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A downscaling approach for constructing high-resolution precipitation dataset over the Tibetan Plateau from ERA5 reanalysis

机译:从ERA5 Reany分析构建藏高高原高分辨率降水数据集的镇压方法

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摘要

Current gridded precipitation datasets are hard to meet the requirements of hydrological and meteorological applications in complex-terrain areas due to their coarse spatial resolution and large uncertainties. Highresolution atmospheric simulations are capable of describing the influence of topography on precipitation but are difficult to be used to obtain long-term precipitation datasets because they are computationally expensive, while reanalysis data has a long-term coverage and can provide reasonable large-scale spatial and temporal variability of precipitation. This study presents an approach to obtain long-term high-resolution precipitation datasets over complex-terrain areas by combining the ERA5 reanalysis with short-term high-resolution atmospheric simulation. The approach consists of two main steps: first, the ERA5 precipitation is corrected by the high-resolution simulation at the coarse spatial resolution; second, the corrected data is downscaled using a convolution neural network (CNN) based model at daily scale. The proposed approach is applied to the Tibetan Plateau (TP). The downscaled results from ERA5 have a finer spatial structure than ERA5 and can reproduce the spatial patterns of precipitation revealed by the high-resolution simulation. An evaluation based on rain gauge data shows that the downscaled ERA5 has remarkably lower biases than the original ERA5 which overestimates precipitation a lot, and even higher accuracy than the high-resolution simulation data over the TP. The downscaled ERA5 preserves the temporal characteristics of ERA5 which are more consistent with the rain gauge data than that of high-resolution simulation. Since this approach is much less computing resources consuming than the high-resolution simulation, it is an effective method to obtain long-term high-resolution precipitation datasets in complex-terrain areas and is expected to have extensive applications.
机译:由于其粗糙的空间分辨率和大的不确定性,电流包装的降水数据集很难满足复杂地形区域中水文和气象应用的要求。高度大气模拟能够描述地形对沉淀的影响,而是难以用于获得长期降水数据集,因为它们是计算昂贵的,而再分析数据具有​​长期覆盖,可以提供合理的大规模空间和沉淀的时间变异性。本研究提出了一种方法,通过与短期高分辨率大气模拟结合ERA5再分析来获得复杂地形区域的长期高分辨率降水数据集。该方法由两个主步骤组成:首先,通过粗糙空间分辨率的高分辨率模拟来校正ERA5沉淀;其次,校正数据在日常比例下使用基于卷积神经网络(CNN)的模型来缩小。所提出的方法适用于藏高原(TP)。来自ERA5的较低的结果具有比ERA5更精细的空间结构,并且可以再现高分辨率模拟所揭示的降水的空间模式。基于雨量数据的评估表明,较低的ERA5的偏差显着低于原始ERA5,它超要降水量大量,甚至比TP上的高分辨率模拟数据更高的精度。较低的ERA5保留了ERA5的时间特征,其与雨量计数据更符合高于高分辨率模拟。由于这种方法的计算资源远低于高分辨率模拟,因此在复杂地形区域中获得长期高分辨率降水数据集是一种有效的方法,并且预计将具有广泛的应用。

著录项

  • 来源
    《Atmospheric research》 |2021年第7期|105574.1-105574.12|共12页
  • 作者单位

    Chinese Acad Sci Natl Tibetan Plateau Data Ctr Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes & Land Surface P Beijing 100101 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Tsinghua Univ Dept Earth Syst Sci Minist Educ Key Lab Earth Syst Modeling Beijing 100084 Peoples R China|Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing 100101 Peoples R China;

    Tsinghua Univ Dept Earth Syst Sci Minist Educ Key Lab Earth Syst Modeling Beijing 100084 Peoples R China;

    Chinese Acad Sci Natl Tibetan Plateau Data Ctr Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes & Land Surface P Beijing 100101 Peoples R China;

    Southwest Univ Sch Geog Sci Chongqing 400715 Peoples R China;

    Chinese Acad Sci Natl Tibetan Plateau Data Ctr Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes & Land Surface P Beijing 100101 Peoples R China|Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing 100101 Peoples R China;

    Chinese Acad Meteorol Sci Beijing 100081 Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Precipitation; Complex terrain; Downscale; High-resolution atmospheric simulation; Convolution neural network (CNN);

    机译:降水;复杂的地形;低级;高分辨率大气模拟;卷积神经网络(CNN);

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