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Variations of temperature and precipitation extremes in recent two decades over China

机译:近二十年来中国各地极端温度和降水的变化

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摘要

Variations of temperature and precipitation extremes were investigated under the rapid warming over China since the 1990s. Six percentile-based indices derived from daily minimum and maximum surface air temperature and daily precipitation amount at 532 meteorological observing stations were computed and compared in two periods of 1960-1989 and 1990-2007. For China as a whole, the occurrence frequencies of annual cold nights and warm nights derived from daily minimum temperature have changed by - 3.8% and 2.8% respectively, while annual cold days and warm days derived from daily maximum temperature have experienced relatively smaller variations of -2.1% and 1.8% in recent two decades. Notable frequency decreases of cold extremes were found in North China and Northeast China, whereas warm extremes increased profoundly in South China, Southwest China and Northwest China. Frequency decreases of cold extremes mainly occurred in winter. However, warm extremes displayed both remarkable frequency increases in winter and summer. Meanwhile, annual extreme precipitation amount and extreme precipitation days have separately increased by 10.9 mm and 0.12 days, with significant increases in the mid-lower Yangtze River valley and Northwest China, but only slight variations in Northeast China and North China. Considerable increases were also found in South China and Southwest China yet they were not statistically significant. Precipitation extremes were found largely increased in the rainy season from April to September, thus exhibiting similar spatial patterns to that in annual. As in the dry season from October to next March, significant increases of precipitation extremes were detected in Northeast China and North China instead.
机译:在1990年代以来中国迅速升温的情况下,研究了温度和极端降水的变化。在1960-1989年和1990-2007年这两个时期,对来自532个气象观测站的每日最低和最高地面气温以及每日降水量得出的六个基于百分位数的指数进行了计算和比较。在整个中国,由每日最低温度得出的每年冷夜和暖夜的发生频率分别改变了-3.8%和2.8%,而由每日最高温度得出的每年冷夜和暖天的变化相对较小。最近二十年分别为-2.1%和1.8%。在华北和东北地区,极端寒冷的频率明显下降,而在华南,西南和西北地区,极端温暖的频率显着增加。极端寒冷的频率下降主要发生在冬季。然而,温暖的极端在冬季和夏季都显示出明显的频率增加。同时,年极端降水量和极端降水天数分别增加了10.9mm和0.12天,其中长江中下游和西北地区有显着增加,而东北和华北只有很小的变化。在华南和西南地区也发现了相当大的增长,但它们在统计上并不显着。在4月至9月的雨季中,极端降水量大大增加,因此呈现出与年度相似的空间格局。与10月至次年3月的旱季一样,在中国东北和华北地区也发现了极端降水的显着增加。

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  • 来源
    《Atmospheric research》 |2011年第2期|p.143-154|共12页
  • 作者单位

    Key Laboratory of Mesoscale Severe Weather, Ministry of Education, and School of Atmospheric Sciences, Nanjing University, 210093, PR China;

    Key Laboratory of Mesoscale Severe Weather, Ministry of Education, and School of Atmospheric Sciences, Nanjing University, 210093, PR China;

    Key Laboratory of Mesoscale Severe Weather, Ministry of Education, and School of Atmospheric Sciences, Nanjing University, 210093, PR China;

    Key Laboratory of Mesoscale Severe Weather, Ministry of Education, and School of Atmospheric Sciences, Nanjing University, 210093, PR China;

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  • 正文语种 eng
  • 中图分类
  • 关键词

    temperature precipitation extreme events china;

    机译:温度降水极端事件中国;

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