滹沱河流域植被覆盖时空演变及其与SPEI的相关关系
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Spatial-temporal change of vegetation cover and its relationship with SPEI in Hutuo river basin
  • 作者:李镇 ; 齐菲 ; 尙国琲 ; 孙雷刚 ; 夏玉杰
  • 英文作者:LI Zhen;QI Fei;SHANG Guofei;SUN Leigang;XIA Yujie;School of Land Resources and Urban and Rural Planning,Hebei GEO University;Institute of Geographical Sciences,Hebei Academy of Sciences;
  • 关键词:中分辨率成像光谱仪-归一化植被指数 ; 时空演变 ; SPEI ; 相关分析 ; 滹沱河流域
  • 英文关键词:MODIS NDVI;;Spatial-temporal change;;SPEI;;Correlation analysis;;Hutuo river basin
  • 中文刊名:NSBD
  • 英文刊名:South-to-North Water Transfers and Water Science & Technology
  • 机构:河北地质大学土地资源与城乡规划学院;河北省科学院地理科学研究所;
  • 出版日期:2018-01-08 10:20
  • 出版单位:南水北调与水利科技
  • 年:2018
  • 期:v.16;No.94
  • 基金:河北省水利科研与推广计划项目(2016-71);; 河北地质大学博士科研基金项目(BQ201605)~~
  • 语种:中文;
  • 页:NSBD201801023
  • 页数:9
  • CN:01
  • ISSN:13-1334/TV
  • 分类号:151-159
摘要
选择2001-2015年MODIS NDVI(250m)及14个气象站点气温、降水数据,通过计算标准化降水蒸散指数(SPEI),探究滹沱河流域近15年植被覆盖时空演变特征,分别从月、季节、年等尺度探究植被覆盖与SPEI的相关关系。结果显示:(1)近15年滹沱河流域归一化植被指数(NDVI)呈显著增加趋势,增速为0.024/(10a)。(2)植被恢复以明显改善为主,覆盖范围占整个流域面积的51.58%,主要分布于流域中、上游。(3)滹沱河流域SPEI总体上呈波动上升趋势,干旱程度有所降低,流域中游变湿趋势最显著。(4)6月、7月是干旱条件对植被覆盖影响最显著的月份,其中,6月气温对NDVI的影响大于降水,而7月降水对NDVI的影响大于气温;夏季干旱程度对植被覆盖度的影响最为明显;NDVI年际变化与SPEI具有显著正相关关系,干旱对植被生长状态有较大影响。
        Spatial-temporal change of coverage is in favor of understanding the ecosystem response to climatic variability and human-induced land transformations.The objective of this study was to analysis vegetation dynamics its relationship with drought in Hutuo river basin,based on 250 m MODIS NDVI time-series data and monthly temperature and precipitation of 14 meteorological stations(2001-2015).The characteristics of drought were studied using the drought index(standardized precipitation evapotranspiration index,SPEI),and the monthly temperature and precipitation were used to compute the SPEI of 1,3 and 12 month timescale.Results are shown as follows:(1)The NDVI of the study area was improvement progressively from 2001 to2015,with a linear tendency being 0.024/(10 a).(2)The largest proportion of the contribution to vegetation restoration was observed in the significantly improved area,and the area where the values of NDVI significantly increased accounts for reached 51.58% was mainly located in the upstream and midstream of Hutuo river basin.(3)The SPEI was fluctuating upward trend,which indicated that drought could be easing over the past 15 years in Hutuo river basin.And the trend was most marked in the midstream.(4)Correlation analysis results showed that the SPEI had a strong influence on vegetation coverage mainly occurred in June and July on the monthly,and temperature was the dominant factor affecting the change of vegetation in June,while precipitation was the dominant factor in July.Seasonally,drought in summer had more influence on vegetation coverage.There was a positive correlation between the annual NDVI and annual SPEI,and drought has a great influence on vegetation growth.
引文
[1]朴世龙,方精云.1982-1999年我国陆地植被活动对气候变化响应的季节差异[J].地理学报,2003,58(1):119-125.(PIAO S L,FANG J Y.Seasonal changes in vegetation activity in response to climate changes in China between 1982and 1999[J].Acta Geographica Sinica,2003,58(1):119-125.(in Chinese))
    [2]胡婵娟,郭雷.植被恢复的生态效应研究进展[J].生态环境学报,2012,21(9):1640-1646.(HU C J,GUO L.Advances in the research of ecological effects of vegetation restoration[J].Ecology and Environmental Sciences,2012,21(9):1640-1646.(in Chinese))DOI:10.16258/j.cnki.1674-5906.2012.09.007.
