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Ensemble prediction for nowcasting with a convection-permitting model—I: description of the system and the impact of radar-derived surface precipitation rates

机译:对流允许模型的综合预报预报——I:系统描述以及雷达衍生的地面降水速率的影响

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摘要

A key strategy to improve the skill of quantitative predictions of precipitation, as well as hazardous weather such as severe thunderstorms and flash floods is to exploit the use of observations of convective activity (e.g. from radar). In this paper, a convection-permitting ensemble prediction system (EPS) aimed at addressing the problems of forecasting localized weather events with relatively short predictability time scale and based on a 1.5 km grid-length version of the Met Office Unified Model is presented. Particular attention is given to the impact of using predicted observations of radar-derived precipitation intensity in the ensemble transform Kalman filter (ETKF) used within the EPS. Our initial results based on the use of a 24-member ensemble of forecasts for two summer case studies show that the convective-scale EPS produces fairly reliable forecasts of temperature, horizontal winds and relative humidity at 1 h lead time, as evident from the inspection of rank histograms. On the other hand, the rank histograms seem also to show that the EPS generates too much spread for forecasts of (i) surface pressure and (ii) surface precipitation intensity. These may indicate that for (i) the value of surface pressure observation error standard deviation used to generate surface pressure rank histograms is too large and for (ii) may be the result of non-Gaussian precipitation observation errors. However, further investigations are needed to better understand these findings. Finally, the inclusion of predicted observations of precipitation from radar in the 24-member EPS considered in this paper does not seem to improve the 1-h lead time forecast skill.
机译:提高对降水以及严重雷暴和山洪等危险天气的定量预测技能的一项关键策略是利用对流活动观测值(例如来自雷达的观测值)的使用。本文提出了一种对流集成预报系统(EPS),该系统旨在解决基于可预测时间尺度相对较短的气象局统一模型的1.5 km网格长度版本的局部天气事件的预​​报问题。特别注意在EPS中使用的集合变换卡尔曼滤波器(ETKF)中使用雷达派生的降水强度的预测观测值的影响。我们的初步结果基于对两个夏季案例研究使用的24人预报集合,表明对流规模EPS在提前1小时的时间段内就温度,水平风和相对湿度产生了相当可靠的预报,从检查中可以明显看出等级直方图。另一方面,等级直方图似乎也表明EPS产生的散布太大,无法预测(i)表面压力和(ii)表面降水强度。这些可能表明,对于(i)用于生成表面压力等级直方图的表面压力观测误差标准偏差值太大,并且对于(ii)可能是非高斯降水观测误差的结果。但是,需要进一步调查以更好地理解这些发现。最后,本文所考虑的24人EPS中包含雷达的降水观测预报似乎并未提高1小时提前期预报技能。

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