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Simulation of a persistent medium-term precipitation event over the western Iberian Peninsula

机译:伊比利亚半岛西部持续中期降水事件的模拟

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This study evaluated the performance of the WRFARW (Weather Research and Forecasting with Advanced Research) weather prediction model in simulating the spatial and temporal patterns of an extreme rainfall period over a complex orographic region in north-central Portugal. The analysis was performed during the rainy season and, more specifically, the month of December 2009. In this period, the region of interest was under the influence of a sequential passage of low-pressure systems associated with frontal surfaces. These synoptic weather patterns were responsible for long periods of rainfall, resulting in a high monthly precipitation. The WRF model results during the study period were furthermore evaluated with the specific objective to complement gaps in the precipitation recordings of a reference meteorological station (located in Pousadas), the data of which are fundamental for hydrological studies in nearby experimental catchments. Three distinct WRF model runs were forced with initial fields and boundary conditions obtained from a global domain model: (1) a reference experiment with no nudging (RunRef); (2) observational nudging for a specific location, i.e. the above-mentioned Pousadas reference station (RunObsN); and (3) nudging to the analysed field (Run- GridN). Model performance was evaluated, using several statistical parameters, against a dataset of 27 rainfall stations that were grouped by elevation. The three model runs had similar performances, even though RunGridN resulted in a slight improvement. Regarding the other two experiments, this improvement justifies its use for complementing the surface measurements at the Pousadas reference station. Overall model accuracy, expressed in root mean square error (RMSE), of the three runs was comparable for the stations of the different elevations classes. Even so, it was slightly better for stations in the lowlands than the highlands. Furthermore, model predictions tended to be less accurate for stations located in rough terrain and deep valleys.
机译:这项研究评估了WRFARW(天气预报和高级研究天气预报)天气预报模型在模拟葡萄牙中北部复杂地形区域上极端降雨期的时空格局方面的性能。该分析是在雨季,尤其是2009年12月进行的。在此期间,感兴趣的区域受到与额表面相关的低压系统相继通过的影响。这些天气状况导致长时间的降雨,导致每月高降水量。此外,还以特定目的评估了研究期间的WRF模型结果,以补充参考气象站(位于Pousadas)的降水记录中的差距,这些数据对于附近实验流域的水文研究至关重要。从全局域模型获得的初始场和​​边界条件迫使三个不同的WRF模型运行:(1)不带微调的参考实验(RunRef); (2)对特定位置,即上述的Pousadas参考站(RunObsN),进行观测推射; (3)轻触分析的字段(RunGridN)。使用几个统计参数,针对按海拔高度分组的27个降雨站的数据集,评估了模型的性能。尽管RunGridN略有改进,但三个模型运行具有相似的性能。关于其他两个实验,此改进证明其可用于补充Pousadas参考站的表面测量。这三个运行的总体模型精度以均方根误差(RMSE)表示,在不同海拔级别的站点上具有可比性。即使这样,在低地站比高地站要好一些。此外,对于位于崎terrain地形和深谷中的测站,模型预测往往不太准确。

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