近50年西南地区降水的时空分布特征
Spatial and Temporal Distribution Characteristics of Precipitation over Southwest China in the Past 50 Years
摘要:
利用1960~2014年的西南地区93个站的逐月降水资料,统计分析了西南地区(95˚E~111˚E, 20˚N~35˚N)全年和春、夏、秋、冬季降水的时空分布特征。取得主要结论如下:1) 降水时间分布上,西南地区夏季降水最多;而冬季降水最少。同时西南地区全年和夏季降水量在1968年最多,而在2011年最少;春季降水量在1990年最多,而在1979年最少;秋季降水量在1982年最多,而在2009年最少;冬季降水量在1969年最多,而在2009年最少。2) 降水空间分布上总体存在三个特点:一是西南地区降水有从东到西递减的趋势;二是川西高原为少雨区并且在四川中部有一多雨区;三是西南地区夏季是多雨季,而冬季是少雨季。3) 对西南地区降水的EOF分析而言,我国西南地区全年、春季、夏季、秋季和冬季降水第一模态在空间上都表现为全区一致性,具有下降的年际变化特征。
Abstract:
Using monthly precipitation data from 93 stations in southwest China from 1960 to 2014, the spa-tial and temporal distribution of precipitation in spring, summer, autumn, winter and annual in southwest China was statistically analyzed. The main conclusions are as follows: 1) In terms of precipitation time distribution, summer precipitation is the most, and winter precipitation is the least. The annual average and summer precipitation in the southwest was the highest in 1968, and the lowest in 2011; Spring precipitation was the highest in 1990 and the lowest in 1979; Autumn precipitation was the highest in 1982 and the lowest in 2009; Winter precipitation was the highest in 1969 and the lowest in 2009. 2) There are three characteristics in the spatial distribution of precipitation: first, there is a trend of decreasing precipitation in southwest region from east to west; second, the western of Sichuan plateau is a less rain area and there is a rain-prone area in central of Sichuan; third, southwest region summer is a more rain season, but winter is a less rain season. 3) For the EOF analysis of precipitation in southwest China, the first modal of annual, spring, summer, autumn and winter precipitation in southwest China is consistent in space and has the characteristics of declining inter-annual variation.
参考文献
|
[1]
|
Solomon, S., Qin, D. and Manning, M. (2007) The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Computational Geometry, 2, 1-21.
|
|
[2]
|
Trenberth, K.E. (1998) Atmos-pheric Moisture Residence Times and Cycling: Implications for Rainfall Rates with Climate Change. Climate Change, 39, 667-694. [Google Scholar] [CrossRef]
|
|
[3]
|
Allen, M.R. and Ingram, W.J. (2002) Constraints on the Future Changes in Cli-mate and the Hydrological Cycle. Nature, 419, 224-232. [Google Scholar] [CrossRef] [PubMed]
|
|
[4]
|
闵屾, 钱永甫. 中国极端降水事件的区域性和持续性研究[J]. 水科学进展, 2008, 19(6): 763-761.
|
|
[5]
|
孙清元, 郑万模, 倪化勇. 我国西南地区山地灾害灾情年际综合评估[J]. 沉积与特提斯地质, 2007, 27(3): 105-107.
|
|
[6]
|
崔云, 孔纪名, 田述军. 强降雨在山地灾害链成灾演化中的关键控制作用[J]. 山地学报, 2011, 29(1): 87-89.
|
|
[7]
|
张天宇, 程炳岩, 刘晓冉, 等. 重庆汛期极端降水事件分析[J]. 热带气象学报, 2009, 25(4): 475-482.
|
|
[8]
|
叶香, 陆维松, 张天宇, 等. 近46a重庆汛期极端降水量异常特征[J]. 南京气象学院学报, 2008, 31(5): 646-654.
|
|
[9]
|
刘丽, 陶云. 云南省汛期极端强降水事件的气候特征[J]. 干旱气象, 2012, 30(1): 15-20.
|
|
[10]
|
张顺谦, 马振峰. 1961~2009年四川极端强降水变化趋势与周期性分析[J]. 自然资源学报, 2011, 26(11): 1918-1929.
|
|
[11]
|
王学锋, 郑小波, 黄玮, 等. 近47年云贵高原汛期强降水和极端降水变化特征[J]. 长江流域资源与环境, 2010, 19(11): 1350-1355.
|
|
[12]
|
张焕, 翟盘茂, 唐红玉. 1961~2000年西南地区小时降水变化特征[J]. 气候变化研究进展, 2011, 7(1): 8-13.
|