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首页> 外文期刊>Quarterly Journal of the Royal Meteorological Society >On the dynamical downscaling and bias correction of seasonal-scale winter precipitation predictions over North India
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On the dynamical downscaling and bias correction of seasonal-scale winter precipitation predictions over North India

机译:印度北部季节尺度冬季降水预报的动态降尺度和偏差校正

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This study presents the results of high-resolution (30 km) climate simulations over North India using an optimized configuration of the Regional Climate Model (RegCM), driven by a global spectral model (T80 model with horizontal resolution of similar to 1.4.) for a period of 28 years (1982-2009). The main aim of this work is to analyze the capabilities of the RegCM to simulate the wintertime precipitation over North India in the recent past. The RegCM validation revealed a good improvement in reproducing the precipitation compared to results obtained from the T80 model. This improvement comes due to better representation of vertical pressure velocity, moisture transport, convective heating rate and temperature gradient at two different latitudinal zones. Moreover, orography in the high-resolution RegCM improves the precipitation simulation in the region where sharp orography gradient plays an important role in wintertime precipitation processes. Two bias correction (BC) methods namely mean bias-remove (MBR) and quantile mapping (QM) have been applied on the T80 driven RegCM model simulations. It was found that the QM method is more skillful than the MBR in simulating the wintertime precipitation over North India. A comparison of model-simulated and bias corrected precipitation with observed precipitation at 17 station locations has also been carried out. Overall, the results suggest that when the BC is applied on dynamically downscaled model, it has better skill in simulating the precipitation over North India and this model is a useful tool for further regional downscaling studies.
机译:这项研究使用区域光谱模型(RegCM)的优化配置,由全球光谱模型(水平分辨率近似于1.4的T80模型)驱动,展示了印度北部高分辨率(30 km)气候模拟的结果。期限为28年(1982年至2009年)。这项工作的主要目的是分析RegCM模拟最近印度北部冬季降水的能力。与从T80模型获得的结果相比,RegCM验证显示出在再现降水方面有很好的改善。该改进归因于在两个不同纬度区域上更好地表示了垂直压力速度,水分输送,对流加热速率和温度梯度。此外,高分辨率RegCM的地形学改善了陡峭的地形学梯度在冬季降水过程中起重要作用的区域的降水模拟。 T80驱动的RegCM模型仿真已应用了两种偏差校正(BC)方法,即均值偏差去除(MBR)和分位数映射(QM)。研究发现,在模拟印度北部冬季降水时,QM方法比MBR更熟练。还进行了模型模拟和偏正校正的降水与在17个观测站位置观测到的降水的比较。总体而言,结果表明,将BC应用于动态降尺度模型时,它具有更好的模拟印度北部降水的技能,该模型是进行进一步的区域降尺度研究的有用工具。

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