物理参数化和初始化等模型配置。在此背景下,通过考虑在2013年6月15日至18日在印度的Ganga盆地在印度的Ganga盆地在山麓地区,研究了WRF模型,以研究不同流程对极端降雨模拟的影响。喜马拉雅山。使用涉及四种不同的微妙(MP),两个Cumulus(Cu)参数化,两个行星边界层(PBL)和两个地面物理选项的集合模拟该事件,以及WRF模型中的不同分辨率(网格间距)。评估模拟的降雨从18张雨量和热带降雨测量任务多卫星降水分析(TMPA)3B42RT版本7数据的观察。从分析中,应该指出的是,MP方案的选择会影响降雨的空间模式,而PBL和Cu参数化的选择会影响模型模拟中的降雨量。此外,使用戈达德MP,MELLOR-YAMADA-JANJIC PBL和BETTS-MILLER-JANJIC CU方案的WRF运行,在模拟这种大雨事件时执行“最佳”。所选择的配置评估了几个沉重的降雨事件,在该地区的季风季节不同的季节发生。通过公司成立改善了模型性能

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