    [3]赵健赟,彭军.基于MODIS NDVI的青海高原植被覆盖时空变化特征分析[J].干旱区资源与环境,2016,30(4):67-73.(ZHAO J Y,PENG J.Spatiotemporal variation of the vegetation coverage in Qinghai Plateau based on MODIS NDVI data[J].Journal of Arid Land Resources and Environment,2016,30(4):67-73.(in Chinese))DOI:10.13448/j.cnki.jalre.2016.115.
    [4]李双双,延军平,万佳.近10年陕甘宁黄土高原区植被覆盖时空变化特征[J].地理学报,2012,(37)7:960-970.(LI S S,YAN J P,WAN J.The spatial-temporal changes of vegetation restoration on Loess Plateau in Shaanxi-Gansu-Ningxia region[J].Acta Geographica Sinica,2012,(37)7:960-970.(in Chinese))
    [5]赵舒怡,宫兆宁,刘旭颖.2001-2013年华北地区植被覆盖度与干旱条件的相关分析[J].地理学报,2015,70(5):717-729.(ZHAO S Y,GONG Z N,LIU X Y.Correlation analysis between vegetation coverage and climate drought conditions in North China during 2001-2013[J].Acta Geographica Sinica,2015,70(5):717-729.(in Chinese))DOI:10.11821/dlxb201505004.
    [6]中国国家气象局.气象干旱等级国家标准GB/T20481-2006[S].北京:中国标准出版社,2006.(The China meteorological administration.The national standard of the Classification of Meteorological Drought GB/T20481-2006[S].Beijing:China Standards Press,2006.(in Chinese))
    [7]张强,姚玉璧,李耀辉,等.中国西北地区干旱气象灾害监测预警与减灾技术研究进展及其展望[J].地球科学进展,2015,30(2):196-213.(ZHANG Q,YAO Y B,LI Y H,et al.Research progress and prospect on the monitoring and early warning and mitigation technology of meteorological drought disaster in northwest China[J].Advances in Earth Science,2015,30(2):196-213.(in Chinese))DOI:10.11867/j.issn.1001-8166.2015.02.0196.
    [8]王兆礼,黄泽勤,李军,等.基于SPEI和NDVI的中国流域尺度气象干旱及植被分布时空演变[J].农业工程学报,2016,32(14):177-186.(WANG Z L,HUANG Z Q,LI J,et al.Assessing impacts of meteorological drought on vegetation at catchment scale in China based on SPEI and NDVI[J].Transactions of the Chinese Society of Agricultural Engineering(Transactions of the CSAE),2016,32(14):177-186.(in Chinese))DOI:10.11975/j.issn.1002-6819.2016.14.0187.
    [9]阿多,赵文吉,宫兆宁,等.1981—2013华北平原气候时空变化及其对植被覆盖度的影响[J].生态学报,2017,37(2):1-17.(A D,ZHAO W J,GONG Z N,et al.Temporal analysis of climate change and its relationship with vegetation cover on the north china plain from 1981to 2013[J].Acta Ecologica Sinica,2017,37(2):576-592.(in Chinese))DOI:10.5846/stxb201507301600.
    [10]PARUELO J M,EPSTEIN H E,LAUENROTH W K,et al.A NPP estimates from NDVI for the central grassland region of the United States[J].Ecology,1997,78(3):953-958.
    [11]武正丽,贾文雄,刘亚荣,等.近10a来祁连山植被覆盖变化研究[J].干旱区研究,2014,31(1):80-87.(WU Z L,JIA W X,LIU Y R,et al.Change of vegetation coverage in the Qilian Mountains in recent 10years[J].Arid Zone Research,2014,31(1):80-87.(in Chinese))DOI:10.13866/j.azr.2014.01.023.
    [12]ECKERT S,HSLER F,LINIGER H,et al.Trend analysis of MODIS NDVI time series for detecting land degradation and regeneration in Mongolia[J].Journal of Arid Environments,2015,113:16-28.DOI:10.1016/j.jaridenv.2014.09.001.
    [13]SHAO Y,LUNETTA R S,WHEELER B,et al.An evaluation of time-series smoothing algorithms for land-cover classifications using MODIS-NDVI multi-temporal data[J].Remote Sensing of Environment,2016,174:258-265.DOI:10.1016/j.rse.2015.12.023
    [14]ZHAO Maosheng,RUNNING S W.Drought-induced reduction in global terrestrial net primary production from 2000through 2009[J].science,2010,329(5994):940-943.DOI:10.1126/science.1199544.
