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Downscaling an intense precipitation event in complexterrain: the importance of high grid resolution

机译:降低复杂 r n地形中的强降水事件的规模:高网格分辨率的重要性

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Floods due to intense rainfall are a major hazard to both people and infrastructure in western Norway. Here steep orography enhances precipitation and the complex terrain channels the runoff into narrow valleys and small rivers. In this study we investigate a major rainfall and flooding event in October 2014. We compare high-resolution numerical simulations with measurements from rain gauges deployed in the impacted region. Our study has two objectives: (i) to understand the dynamical processes that drove the high rainfall and (ii) the importance of high grid resolution to resolve intense rainfall in complex terrain. This is of great interest for numerical weather prediction and hydrological modelling. Our approach is to dynamically downscale the ERA-Interim reanalysis with the Weather Research and Forecasting model (WRF). We find that WRF gives a substantially better representation of precipitation both in terms of absolute values as well as spatial and temporal distributions than a coarse resolution reanalysis. The largest improvement between the WRF simulations is found when we decrease the horizontal model grid spacing from 9 km to 3 km. Only minor additional improvements are obtained when downscaling further to 1 km. We believe that this is mainly related to the orography in the study area and its representation in the model. Realistic representations of gravity waves and the seeder-feeder effect seem to play crucial roles in reproducing the precipitation distribution correctly. An analysis of associated wavelengths shows the importance of the shortest resolvable length scales. On these scales our simulations also show differences in accumulated precipitation of up to 300 mm over four days, further emphasising the need for resolving short wavelengths. Therefore, our results clearly demonstrate the need for high-resolution dynamical downscaling for extreme weather impact studies in regions with complex terrain.
机译:暴雨造成的洪水对挪威西部的人和基础设施均构成重大危害。这里陡峭的地形增强了降水,复杂的地形引导径流进入狭窄的山谷和小河。在这项研究中,我们调查了2014年10月的一次主要降雨和洪水事件。我们将高分辨率数值模拟与受影响地区部署的雨量计的测量结果进行了比较。我们的研究有两个目标:(i)了解导致高降雨的动力学过程,(ii)高网格分辨率对于解决复杂地形中的强降雨的重要性。这对于数值天气预报和水文建模非常感兴趣。我们的方法是使用天气研究和预报模型(WRF)动态缩减ERA-Interim重新分析的规模。我们发现,与绝对分辨率再分析相比,WRF在绝对值以及时空分布方面都能更好地表示降水。当我们将水平模型网格间距从9 km减小到3 km时,可以发现WRF模拟之间的最大改进。当进一步缩小到1 km时,只会获得较小的额外改进。我们认为这主要与研究区域的地形及其在模型中的表示有关。重力波和播种机-进料器效应的逼真的表示似乎在正确地再现降水分布中起着关键作用。对相关波长的分析显示了最短可分辨长度标尺的重要性。在这些尺度上,我们的模拟还显示了四天内累积的最大降水量差异达300毫米,进一步强调了解决短波长的需求。因此,我们的结果清楚地表明,对于地形复杂的地区的极端天气影响研究,需要高分辨率的动态降尺度。

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