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Evaluation of NU-WRF Rainfall Forecasts for IFloodS

机译:评估IFloodS的NU-WRF降雨预测

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The Iowa Flood Studies (IFloodS) campaign was conducted in eastern Iowa as a pre-GPM-launch campaign from 1 May to 15 June 2013. During the campaign period, real-time forecasts were conducted utilizing the NASA-Unified Weather Research and Forecasting (NU-WRF) Model to support the daily weather briefing. In this study, two sets of the NU-WRF rainfall forecasts are conducted with different soil initializations, one from the spatially interpolated North American Mesoscale Forecast System (NAM) and the other produced by the Land Information System (LIS) using daily analysis of bias-corrected stage IV data. Both forecasts are then compared with NAM, stage IV, and Multi-Radar Multi-Sensor (MRMS) quantitative precipitation estimation (QPE) to understand the impact of land surface initialization on the predicted precipitation. In general, both NU-WRF runs are able to reproduce individual peaks of precipitation at the right time. NU-WRF is also able to replicate a better rainfall spatial distribution compared with NAM. Further sensitivity tests show that the high-resolution runs (1 and 3 km) are able to better capture the precipitation event compared to its coarser-resolution counterpart (9 km). Finally, the two sets of NU-WRF simulations produce very close rainfall characteristics in bias, spatial and temporal correlation scores, and probability density function. The land surface initialization does not show a significant impact on short-term rainfall forecast, which is largely because of high soil moisture during the field campaign period.
机译:2013年5月1日至6月15日,在爱荷华州东部开展爱荷华州洪水研究(IFloodS)运动,这是GPM之前的一项运动。在运动期间,利用NASA统一的天气研究和预报( NU-WRF)模型来支持每日天气简报。在这项研究中,使用不同的土壤初始化方法进行了两组NU-WRF降雨预测,一组来自空间插值的北美中尺度预报系统(NAM),另一组由土地信息系统(LIS)使用偏差的日常分析产生-校正的IV阶段数据。然后将这两个预测与NAM,第四阶段和多雷达多传感器(MRMS)定量降水估计(QPE)进行比较,以了解地面初始化对预测降水的影响。通常,两种NU-WRF运行都能够在适当的时间再现各个降水峰。与NAM相比,NU-WRF还能够复制更好的降雨空间分布。进一步的敏感性测试表明,与分辨率较粗略的分辨率(9 km)相比,高分辨率分辨率(1 km和3 km)能够更好地捕获降水事件。最后,两组NU-WRF模拟在偏差,空间和时间相关性得分以及概率密度函数方面产生了非常接近的降雨特征。地表初始化对短期降雨预报没有显着影响,这主要是由于田间运动期间土壤湿度高。

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