    [15]丁文荣.金沙江下段植被NDVI变化趋势及其归因[J].南水北调与水利科技,2017,15(1):107-112.(DING W R.Study on the relationship between change trend of NDVI and environment factors in the lower section of Jinsha River,China[J].South-to-North Water Transfers and Water Science&Technology,2017,15(1):107-112.(in Chinese))DOI:10.13476/j.cnki.nsbdqk.2017.01.018.
    [16]赵新来,李文龙,Guo Xulin,等.Pa、SPI和SPEI干旱指数对青藏高原东部高寒草地干旱的响应比较[J].草业科学,2017,34(2):273-282.(ZHAO X L,LI W L,GUO X L,et al.The responses of Pa,SPI and SPEI to dry climate in alpine meadows of eastern Qinghai-Tibet Plateau[J].Pratacultural Science,2017,34(2):273-282.(in Chinese))DOI:10.11829/j.issn.1001-0629.2016-0187.
    [17]江姗珊,张增信,王玮琳,等.植被动态演变规律及其与极端气候事件的关系[J].南京林业大学学报(自然科学版),2016,40(5):74-80.(JIANG S S,ZHANG Z X,WANG W L,et al.Dynamic variation rules of vegetation cover in Jiangsu Province and its response to climate change[J].Journal of Nanjing Forestry University(Natural Sciences Edition),2016,40(5):74-80.(in Chinese))DOI:10.3969/j.issn.1000-2006.2016.05.012.
    [18]VICENTE-SERRANO S M,GOUVEIA C,CAMARERO J J,et al.Response of vegetation to drought time-scales across global land biomes[J].Proceedings of the National Academy of Sciences of the United States of America,2013,110(1):52-57.DOI:10.1073/pnas.1207068110.
    [19]张艳芳,吴春玲,张宏运,等.黄河源区植被指数与干旱指数时空变化特征[J].山地学报,2017,35(02):142-150.(ZHANG Y F,WU C L,ZHANG H Y,et al.Dependency relationship between NDVI and SPEI for spatial-temporal variations in the source areas of the Yellow River.(in Chinese))DOI:10.16089/j.cnki.1008-2786.000206.
    [20]孔冬冬,张强,顾西辉,等.植被对不同时间尺度干旱事件的响应特征及成因分析[J].生态学报,2016,36(24):7908-7918.(KONG D D,ZHANG Q,GU X H,et al.Vegetation responses to drought at different time scales in China[J].Acta Ecologica Sinica,2016,36(24):7908-7918.(in Chinese))DOI:10.5846/stxb201506111182.
    [21]VICENTE-SERRANO S M,BEGUER?A S,L?PEZMORENO J I.A multi-scalar drought index sensitive to global warming:The standardized precipitation evapotranspiration index[J].Journal of Climate,2010,23:1696-1718.DOI:10.1175/2009JCLI2909.1.
    [22]VICENTE-SERRANO S M,L?PEZ-MORENO J I,LORENZO-LACRUZ J,et al.The NAO impact on droughts in the mediterranean region[J].Advances in Global Change Research,2011,46:23-40.
    [23]周丹,张勃,任培贵,等.基于标准化降水蒸散指数的陕西省近50a干旱特征分析[J].自然资源学报,2014,29(4):677-688.(ZHOU D,ZHANG B,REN P G,et al.Analysis of Drought Characteristics of Shaanxi Province in Recent 50Years Based on Standardized Precipitation Evapotranspiration Index[J].Journal of Natural Resources,2014,29(4):677-688.(in Chinese))
    [24]张瑞钢,莫兴国,林忠辉.滹沱河上游山区近50年蒸散变化及主要影响因子分析[J].地理学报,2012,32(5):628-634.(ZHANG R G,MO X G,LIN Z H,et al.The trend and the principal influence factors of evapotranspiration in Hutuo river basin during last 50years[J].Acta Geographica Sinica,2012,32(5):628-634.(in Chinese))
    [25]宋保平,过仲阳,郑艳侠,等.近50年来滹沱河流域水资源变化规律与影响因素[J].南水北调与水利科技,2013,11(4):17-21.(SONG B P,GUO Z Y,ZHENG Y X,et al.Variation characteristics and their impact factors of water resources in the Hutuo river basin during 50years[J].?South-to-North Water Transfers and Water Science&Technology,2013,11(4):17-21.(in Chinese))DOI:10.3724/SP.J.1201.2013.04017.
