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首页> 外文期刊>Journal of hydrometeorology >Validation of a High-Resolution Version of the Regional Climate Model RegCM3 over the Carpathian Basin
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Validation of a High-Resolution Version of the Regional Climate Model RegCM3 over the Carpathian Basin

机译:喀尔巴阡盆地区域气候模式RegCM3高分辨率版本的验证

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This paper presents a validation study for a high-resolution version of the Regional Climate Model version 3 (RegCM3) over the Carpathian basin and its surroundings. The horizontal grid spacing of the model is 10 km the highest reached by RegCM3. The ability of the model to capture temporal and spatial variability of temperature and precipitation over the region of interest is evaluated using metrics spanning a wide range of temporal (daily to climatology) and spatial (inner domain average to local) scales against different observational datasets. The simulated period is 1961-90. RegCM3 shows small temperature biases but a general overestimation of precipitation, especially in winter; although, this overestimate may be artificially enhanced by uncertainties in observations. The precipitation bias over the Hungarian territory, the authors' main area of interest, is mostly less than 20%. The model captures well the observed late twentieth-century decadal-to-interannual and interseasonal variability. On short time scales, simulated daily temperature and precipitation show a high correlation with observations, with a correlation coefficient of 0.9 for temperature and 0.6 for precipitation. Comparison with two Hungarian station time series shows that the model performance does not degrade when going to the 10-km gridpoint scale. Finally, the model reproduces the spatial distribution of dry and wet spells over the region. Overall, it is assessed that this high-resolution version of RegCM3 is of sufficiently good quality to perform climate change experiments over the Carpathian region and, in particular, the Hungarian territory for application to impact and adaptation studies.
机译:本文针对喀尔巴阡盆地及其周围地区的高分辨率区域气候模型版本3(RegCM3)进行了验证研究。该模型的水平网格间距是RegCM3达到的最高10 km。使用跨越不同观察数据集的大范围时间尺度(从每日到气候)和空间尺度(从内域到局部)的度量来评估模型捕获感兴趣区域上温度和降水的时空变化的能力。模拟期为1961-90年。 RegCM3表现出较小的温度偏差,但普遍高估了降水,尤其是在冬天;虽然,高估可能会因观测不确定性而人为地加剧。作者主要关注的匈牙利领土上的降水偏向大多不到20%。该模型很好地捕捉了二十世纪后期观测到的年代际到年际和季节间的变化。在短时间尺度上,模拟的每日温度和降水与观测值显示高度相关,温度的相关系数为0.9,降水的相关系数为0.6。与两个匈牙利气象站时间序列的比较表明,当达到10公里的网格点比例时,模型的性能不会降低。最后,该模型再现了该区域干,湿拼写的空间分布。总体而言,据评估,RegCM3的高分辨率版本具有足够好的质量,可以在喀尔巴阡地区,尤其是匈牙利领土上进行气候变化实验,以应用于影响和适应研究。

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