干旱区研究 ›› 2016, Vol. 33 ›› Issue (3): 619-627.doi: 10.13866/j.azr.2016.03.23

• 气候变化 • 上一篇    下一篇

秦岭南北气候干湿变化与降水非均匀性的关系

李英杰, 延军平, 刘永林   

  1. 陕西师范大学旅游与环境学院,陕西 西安 710062
  • 收稿日期:2015-08-25 修回日期:2015-11-14 出版日期:2016-05-15 发布日期:2016-05-31
  • 作者简介:李英杰(1990-),男,硕士,主要从事全球气候变化与区域灾害防治研究. E-mail: lyj@snnu.edu.cn
  • 基金资助:
    教育部人文社会科学重点研究基地重大项目(15JJD790022);国家社会科学基金重点项目(14AZD094,14XKS019)资助

Relationship between Dryness/Wetness and Precipitation Heterogeneity in the North and South of the Qinling Mountains

LI Ying-jie, YAN Jun-ping, LIU Yong-lin   

  1. College of Tourism and Environmental Sciences,Shaanxi Normal University,Xi'an 710062,Shaanxi,China
  • Received:2015-08-25 Revised:2015-11-14 Published:2016-05-15 Online:2016-05-31

摘要: 选取1960—2014年秦岭南北27个气象站点的逐月气象资料,基于Hurst指数、Mann-Kendall检验、小波分析等方法,分析了秦岭南北干湿变化、降水非均匀性及两者相关性。结果表明:① 近55 a来秦岭南北趋于干旱化,1994年气候突变后干旱化趋势尤为显著,Hurst指数表明此干旱化趋势将进一步持续。地域上,以秦岭主山脉为界,秦岭南北呈“南湿北干”的空间格局。② 秦岭以南降水集中度(PCD)高于秦岭以北,全区PCD呈显著上升趋势,且有自西向东扩展的演变趋势。③ 标准化降水蒸散指数(SPEI)与PCD呈显著(P<0.02)正相关,秦岭以南普遍高于秦岭以北;而SPEI与降水集中期(PCP)的相关性则较差。④ 秦岭南北大部地区降水越分散,气候越趋于干旱。

关键词: 标准化降水蒸散指数(SPEI), 干湿变化, 干旱, 降水集中度(PCD), 降水集中期(PCP), 秦岭

Abstract: The values of SPEI(Standardized Precipitation Evapotranspiration Index),PCD(Precipitation-Concentration Degree),and PCP(Precipitation-Concentration Period)were calculated separately based on the metrological dataset derived from China Meteorological Data Sharing Service System.The dryness/wetness characters,precipitation heterogeneity and their relationship in the study area were analyzed using the Hurst Index,Mann-Kendall test and Morlet Wavelet analysis.The results are as follows: ① Climate in the study area was inclined to dryness in recent 55 years,and this trend was especially significant since 1995.Furthermore,the Hurst Index indicated that such dryness would persist for several years,and the persistence intensity in the north was stronger than that in the south of the Qinling Mountains.Spatially,the general climate was in a pattern of “moist in the south and dry in the north”;② The PCD in the study area was significantly increased,the spatial range of precipitation-concentration expanded from the west to the east during the period of 1960-2014,and the PCD in the south was higher than that in the north;③ There was a significant positive correlation between SPEI and PCD,and the correlation coefficient in the south was higher than that in the north of the Qinling Mountains.Whereas the correlation between SPEI and PCP was poor,and the correlation coefficient reached 0.3 only at 26% meteorological stations distributed mainly in the southeast;④ In the study areas,the higher the precipitation dispersion was,the more serious the drought would be.

Key words: SPEI, dryness/wetness variation, drought, PCD, PCP, the Qinling Mountains