长江流域资源与环境 >> 2018, Vol. 27 >> Issue (04): 829-.doi: 10.11870/cjlyzyyhj201804014

• 生态环境 • 上一篇    下一篇

我国南方地区50 a冬季降水和相对湿度特征分析

曾波1, 王钦2   


  1. (1.中国气象局成都高原气象研究所/高原与盆地暴雨旱涝灾害四川省重点实验室,四川 成都 610072;
    2.中国民航飞行学院广汉分院,四川 广汉 618307)
  • 出版日期:2018-04-21

Analysis of Precipitation and Relative Humidity in Winter in South of China in the Past 50 Years#br#

ZENG Bo1,WANG Qing2   

  1.  
    (1.Chengdu Institute of Plateau Meteorological, China Meteorology Administration/Heavy Rain and DroughtFlood
     Disasters in Plateau and Basin Key Laboratory of Sichuan Province, Chengdu 610072, China;
    2.Civil Aviation Flight University of China, Guanghan 618307,China)
  • Online:2018-04-21

摘要:

根据中国地面气候日值数据集资料,利用气候趋势系数、气候倾向率等方法,研究了我国南方地区冬季50 a降水和湿度的时空变化特征,并运用基尼系数对降水均匀性的空间分布进行了分析。结果表明:降水和相对湿度分布皆自西北向东南递增,最大中心位于长江以南附近内陆区域,最小值基本位于高原。降水强度整体呈现增加趋势,在沿长江附近区域以及云南部分地区增强明显,最大气候倾向率为1.0 mm/d/10 a左右,有明显的突变时间,为1979年;降水量呈微弱的增加趋势,其中云贵和川渝局部区域降水量呈减少趋势,为-3 mm/10 a左右,没有明显的突变时间;降水日数在长江以南局部区域及云贵区域显著减少,其中云南的西南地区为最小气候倾向率-10 d/10 a,明显突变时间为1980年;相对湿度表现出一定的局地增减趋势,长江以北(南)主要呈微弱增加(减少)趋势,云南南部减小趋势显著;相对湿度和降水呈明显的正相关,其中与降水量和降水日数相关系数高达0.784、0.753。降水量基尼系数的空间分布与降水分布相似,只是降水分布的大(小)值中心为基尼系数小(大)值中心,不同年代及冬季不同月份的降水量基尼系数大(小)值区域范围有所增减。总的来看,我国南方冬季中部和东部大部分区域为降水均匀区,西南高原区域为不均匀区。
关键词: 南方地区;冬季;降水;相对湿度

Abstract:

Based on the Chinese surface climatologically daily dataset, the time and spatial variation of precipitation and relative humidity of 50 winters in the South China are studied by using the methods of climate tendency coefficient, climate tendency rate, and so on. Furthermore the spatial distribution of precipitation uniformity is analyzed by using Gini coefficient. The results show that the precipitation and relative humidity increased from northwest to southeast, the maximum center is located at the inland area near the south of Yangtze River, and the minimum center is located at plateau. The precipitation intensity increased overall, the region along the Yangtze River and part of Yunnan province increased obviously, the maximum climate tendency rate is about 1 mm/ day /10 a, and there is obvious mutation in 1979; precipitation increased slightly, but in the area of Yunnan, Guizhou and part of SichuanChongqin province, the precipitation amount showed a decreasing trend, about -3 mm/10 a, there is no obvious mutation; the precipitation days reduced significantly in the south of Yangtze River, Yunnan and Guizhou province, the minimum climate tendency rate in the southwest of Yunnan is about -10 days /10 a, mutation time is 1980; relative humidity showed a trend of increase or decrease locally, the relative humidity increased(decreased) slightly in the north(south) of the Yangtze River, the trend in south Yunnan is decreased significantly. There is positive relationship between relative humidity and precipitation, especially the relative coefficient with the precipitation amount and precipitation days is up to 0.784 and 0.753 respectively. The spatial pattern of Gini coefficient is similar to that of precipitation, however maximum (minimum) center of precipitation is corresponding to the center of minimum (maximum) of Gini coefficient, the range of maximum or minimum region has some variation in different periods and different months of winter. Generally speaking, most region of central and eastern South China in winter is precipitation homogeneous area, and the southwest plateau is uneven area.
Key words:South China; winter; precipitation; relative humidity

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