黄土高原昼夜不对称性增温及其对植被NDVI的影响
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  • 英文篇名:Diurnal asymmetry of temperature and its effect on NDVI in Loess Plateau
  • 作者:马利群 ; 秦奋 ; 孙九林 ; 王浩 ; 夏浩铭
  • 英文作者:MA Liqun;QIN Fen;SUN Jiulin;WANG Hao;XIA Haoming;The College of Environment and Planning of Henan University;Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences;School of Civil Engineering and Architecture of Henan University;
  • 关键词:黄土高原 ; 生长季 ; 日最高气温 ; 夜最低气温 ; 不对称增温 ; NDVI ; 植被动态响应 ; 昼夜增温 ; 气候变暖
  • 英文关键词:Loess Plateau;;growing season;;maximum temperature;;minimum temperature;;asymmetric warming;;NDVI;;vegetation dynamics;;day and nighttime warming;;global warming
  • 中文刊名:ZRZY
  • 英文刊名:Resources Science
  • 机构:河南大学环境与规划学院;中国科学院地理科学与资源研究所;河南大学土木建筑学院;
  • 出版日期:2018-08-25
  • 出版单位:资源科学
  • 年:2018
  • 期:v.40
  • 基金:教育部基地重大项目(16JJD770019);; 河南省高等学校重点科研项目(18A170002);; 河南省高校科技创新团队支持计划(16IRTSTHN012)
  • 语种:中文;
  • 页:ZRZY201808017
  • 页数:9
  • CN:08
  • ISSN:11-3868/N
  • 分类号:192-200
摘要
本文选取1982—2015年黄土高原及周边地区102个气象站点的气象观测资料,结合归一化植被指数(NDVI)和植被类型数据,采用Mann-Kendall(M-K)非参数检验法和二阶偏相关分析法,分析了黄土高原植被生长季日最高气温(T_(max))和夜间最低气温(T_(min))的时间序列变化趋势和空间格局、并分植被类型探讨昼夜不对称性增温对植被的影响。研究表明:(1)1982—2015年间黄土高原植被生长季T_(max)及T_(min)都存在极为显著的上升趋势(P<0.01),植被生长季T_(min)的增温速率约为T_(max)增温速率的1.6倍,昼夜增温呈不对称性;(2)昼夜不对称性增温对植被动态的影响呈现明显的分异特征,植被生长季植被NDVI与T_(min)表现出比T_(max)更显著的相关性,即相对于白天增温,夜间增温的变化对黄土高原植被的影响程度更加显著;(3)不同植被类型的NDVI与昼夜增温的偏相关分析可知,除草原、农作物外其他植被类型均与T_(max)表现为显著偏正相关(P<0.05);不同植被类型与T_(min)的偏相关关系差异明显,农作物与T_(min)表现为显著偏负相关(P<0.01),其他植被类型与T_(min)均呈偏正相关性(P<0.05)。
        In this paper, the meteorological observation data of 102 meteorological stations in the Loess Plateau and its surrounding areas in 1982-2015 were selected. The Normalized Difference Vegetation Index(NDVI) and vegetation type data were used. And the Mann-kendall(m-k) Nonparametric test method and the second-order partial correlation analysis were adopted. The time series change trend and spatial pattern in the growing seasonal minimum temperature(T_(min)) and maximum temperature(T_(max)) over the Loess Plateau between 1982 and 2015 were analyzed, and the effects of asymmetric warming on different vegetation type were discussed. The results show that:(1)We found a persistent increase(P<0.01) in the growing seasonal T_(min) and T_(max) over the Loess Plateau between 1982-2015, whereas the rate of increase of T_(min) was 1.6 times that of T_(max).(2)The influence of diurnal asymmetry on vegetation dynamics showed an obvious difference, and NDVI and T_(min) showed a more significant correlation than NDVI and T_(max) in vegetative growth season. The effect of nighttime warming on NDVI in the Loess plateau is more significant than that of daytime warming.(3) We also found diverse responses of vegetation type to daytime and night-time warming across the Loess Plateau. We found that the partial correlation between NDVI and T_(max) was positive(P<0.05) except grassland and crop. The partial correlation between T_(min) and NDVI of crop was negative(P<0.01), and the partial correlation between T_(min) and NDVI of other vegetation was positive(P<0.05). Our results provide a demonstration for studying regional responses of vegetation to climate extremes under global climate change.
