论文

Evolvement of Precipitation Extremes in Northeast China on the Background of Climate Warming

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  • 1. Chinese Academy of Meteorological Sciences, Beijing 100081;
    2. Nanjing University of Information Science and Technology, Nanjing, Jiangsu 2100441;
    3. Institute of Atmospheric Environment, China Meteorological Dministration, Shenyang, Liaoning 110016

Received date: 2007-04-12

  Revised date: 2007-09-10

  Online published: 2008-03-20

Abstract

Determination of the threshold by Gamma distribution function and study on spatial and temporal change of precipitation extremes are based on the daily precipitation data of 93 stations during the period 1959-2002 in Northeast China. The main results are summarized as follows: The precipitation extremes’ thresholds decreased gradually from the southeast littoral areas to the northwestern inland. Precipitation extremes were concentrated in June-September, and the increasing was a catastrophe during the period 1985-2002. The probability of the precipitation extremes successively occurred was greater, in which the neighbouring extremes separated by a time gap of 1-5 days was 23.7%. The total extremes increased especially in the lower reaches of the Songhua River and the Mudanjiang River,and the upper reaches of the Liaohe River,as the same with the precipitantion extreme with the time gap of 1-5 days.

Cite this article

YANG Su-Ying, SUN Feng-Hua, MA Jian-Zhong . Evolvement of Precipitation Extremes in Northeast China on the Background of Climate Warming[J]. SCIENTIA GEOGRAPHICA SINICA, 2008 , 28(2) : 224 -228 . DOI: 10.13249/j.cnki.sgs.2008.02.224

References

[1] G O P Obasi. Reducing vulnerability to weather and climate extremes, Information and Public Affairs Office. WMO,2002.
[2] Houghton J T,Y Ding, D J Griggs, et al. Climate change 2001:Scientific Basis[M]. Cambridge University Press, 2001: 881.
[3] World Meteorological Organization-No. 966, WMO Statement on the status of the global climate in 2003: global temperatures in 2003 in third warmest. Geneva, 16 December 2003.
[4] 姜付仁,程晓陶,向立云,等.美国20世纪洪水损失分析及中美90年代比较研究[J].水科学进展,114(13):384~388.
[5] 张耀存,张录军.东北气候和生态过渡区50年来降水和温度概率分布特征变化[J].地理科学,2005,25(5):561~566.
[6] 靳立亚,符娇兰,陈发虎.近44年来中国西北降水量变化的区域差异以及对全球变暖的响应[J].地理科学,2005,25(5):567~572.
[7] 王翠花,李雄,缪启龙.中国近50年来日最低气温变化特征研究[J].地理科学,2003,23(4): 442~448.
[8] 刘晓东,安芷生,方建刚,等.全球气候变暖条件下黄河流域降水的可能变化[J].地理科学,2002,22(5):513~519.
[9] 翟盘茂,潘晓华.中国北方近50年温度和降水极端降水事件变化[J].地理学报,2003,23(supplement): 1~10.
[10] 严中伟,杨赤.近几十年中国极端气候变化格局[J].气候与环境研究,2000,5(3):267~272.
[11] 刘小宁.我国暴雨极端事件的气候变化特征[J].灾害学,1999,14(1):54~59.
[12] 龚道溢,韩晖.华北农牧交错带夏季极端气候的趋势分析[J].地理学报, 2004,59(2):230~238.
[13] 孙凤华,任国玉,赵春雨,等.中国东北地区及不同典型下垫面的气温异常变化分析[J].地理科学, 2005,25(2):167~171.
[14] 孙凤华,杨素英,陈鹏狮.东北地区近44 年的气候暖干化趋势分析及可能影响[J].生态学杂志, 2005,24(7):751~755.
[15] 孙力.中国东北地区夏季旱涝的分析研究[J].地理科学,2002,22(3):311~316.
[16] Su B D, Xiao B, Zhu D, et al. Trends in frequency of precipitation extremes in the Yangtze River basin, China: 1960~2003 [J]. Hydrol. Sci. J., 2005, 50(3):479-492.
[17] Kendall M G. Rank Correlation Methods.3rd ed[M]. New York:Hafner Publishing Company, 1962.
[18] 杨素英,王谦谦,孙凤华.中国东北南部冬季气温异常及其大气环流特征变化[J].应用气象学报,2005,16(3):334~344.
[19] 卢爱刚,庞德谦,何元庆,等.全球升温对中国区域温度纬向梯度的影响[J].地理科学,2006,26(3):345~350.
[20] 许炯心.人类活动和降水变化对嘉陵江流域侵蚀产沙的影响[J].地理科学,2006,26(4): 432~487.
[21] 吴宏安,蒋建军,周杰,等.基于影象融合的干旱区城镇居民地信息提取研究[J].地理科学,2006,26(4):477~482.
[22] 曲金华,江志红,谭桂容,等.冬季北大西洋海温年际、年代际变化与中国气温的关系[J].地理科学,2006,26(5):557~563.
[23] 徐新良,刘纪远,曹明奎,等.近期气候波动与LUCC过程对东北农田生产潜力的影响[J].地理科学,2007,27(3):318~324.
[24] 何云玲,张一平,杨小波.中国内陆热带地区近40年气候变化特征[J].地理科学,2007,27(4):499~505.
[25] 房巧敏,龚道溢,毛睿.中国近46年来冬半年日降水变化特征分析[J].地理科学,2007,27(5):711~717.
[26] 李红军,江志红,魏文寿.近40年来塔里木河流域旱涝的气候变化[J].地理科学,2007,27(6):801~807.
[27] 魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,1999: 44~45.
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