干旱区研究 ›› 2011, Vol. 28 ›› Issue (6): 944-949.

• 气候及其灾害 • 上一篇    下一篇

陕西秦岭南北旱涝灾害时空变化趋势分析

 宋春英, 延军平, 张立伟   

  1. 陕西师范大学 旅游与环境学院,陕西 西安 710062
  • 收稿日期:2010-11-04 修回日期:2010-12-09 出版日期:2011-11-15 发布日期:2012-01-16
  • 作者简介:宋春英(1986-),女,山东菏泽人,硕士研究生,主要从事全球变化与自然灾害研究.E-mail:songchunying@stu.snnu.edu.cn
  • 基金资助:

    国家自然科学基金项目“秦岭南北全球变化适应度评价及可持续发展模式选择”(40871052)资助

Temporal and Spatial Trends of Drought and Flood in the South and North of the Qinling Mountains in Shaanxi Province

 SONG  Chun-Ying, YAN  Jun-Ping, ZHANG  Li-Wei   

  1. College of Tourism and Environment Sciences, Shaanxi Normal University, X]i’an 710062, China
  • Received:2010-11-04 Revised:2010-12-09 Online:2011-11-15 Published:2012-01-16

摘要: 根据1961-2009年秦岭南北57个站点的月降水资料,采用区域旱涝指标和[WTBX]Z[WTBZ]指数,运用MannKendall检验、小波分析、Kriging插值等方法,对秦岭南北旱涝时空变化趋势进行分析。结果表明:① 关中地区年平均气温倾向率大于陕南,气温突变年均为1996年。② 近49年来,关中地区暖干化及春旱、夏涝的趋势较陕南显著。气温突变后秦岭南北重旱频次所占比例均增大,偏涝比例均减小。关中旱涝存在明显的3~4年和22~27年的变化周期,陕南存在3~4年和24~30年的旱涝周期,这种变化周期与厄尔尼诺和太阳活动周期相对应。③ 秦岭南北年大旱频次,陕南大于关中。大涝频次分布规律性不强,中心点零星分布。冬季旱涝频次呈纬向分布,春、夏季和秋季呈经向分布。

关键词: 气候变化, 旱涝灾害, 时空分布, 变化周期, 厄尔尼诺, 秦岭, 陕西

Abstract: Based on the monthly precipitation data observed by 57 meteorological stations in the Qinling Mountains during the period from 1961 to 2009, this paper analyzes the temporal and spatial trends of drought and flood in the north and south of the Qinling Mountains and the response of regional drought index and Z index to global climate change using mainly the MK mutation test, wavelet analysis and Kriging interpolation. The conclusions are as follow: (1) Climate trend rate of average annual temperature in Guanzhong was higher than that in south Shaanxi Province, and the abrupt change of average annual temperature occurred in 1996 in these two areas; (2) In recent 49 years, the warmingdrying trend, spring drought and summer flood in Guanzhong were more significant than that in south Shaanxi Province. The proportion of severe drought increased in both the north and south of the Qinling Mountains, but that of partial flood decreased after the abrupt change of average annual temperature. There were the 3-4year and 22-27year periodicities of drought and flood in Guanzhong, but 3-4year and 24-30year ones in south Shaanxi Province, and these periodicities corresponded to the occurrence of El Nino and solar activity; (3) Frequency of severe drought in south Shaanxi Province was higher than that in Guanzhong. The distribution regularity of annual severe flood frequency was not strong, and the centers were scattered. Frequency of drought and flood was distributed in a latitudinal way in winter but in a longitudinal way in other seasons.

Key words: climate change, drought, spatio temporal distribution, periodic variations, El Nino, the Qinling Mountains, Shaanxi Province

中图分类号: 

  • P426.616