Climatic Change

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
Expand
  • College of Tourism and Environmental Sciences,Shaanxi Normal University,Xi'an 710062,Shaanxi,China

Received date: 2015-08-25

  Revised date: 2015-11-14

  Online published: 2016-05-31

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.

Cite this article

LI Ying-jie , YAN Jun-ping , LIU Yong-lin . Relationship between Dryness/Wetness and Precipitation Heterogeneity in the North and South of the Qinling Mountains[J]. Arid Zone Research, 2016 , 33(3) : 619 -627 . DOI: 10.13866/j.azr.2016.03.23

References

〔1〕 卫捷,马柱国.Palmer 干旱指数、地表湿润指数与降水距平的比较〔J〕.地理学报,2003,58(增刊):117-124.〔Wei Jie,Ma Zhuguo.Comparison of Palmer drought severity index,percentage of precipitation anomaly and surface humid index〔J〕.Acta Geographica Sinica,2003,58(Suppl.):117-124.〕
〔2〕 McKee T B,Doesken N J,Kleist J.The Relationship of Drought Frequency and Duration to Time Scales〔M〕.USA,American Meteorological Society Boston,MA,1993:179-183.
〔3〕 张强,邹旭恺,肖风劲.气象干旱等级〔S〕.中华人民共和国国家标准.北京:中国标准出版社,2006:1-16.〔Zhang Qiang,Zou Xukai,Xiao Fengjin.Classification of Meteorological Drought〔S〕.Beijing:China Standards Press,2006:1-16.〕
〔4〕 邹旭恺,任国玉,张强.基于综合气象干旱指数的中国干旱变化趋势研究〔J〕.气候与环境研究,2010,15(4):371-378.〔Zou Xukai,Ren Guoyu,Zhang Qiang .Droughts variations in China based on a compound index of meteorological drought〔J〕.Climatic and Environmental Research,2010,15(4):371-378.〕
〔5〕 袁文平,周广胜.标准化降水指标与Z指数在我国应用的对比分析〔J〕.植物生态学报,2004,28(4):523-529.〔Yuan Wenping,Zhou Guangsheng.Comparison between standardized precipitation index and Z-index in China〔J〕.Acta Phytoecologica Sinica,2004,28(4):523-529.〕
〔6〕 王帅兵,李常斌,杨林山,等.基于标准化降水指数与Z指数的洮河流域干旱趋势分析〔J〕.干旱区研究,2015,32(3):565-572.〔Wang Shuaibing,Li Changbin,Yang Linshan,et al.Drought trend analysis based on standardized precipitation index and the Z index in the Tao River Basin〔J〕.Arid Zone Research,2015,32(3):565-572.〕
〔7〕 王玉娟,王树东,曾红娟,等.基于作物缺水指数法的渭河流域干旱特征〔J〕.干旱区研究,2014,31(1):118-124.〔Wang Yujuan,Wang Shudong,Zeng Hongjuan,et al.Drought characteristic in the Weihe River Basin based on water shortage index of crops〔J〕.Arid Zone Research,2014,31(1):118-124.〕
〔8〕 Abramopoulos F,Rosenzweig C,Choudhury B.Improved ground hydrology calculations for global climate models (GCMs):Soil water movement and evapotranspiration〔J〕.Journal of Climate,1988,1(9):921-941.
〔9〕 Vicente-Serrano S M,Beguería S,López-Moreno J I.A multiscalar drought index sensitive to global warming:the standardized precipitation evapotranspiration index〔J〕.Journal of Climate,2010,23(7):1 696-1 718.
〔10〕石崇,刘晓东.1947—2006 年东半球陆地干旱化特征——基于SPEI数据的分析〔J〕.中国沙漠,2012,32(6):1 691-1 701.〔Shi Chong,Liu Xiaodong.Continent drought characteristics over the Eastern Hemisphere from 1947 to 2006:Analyses based on the SPEI dataset〔J〕.Journal of Desert Research,2012,32(6):1 691-1 701.〕
〔11〕张岳军,郝智文,王雁,等.基于SPEI和SPI指数的太原多尺度干旱特征与气候指数的关系〔J〕.生态环境学报,2014,23(9):1 418-1 424.〔Zhang Yuejun,Hao Zhiwen,Wang Yan,et al.Multiscale characteristics of drought based on SPEI and SPI in association with climate index in Taiyuan〔J〕.Ecology and Environmental Sciences,2014,23 (9):1 418-1 424.〕
