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Spatio-temporal characteristics of precipitation and dryness/wetness in Yangtze River Delta, eastern China, during 1960-2012

机译:1960-2012年中国东部长三角地区降水与干湿变化的时空特征

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摘要

Changes in precipitation have a large effect on human society and are a key factor in the study of the patterns of hydrological and meteorological variables. Based on daily precipitation records during 1960-2012 at 24 meteorological stations in the Yangtze River Delta (YRD), the spatial and temporal variations of six extreme precipitation indices were detected by the modified Mann-Kendall test. Then, the characteristics of dryness/wetness patterns were assessed by Standardized Precipitation Index (SPI) and principal component analysis (PCA) on a 24-month time scale. For precipitation extremes, most of the precipitation indices had increasing trends, especially the annual total precipitation in wet day (PRCPTOT), which showed a significant positive trend distributed mainly in the southern part of the YRD. In contrast, decreasing trends in consecutive dry days (CDD) weredetected at most stations of the YRD, with more than 20% of the stations having negative trends that were statistically significant. Additionally, three dominant geographic sub-regions of dryness/wetness pattern were identified in YRD: the central and southern, northeastern, and northwestern areas of the YRD. With respect to temporal variations of dryness/wetness conditions in each sub-region, a long-term wet tendency in the central and southern area was characterized as being stronger than the tendency in other parts of the YRD over the past 53 years, which indicates that flood disaster may become increasingly serious in the area. Furthermore, a 4 to 8-year period of variation was observed for each sub-region. The results of this study suggest that adaptive water resource measures for future water resource management and water-related disaster reduction mitigation should be considered separately for these regions in the YRD. (C) 2016 Elsevier B.V. All rights reserved.
机译:降水变化对人类社会影响很大,是研究水文和气象变量模式的关键因素。根据1960-2012年长江三角洲(YRD)24个气象站的每日降水记录,通过改进的Mann-Kendall检验检测到六个极端降水指数的时空变化。然后,通过标准化降水指数(SPI)和主成分分析(PCA)在24个月的时间范围内评估干燥/湿润模式的特征。在极端降水方面,大多数降水指数都有增加的趋势,特别是在湿日的年总降水量(PRCPTOT),这显示出显着的正趋势,主要分布在长江三角洲的南部。相比之下,在长三角地区的大多数气象站都发现连续干旱天数(CDD)下降的趋势,其中超过20%的气象站具有统计上显着的负趋势。此外,在长三角地区确定了三个主要的干湿分布地理分区:长三角地区的中部和南部,东北和西北地区。关于每个分区的干湿状况随时间的变化,过去53年来,中部和南部地区的长期湿润趋势要强于长三角其他地区的趋势,这表明该地区的洪灾可能变得越来越严重。此外,每个子区域观察到4至8年的变化期。这项研究的结果表明,应为长三角地区的这些地区分别考虑用于未来水资源管理和减少与水有关的减灾的适应性水资源措施。 (C)2016 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Atmospheric research》 |2016年第mayajun期|196-205|共10页
  • 作者单位

    Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;

    Guangxi Normal Univ, Sch Environm Sci & Resources, Guilin 541000, 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; Dryness/Wetness characteristics; Yangtze River Delta; China;

    机译:降水;干湿特性;长三角;

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