Achleitner Stefan, Fach Stefan, Einfalt Thomas, Rauch Wolfgang
Unit of Environmental Engineering, Institute of Infrastructure, University of Innsbruck, Technikerstr. 13, Innsbruck A-6020, Austria.
Water Sci Technol. 2009;59(6):1145-51. doi: 10.2166/wst.2009.098.
Nowcasting of rainfall may be used additionally to online rain measurements to optimize the operation of urban drainage systems. Uncertainties quoted for the rain volume are in the range of 5% to 10% mean square error (MSE), where for rain intensities 45% to 75% MSE are noted. For larger forecast periods up to 3 hours, the uncertainties will increase up to some hundred percents. Combined with the growing number of real time control concepts in sewer systems, rainfall forecast is used more and more in urban drainage systems. Therefore it is of interest how the uncertainties influence the final evaluation of a defined objective function. Uncertainty levels associated with the forecast itself are not necessarily transferable to resulting uncertainties in the catchment's flow dynamics. The aim of this paper is to analyse forecasts of rainfall and specific sewer output variables. For this study the combined sewer system of the city of Linz in the northern part of Austria located on the Danube has been selected. The city itself represents a total area of 96 km2 with 39 municipalities connected. It was found that the available weather radar data leads to large deviations in the forecast for precipitation at forecast horizons larger than 90 minutes. The same is true for sewer variables such a CSO overflow for small sub-catchments. Although the results improve for larger spatial scales, acceptable levels at forecast horizons larger than 90 minutes are not reached.
除了在线雨量测量外,还可使用降雨临近预报来优化城市排水系统的运行。所引用的雨水量不确定性在均方误差(MSE)的5%至10%范围内,其中降雨强度的均方误差为45%至75%。对于长达3小时的更长预报期,不确定性将增加到数百%。随着下水道系统中实时控制概念的不断增加,降雨预报在城市排水系统中的应用越来越多。因此,不确定性如何影响定义的目标函数的最终评估是一个值得关注的问题。与预报本身相关的不确定性水平不一定会转化为流域水流动力学中产生的不确定性。本文的目的是分析降雨预报和特定下水道输出变量。对于本研究,选择了位于多瑙河北部奥地利林茨市的合流制排水系统。该市总面积为96平方公里,连接了39个市政当局。研究发现,对于大于90分钟的预报期,可用的气象雷达数据会导致降水预报出现较大偏差。对于小流域的下水道变量,如合流污水溢流,情况也是如此。尽管在更大空间尺度上结果有所改善,但在大于90分钟的预报期内仍未达到可接受水平。