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Spatiotemporal Variations of Meteorological Droughts in China During 1961–2014: An Investigation Based on Multi-Threshold Identification

机译:1961-2014年中国气象干旱的时空变化:基于多阈值识别的调查

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Abstract As a major agricultural country, China suffers from severe meteorological drought almost every year. Previous studies have applied a single threshold to identify the onset of drought events, which may cause problems to adequately characterize long-term patterns of droughts. This study analyzes meteorological droughts in China based on a set of daily gridded (0.5°?×?0.5°) precipitation data from 1961 to 2014. By using a multi-threshold run theory approach to evaluate the monthly percentage of precipitation anomalies index ( Pa ), a drought events sequence was identified at each grid cell. The spatiotemporal variations of drought in China were further investigated based on statistics of the frequency, duration, severity, and intensity of all drought events. Analysis of the results show that China has five distinct meteorological drought-prone regions: the Huang-Huai-Hai Plain, Northeast China, Southwest China, South China coastal region, and Northwest China. Seasonal analysis further indicates that there are evident spatial variations in the seasonal contribution to regional drought. But overall, most contribution to annual drought events in China come from the winter. Decadal variation analysis suggests that most of China’s water resource regions have undergone an increase in drought frequency, especially in the Liaohe, Haihe, and Yellow River basins, although drought duration and severity clearly have decreased after the 1960s.
机译:摘要中国是农业大国,几乎每年都遭受着严重的气象干旱。先前的研究已经使用单个阈值来确定干旱事件的发作,这可能会引起问题,无法充分表征长期干旱模式。本研究基于一组1961年至2014年的每日网格(0.5°?×?0.5°)降水数据,分析了中国的气象干旱。采用多阈值运行理论方法评估了降水异常指数的月百分比(Pa ),在每个网格单元处确定了干旱事件序列。根据所有干旱事件的发生频率,持续时间,严重程度和强度的统计数据,进一步调查了中国干旱的时空变化。结果分析表明,中国有五个明显的干旱干旱地区:黄淮海平原,东北,西南,华南沿海地区和西北。季节性分析进一步表明,季节性干旱对区域干旱的贡献存在明显的空间变化。但总体而言,对中国年度干旱事件的最大贡献来自冬季。年代际变化分析表明,尽管1960年代后干旱的持续时间和严重程度明显降低,但中国大多数水资源区域的干旱频率都有所增加,特别是在辽河,海河和黄河流域。

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