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An intercomparison of multiple statistical downscaling methods for daily precipitation and temperature over China: future climate projections

机译:中国日降水量和温度多种统计镇流量方法的相互熟练:未来的气候预测

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摘要

In this study, we use four statistical downscaling methods to statistically downscale seven Coupled Model Intercomparison Project (CMIP5) Global Climate Models (GCMs) and project the changes in precipitation and temperature over China under RCP4.5 and RCP8.5 emission scenarios. The four statistical downscaling methods are bias-correction and spatial downscaling (BCSD), bias-correction and climate imprint(BCCI), bias correction constructed analogues with quantile mapping reordering(BCCAQ), and cumulative distribution function transform(CDF-t). Though large inter-model variability exists in the distribution and magnitude of changes in projected precipitation, particularly for wet spell length (CWD), all downscaling methods generally project a consistent enhancement of precipitation in both summer and winter over most parts of China. For the arid and semiarid Northwest China, the shortened dry spell length (CDD) is accompanied by the pronouncedly intensified very wet days (R95p), as well as the increase in maximum 5-day precipitation amount (Rx5day). In contrast, southeastern regions may experience more consecutive dry days and more severe wet precipitation extremes. The projected changes from different downscaling techniques are fairly similar for temperature, apart from the diurnal temperature range for BCSD. Warming is projected across the whole domain with larger magnitude over the north and in winter under RCP8.5. More summer days and fewer frost days would appear in the future. The bias correction components of downscaling methods cause a higher degree of agreement among models, and the downscaled results generally retain the main climate change signal of the driving models.
机译:在本研究中,我们使用四种统计缩小方法来统计缩小七耦合模型相互熟悉项目(CMIP5)全球气候模型(GCMS),并在RCP4.5和RCP8.5发射方案下将降水量和温度的变化项目投影。四种统计缩小方法是偏压和空间缩小(BCSD),偏置校正和气候印记(BCCI),偏置校正构造了与定量映射重新排序(BCCAQ)和累积分布函数变换(CDF-T)的类似物。虽然在预计降水量的变化的分布和程度上存在大型模型间可变性,但对于湿法法规长度(CWD),所有次要方法通常会在中国大多数地区的夏季和冬季进行一致的降水增强。对于中国西北地区的干旱和半干旱,缩短的干法(CDD)伴随着发音强化的非常潮湿的天(R95P),以及最大5天降水量(RX5Day)的增加。相比之下,东南部地区可能会经历更连续的干燥日,更严重的湿沉淀极端。除了BCSD的昼夜温度范围之外,来自不同尺寸技术的预计变化与温度相当相似。在RCP8.5下,在整个领域中投射到整个领域的整个领域,在北部和冬季更大。未来会出现更多夏日,霜冻时间较少。缩小方法的偏置校正组件在模型之间导致更高程度的一致性,并且缩小结果通常保留驾驶模型的主要气候变化信号。

著录项

  • 来源
    《Climate dynamics》 |2019年第11期|6749-6771|共23页
  • 作者单位

    Nanjing Univ Inst Climate & Global Change Res Sch Atmospher Sci CMA NJU Joint Lab Climate Predict Studies 163 Xianlin Rd Nanjing Jiangsu Peoples R China;

    Nanjing Univ Inst Climate & Global Change Res Sch Atmospher Sci CMA NJU Joint Lab Climate Predict Studies 163 Xianlin Rd Nanjing Jiangsu Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Key Lab Reg Climate Environm Temperate East Asia Beijing Peoples R China;

    Nanjing Univ Inst Climate & Global Change Res Sch Atmospher Sci CMA NJU Joint Lab Climate Predict Studies 163 Xianlin Rd Nanjing Jiangsu Peoples R China;

    Nanjing Univ Inst Climate & Global Change Res Sch Atmospher Sci Nanjing Jiangsu Peoples R China;

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

    Statistical downscaling; Climate change; Intercomparison; China; Extreme;

    机译:统计贬低;气候变化;互相;中国;极端;

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