〔12〕王东,张勃,安美玲,等.基于SPEI的西南地区近53 a干旱时空特征分析〔J〕.自然资源学报,2014,29(6):1 003-1 016.〔Wang Dong,Zhang Bo,An Meiling,et al.Temporal and spatial distributions of drought in Southwest China over the past 53 years based on standardized precipitation evapotranspiration index〔J〕.Journal of Natural Resources,2014,29(6):1 003-1 016.〕
〔13〕刘永林,延军平,岑敏仪.中国降水非均匀性综合评价〔J〕.地理学报,2015,70(3):392-406.〔Liu Yonglin,Yan Junping,Cen Minyi.Comprehensive evaluation of precipitation heterogeneity in China〔J〕.Acta Geographica Sinica,2015,70(3):392-406.〕
〔14〕张录军.中国降水时空分布特征及其形成机制和对旱涝灾害影响的研究〔D〕.南京:南京大学,2004:251-269.〔Zhang Lujun.Distribution Features and Formation Mechanism of Annual Precipitation in China and Their Effects on Drought and Flood Hazard〔D〕.Nanjing:Nanjing University,2004:251-269.〕
〔15〕Zhang Lujun,Qian Yongfu.Annual distribution features of precipitation in China and their interannual variations 〔J〕.Journal of Meteorological Research,2003,17(2):146-163.
〔16〕莫申国,张百平.基于DEM的秦岭温度场模拟〔J〕.山地学报,2007,25(4):406-411.〔Mo Shenguo,Zhang Baiping.Simulation of temperature fields based on DEM in Qinling Mountains〔J〕.Journal of Mountain Science,2007,25(4):406-411.〕
〔17〕张立伟,宋春英,延军平.秦岭南北年极端气温的时空变化趋势研究〔J〕.地理科学,2011,31(8):1 007-1 011.〔Zhang Liwei,Song Chunying,Yan Junping.Spatio-temporal trends of annual extreme temperature in northern and southern Qinling Mountains〔J〕.Scientia Geographica Sinica,2011,31(8):1 007-1 011.〕
〔18〕李双双,杨赛霓,刘宪锋.1960—2013年秦岭-淮河南北极端降水时空变化特征及其影响因素〔J〕.地理科学进展,2015,34(3):354-363.〔Li Shuangshuang,Yang Saini,Liu Xianfeng.Spatiotemporal variability of extreme precipitation in north and south of the Qinling-Huaihe region and influencing factors during 1960-2013〔J〕.Progress in Geography,2015,34(3):354-363.〕
〔19〕宋春英,延军平,张立伟.陕西秦岭南北旱涝灾害时空变化趋势分析〔J〕.干旱区研究,2011,28(6):944-949.〔Song Chunying,Yan Junping,Zhang Liwei.Temporal and spatial trends of drought and flood in the south and north of the Qinling Mountains in Shaanxi Province〔J〕.Arid Zone Research,2011,28(6):944-949.〕
〔20〕李敏敏,延军平.全球变化下秦岭南北旱涝时空变化格局〔J〕.资源科学,2013,35(3):638-645.〔Li Minmin,Yan Junping.Drought and flood spatial and temporal variation in the Qinling Mountains〔J〕.Resources Science,2013,35(3):638-645.〕
〔21〕李双双,延军平,万佳.全球气候变化下秦岭南北气温变化特征〔J〕.地理科学,2012,32(7):853-858.〔Li Shuangshuang,Yan Junping,Wan Jia.The characteristics of temperature change in Qinling Mountains〔J〕.Scientia Geographica Sinica,2012,32(7):853-858.〕
〔22〕汪青春,李凤霞,刘宝康,等.近50 a来青海干旱变化及其对气候变暖的响应〔J〕.干旱区研究,2015,32(1):65-72.〔Wang Qingchun,Li Fengxia,Liu Baokang,et al.Variation in drought and its response to climate warming in Qinghai Plateau in recent 50 Years〔J〕.Arid Zone Research,2015,32(1):65-72.〕
〔23〕陈伏龙,王怡璇,吴泽斌,等.气候变化和人类活动对干旱区内陆河径流量的影响——以新疆玛纳斯河流域肯斯瓦特水文站为例〔J〕.干旱区研究,2015,32(4):692-697.〔Chen Fulong,Wang Yixuan,Wu Zebin,et al.Impacts of climate change and human activities on runoff of continental river in Arid areas:Taking kensiwate hydrological station in Xinjiang Manas River basin as an example〔J〕.Arid Zone Research,2015,32(4):692-697.〕
〔24〕蒋冲,王飞,刘焱序,等.秦岭南北风速时空变化及突变特征分析〔J〕.地理科学,2013,33(2):244-250.〔Jiang Chong,Wang Fei,Liu Yanxu,et al.Spatial-temporal variation and mutation of wind speed in the northern and southern regions of the Qinling Mountains〔J〕.Scientia Geographica Sinica,2013,33(2):244-250.〕