引文
[1]易浪,任志远,张翀,等.黄土高原植被覆盖变化与气候和人类活动的关系[J].资源科学,2014,36(1):166-174.[Yi L,Ren ZY,Zhang C,et al.Vegetation cover,climate and human activities on the Loess Plateau[J].Resources Science,2014,36(1):166-174.]
    [2]夏浩铭,李爱农,赵伟,等.2001-2010年秦岭森林物候时空变化遥感监测[J].地理科学进展,2015,34(10):1297-1305.[Xia H M,Li A N,Zhao W,et al.Spatiotemporal variations of forest phenology in the Qinling zone based on remote sensing monitoring,2001-2010[J].Progress in Geography,2015,34(10):1297-1305.]
    [3]Cong N,Shen M,Yang W,et al.Varying responses of vegetation activity to climate changes on the Tibetan Plateau grassland[J].International Journal of Biometeorology,2017,61(8):1433-1444.
    [4]He B,Chen A,Jiang W,et al.The response of vegetation growth to shifts in trend of temperature in China[J].Journal of Geographical Sciences,2017,27(7):801-816.
    [5]Kong D D,Zhang Q,Singh V P,et al.Seasonal vegetation response to climate change in the Northern Hemisphere(1982-2013)[J].Global and Planetary Change,2017,148:1-8.
    [6]Zhang B,Cui L,Shi J,et al.Vegetation dynamics and their response to climatic variability in China[J].Advances in Meteorology,2017,(14)1-10.
    [7]陈云浩,李晓兵,史培军.1983~1992年中国陆地NDVI变化的气候因子驱动分析[J].植物生态学报,2001,25(6):716-720.[Chen Y H,Li X B,Shi P J.Variation in NDVI driven by climate factors across China,1983-1992[J].Acta Phytoecologica Sinica,2001,25(6):716-720.]
    [8]李本纲,陶澍.AVHRR NDVI与气候因子的相关分析[J].生态学报,2000,20(5):898-902.[Li B G,Tao S.Correlation between AVHRR NDVI and climate factors[J].Acta Ecologica Sinica,2000,20(5):898-902.]
    [9]付新峰,杨胜天,刘昌明.雅鲁藏布江流域NDVI变化与主要气候因子的关系[J].地理研究,2007,26(1):60-65.[Fu X F,Yang S T,Liu C M.Changes of NDVI and their relations with principal climatic factors in the Yarlung Zangbo River Basin[J].Geographical Research,2007,26(1):60-65.]
    [10]李晓兵,史培军.中国典型植被类型NDVI动态变化与气温、降水变化的敏感性分析[J].植物生态学报,2000,24(3):379-382.[Li X B,Shi P J.Sensitivity analysis of variation in NDVI temperature and precipitation in typical vegetation types across China[J].Acta Phytoecologica Sinica,2000,24(3):379-382.]
    [11]Li J,Lewis J,Rowland J,et al.Evaluation of land performance in Senegal using multi-temporal NDVI and rainfall series[J].Journal of Arid Environments,2004,59(3):463-480.
    [12]张翀,任志远,韦振锋.近12年来黄土高原植被覆盖对年内水热条件的响应[J].资源科学,2013,35(10):2017-2023.[Zhang C,Ren Z Y,Wei Z F.Vegetation responses to intra-annual hydrothermal conditions on the loess plateau[J].Resources Science,2013,35(10):2017-2023.]
    [13]苏虹.黄土高原地区植被覆盖变化及其原因分析[D].呼和浩特:内蒙古师范大学,2016.[Su H.Analysis of Vegetation Dynamics and Its Causes of Loess Plateau[D].Hohhot:Inner Mongolia Normal University,2016.]
