长江科学院院报 ›› 2017, Vol. 34 ›› Issue (8): 18-23.DOI: 10.11988/ckyyb.20160730

• 水资源与环境 • 上一篇    下一篇

1970—2013年大西安地区降水时空变化特征分析

从辉a, b, 周维博a, b, 宋扬a, b, 赖光东a, b, 白洁芳a, b   

  1. 长安大学 a.环境科学与工程学院;
    b.旱区地下水文与生态效应教育部重点实验室,西安 710054
  • 收稿日期:2016-07-18 修回日期:2016-09-29 出版日期:2017-08-01 发布日期:2017-08-18
  • 作者简介:从 辉(1992-),女,河北唐山人,硕士研究生,主要从事水文地质方面的研究,(电话)15829601713(电子信箱)853984166@qq.com。

Spatial and Temporal Variations of Precipitation in Big Xi'an Region During 1970-2013

CONG Hui1, 2, ZHOU Wei-bo1, 2, SONG Yang1, 2, LAI Guang-dong1, 2, BAI Jie-fang1, 2   

  1. 1.College of Environmental Science and Engineering, Chang'an University, Xi'an 710054, China;
    2.Key Laboratory of Subsurface Hydrology and Ecology in Arid Areas of Ministry of Education, Chang'an University, Xi'an 710054, China
  • Received:2016-07-18 Revised:2016-09-29 Online:2017-08-01 Published:2017-08-18
  • Contact: 周维博(1956-),男,陕西乾县人,教授,博士生导师,主要从事水资源与水环境及节水灌溉方面的研究,(电话)13991308286(电子信箱)zwbzyz823@163.com。
  • Supported by:
    中国地质调查局地质调查项目(12120113004800)

摘要: 大西安地区降水资源空间差异较大,为深入了解大西安不同区域降水时空分布特征,利用大西安地区14个气象站1970—2013年的逐月降水观测资料,采用滑动平均法、Mann-Kendall检验法、小波分析法以及克里金插值法,对大西安5个区域降水量的时空变化特征进行了分析。结果表明:大西安地区年均降水量为576.65 mm,整体呈下降趋势,下降率为-10.04 mm/(10 a),东部较西部下降显著,北部较南部下降显著;年内降水量分配不均,降水主要集中在7—9月份,占全年降水总量的50.84%,春、秋季降水量呈下降趋势,夏季降水量呈上升趋势;研究区年降水量变化的第1主周期为28 a;全区多年降水量呈现出少—多—少—多的波动趋势,突变年份为1980年和1991年;年代际降水量呈现出增加—减少—增加的趋势;年降水量空间分布不均,呈现自东南向西北逐渐减少的趋势。上述研究成果可为大西安地区降水资源的合理利用提供参考。

关键词: 大西安地区, 降水变化, 空间分布, Mann-Kendall检验法, 克里金插值法

Abstract: The spatial distribution of precipitation is uneven in Big Xi'an region. According to the monthly precipitation data from 14 meteorological stations in Big Xi'an during 1970-2013, we analyzed the spatial and temporal variations of precipitation in five areas of Big Xi'an region by using moving average method, Mann-Kendall test method, wavelet analysis method and the Kriging interpolation method. Results show that the average annual precipitation in Big Xi'an region was 576.65 mm, decreasing overall with a rate of -10.04 mm/10 a. Decreases in precipitation in the east and north of Xi'an were more obvious than those in the west and south. Moreover, the distribution of precipitation in a year was uneven, mainly from July to September, accounting for 50.84% of the total annual precipitation. In addition, precipitations in spring and autumn presented a downward trend, but precipitation in summer was in an upward trend. The first main period of annual precipitation change in the study area was 28 years. Precipitation in multiple years in the area experienced a fluctuation in “less-more-less-more” trend, with abrupt changes in 1980 and 1991; but interdecadal precipitation in the study area showed a trend from increase to decline and then to increase. In addition, the spatial distribution of annual precipitation is uneven, gradually decreasing from the southeast to the northwest. The research results could offer reference to the rational utilization of precipitation resources in Big Xi'an region.

Key words: Big Xi'an region, precipitation variation, spatial distribution, Mann-Kendall test, Kriging interpolation method

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