〔25〕万佳,延军平.秦岭南北生态地理界线对气候变化的响应〔J〕.干旱区资源与环境,2013,27(9):104-108.〔Wan Jia,Yan Junping.Interdecadal changes of eco-geographical boundaries in Qinling Mountains〔J〕.Journal of Arid Land Resources and Environment,2013,27(9):104-108.〕
〔26〕周丹,张勃,沈彦俊.潜在蒸散量估算方法对干旱侦测指数计算的影响〔J〕.中国农业气象,2014,35(3):258-267.〔Zhou Dan,Zhang Bo,Shen Yanjun.Effect of potential evapotranspiration estimation method on reconnaissance drought index(RDI) calculation〔J〕.Chinese Journal of Agrometeorology,2014,35(3):258-267.〕
〔27〕王米雪,延军平,李双双.1960—2013年中国东南沿海地区旱涝时空变化特征及其趋势分析〔J〕.资源科学,2014,36(11):2 307-2 315.〔Wang Mixue,Yan Junping,Li Shuangshuang.Spatial-temporal variation and the tendency of droughts and floods on the southeast coast of China over 54 years〔J〕.Resources Science,2014,36(11):2 307-2 315.〕
〔28〕刘珂,姜大膀.基于两种潜在蒸散发算法的SPEI对中国干湿变化的分析〔J〕.大气科学,2015,39(1):23-36.〔Liu Ke,Jiang Dabang.Analysis of dryness/wetness over China using standardized precipitation evapotranspiration index based on two evapotranspiration algorithms〔J〕.Chinese Journal of Atmospheric Sciences,2015,39(1):23-36.〕
〔29〕张录军,钱永甫.长江流域汛期降水集中程度和洪涝关系研究〔J〕.地球物理学报,2004,47(4):622-630.〔Zhang Lujun,Qian Yongfu.A study on the feature of precipitation concentration and its relation to floods producing in the Yangtze River Valley of China〔J〕.Chinese Journal of Geophysics,2004,47(4):622-630.〕
〔30〕Łabędzki L.Estimation of local drought frequency in central Poland using the standardized precipitation index SPI〔J〕.Irrigation and Drainage,2007,56(1):67-77.
〔31〕冯新灵,冯自立,罗隆诚,等.青藏高原冷暖气候变化趋势的 R/S 分析及 Hurst 指数试验研究〔J〕.干旱区地理,2008,31(2):175-181.〔Feng Xinling,Feng Zili,Luo Longcheng,et al.Fractal analysis of climate change and Hurst Index experiment in Tibetan Plateau in future〔J〕.Arid Land Geography,2008,31(2):175-181.〕
〔32〕赵晶,王乃昂.近 50 年来兰州城市气候变化的 R/S 分析〔J〕.干旱区地理,2002,25(1):90-95.〔Zhao Jing,Wang Nai'ang.R/S analysis of urbanization effect on climate in lanzhou〔J〕.Arid Land Geography,2002,25(1):90-95.〕
〔33〕李慧,王位泰.西北地区夏季降水的气候特征分析〔J〕.中国农业气象,2005,26(3):158-160,204.〔Li Hui,Wang Weitai.Analysis of climate character of summer precipitation in Northwest China〔J〕.Chinese Journal of Agrometeorology,2005,26(3):158-160,204.〕
〔34〕孙卫国,程炳岩,郭渠.东亚季风环流对华北地区降水蒸发差的影响〔J〕.中国农业气象,2009,30(3):327-334.〔Sun Weiguo,Cheng Bingyan,Guo Qu.Influence of east asian monsoon circulation on precipitation-evaporation difference in North China〔J〕.Chinese Journal of Agrometeorology,2009,30(3):327-334.〕
〔35〕赵平,周自江.东亚副热带夏季风指数及其与降水的关系〔J〕.气象学报,2005,63(6):933-941.〔Zhao Ping,Zhou Zijiang.East asian subtropical summer monsoon index and its relationships to rainfall〔J〕.Acta Meteorologica Sinica,2005,63(6):933-941.〕
〔36〕张强,张杰,孙国武,等.祁连山山区空中水汽分布特征研究〔J〕.气象学报,2007,65(4):633-643.〔Zhang Qiang,Zhang Jie,Sun Guowu,et al.Research on atmospheric water-vapor distribution over Qilianshan mountains〔J〕.Acta Meteorologica Sinica,2007,65(4):633-643.〕
〔37〕张良,张强,冯建英,等.祁连山地区大气水循环研究I.空中水汽输送年际变化分析〔J〕.冰川冻土,2014,36(5):1 079-1 091.〔Zhang Liang,Zhang Qiang,Feng Jianying,et al.A study of atmospheric water cycle over the Qilian Mountains I.Variation of annual water vaportransport〔J〕.Journal of Glaciology and Geocryology,2014,36(5):1 079 -1 091.〕
Outlines

/