    [26]孙雷刚,郑振华.基于RS的近30年滹沱河流域植被覆盖度动态变化研究[J].地理与地理信息科学,2014,30(6):36-60,45.(SUN L G,ZHENG Z H.RS-based study on dynamic change of vegetation coverage in Hutuo river watershed in the past 30years[J].Geography and Geo-information Science,2014,30(6):36-60,45.(in Chinese))DOI:10.3969/j.issn.1672-0504.2014.06.008.
    [27]张金屯.五台山植被类型及分布[J].山西大学学报,1986,(2):87-91.(ZHANG J T.The vegetation types and their distribution on Wutai mountains in Shanxi province[J].Learned Periodical Society Shanxi University,1986,(2):87-91.(in Chinese))
    [28]HOLBEN B N.Characteristics of maximum-value composite images from temporal AVHRR data[J].International Journal of Remote Sensing,1986,7(11):1471-1434.
    [29]何远梅,姚文俊,张岩,等.黄土高原区植被恢复的空间差异性分析[J].中国水土保持科学,2015,13(2):63-69.(HE Y M,YAO W J,ZHANG Y,et al.Spatial variability of vegetation restoration on the Loess Plateau based on MODIS/NDVI[J].Science of Soil and Water Conservation,2015,13(2):63-69.(in Chinese))DOI:10.16843/j.sswc.2015.02.011.
    [30]王永财,孙艳玲,王中良.1998-2011年海河流域植被覆盖变化及气候因子驱动分析[J].资源科学,2014,36(3):594-602.(WANG Y C,SUN Y L,WANG Z L.Spatial-temporal change in vegetation cover and climate factor drivers of variation in the Haihe River Basin 1998-2011[J].Resources Science,2014,36(3):594-602.(in Chinese))
    [31]赵安周,刘宪锋,朱秀芳,等.2000-2014年黄土高原植被覆盖时空变化特征及其归因[J].中国环境科学,2016,36(5):1568-1578.(ZHAO A Z,LIU X F,ZHU X F,et al.Spatiotemporal analyses and associated driving forces of vegetation coverage change in the Loess Plateau[J].China Environmental Science,2016,36(5):1568-1578.(in Chinese))DOI:10.3969/j.issn.1000-6923.2016.05.043.
    [32]穆少杰,李建龙,陈奕兆,等.2001-2010年内蒙古植被覆盖度时空变化特征[J].地理学报,2012,67(9):1255-1268.(MU S J,LI J L,CHEN Y Z,et al.Spatial differences of variations of vegetation coverage in Inner Mongolia during 2001-2010[J].Acta Geographica Sinica,2012,67(9):1255-1268.(in Chinese))
    [33]白建军,白江涛,王磊.2000~2010年陕北地区植被NDVI时空变化及其与区域气候的关系[J].地理科学,2014,34(7):882-888.(BAI J J,BAI J T,WANG L.Spatio-temporal change of vegetation NDVI and its relations with regional climate in Northern Shaanxi Province in 2000-2010[J].Scientia Geographica Sinica,2014,34(7):882-888.(in Chinese))
    [34]刘斌,孙艳玲,王中良,等.华北地区植被覆盖变化及其影响因子的相对作用分析[J].自然资源学报,2015,30(1):12-23.(LIU B,SUN Y L,WANG Z L,et al.Analysis of the vegetation cover change and the relative role of its influencing factors in North China[J].Journal of Natural Resources,2015,30(1):12-23.(in Chinese))DOI:10.11849/zrzyxb.2015.01.002.
    [35]仝莉棉,曾彪,王鑫.2000-2012年山西省不同植被类型物候变化及其对气候变化的响应[J].水土保持研究,2016,23(02):194-200.TONG L M,ZENG B,WANG X.Phenological variation of different vegetation types and its responds to climate changes in shanxi province from 2000to 2012[J].Research of soil and water conservation,2012,67(9):1255-1268.(in Chinese))DOI:10.13869/j.cnki.rswc.2016.02.037.
    [36]穆少杰,李建龙,周伟,等.2001—2010年内蒙古植被净初级生产力的时空格局及其与气候的关系[J].生态学报,2013,33(12):3752-3764.MU S J,LI J L,ZHOU W,et al.Spatial-temporal distribution of net primary productivity and its relationship with climate factors in Inner Mongolia from 2001to 2010[J].Acta Ecologica Sinic,2013,33(12):3752-3764.(in Chinese))DOI:10.5846/stxb201205030638.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700