    [14]王学春,李军,王红妮,等.黄土高原冬小麦田土壤水分与小麦产量对降水和气温变化响应的模拟研究[J].自然资源学报,2017,32(8):1398-1410.[Wang X C,Li J,Wang H N,et al.Simulation of the response of soil water in winter wheat field and winter wheat yield to rainfall and temperature change on the loess plateau[J].Journal of Natural Resources,2017,32(8):1398-1410.]
    [15]何远梅.黄土髙原植被覆盖变化与区域气候变化的相互效应[D].北京:北京林业大学2015.[He Y M.Interaction between Vegetation Cover and Region Climate on the Loess Plateau[D].Beijing:Beijing Forestry University,2015.]
    [16]Stocker T F,Qin G K,Plattner M,et al.The Working Group I Contribution to the IPCC’s Fifth Assessment Report[R].Cambridge:2013 Climate Change the Physical Science Basis,2013.
    [17]Ji F,Wu Z,Huang J,et al.Evolution of land surface air temperature trend[J].Nature Climate Change,2014,4(6):462-466.
    [18]Pepin N C,Seidel D J.A global comparison of surface and free-air Journal of Geophysical Research Atmospheres,2005,110(D3):1-15.
    [19]Harvey L D D,Warm days,hot nights[J].Nature,1995,377(6544):15-16.
    [20]Peng S,Piao S,Ciais P,et al.Asymmetric effects of daytime and night-time warming on Northern Hemisphere vegetation[J].Nature,2013,501(7465):88-92.
    [21]Xia H M,Li A N,Feng G,et al.The effects of asymmetric diurnal warming on vegetation growth of the Tibetan Plateau over the past three decades[J].Sustainability,2018,10(4):1-14.
    [22]Ju H,Velde M,Lin E,et al.The impacts of climate change on agricultural production systems in China[J].Climatic Change,2013,120(1):313-324.
    [23]王丹,乔匀周,董宝娣,等.昼夜不对称性与对称性升温对大豆产量和水分利用的影响[J].植物生态学报,2016,40(8):827-833.[Wang D,Qiao Y Z,Dong B D,et al.Differential effects of diurnal asymmetric and symmetric warming on yield and water utilization of soybean[J].Chinese Journal of Plant Ecology,2016,40(8):827-833.]
    [24]江晓东,刘诚,徐家平,等.昼夜不对称增温对冬小麦花后冠层反射光谱特性的影响[J].农业工程学报,2014,30(12):115-122.[Jiang X D,Liu C,Xu J P,et al.Effects of asymmetric warming in daytime and nighttime on canopy spectral reflectance of post-anthesis winter wheat[J].Transactions of the Chinese Society of Agricultural Engineering,2014,30(12):115-122.]
    [25]江晓东,苏海报,王晓梅,等.昼夜不对称增温对麦田土壤水分的影响[J].灌溉排水学报,2014,33(4-5):283-286.[Jiang X D,Su H B,Wang X M,et al.Effect of asymmetric between day and night warming on soil moisture in wheat field[J].Journal of Irrigation and Drainage,2014,33(4-5):283-286.]
    [26]田云录,陈金,邓艾兴,等.开放式增温下非对称性增温对冬小麦生长特征及产量构成的影响[J].应用生态学报,2011,22(3):681-686.[Tian Y L,Chen J,Deng A X,et al.Effects of asymmetric warming on the growth characteristics and yield components of winter wheat under free air temperature increased[J].Chinese Journal of Applied Ecology,2011,22(3):681-686.]
    [27]董文军,邓艾兴,张彬,等.开放式昼夜不同增温对单季稻影响的试验研究[J].生态学报,2011,31(8):2169-2177.[Dong W J,Deng A X,Zhang B,et al.An experimental study on the effects of different diurnal warming regimes on single cropping rice with Free Air Temperature Increased(FATI)facility[J].Acta Ecologica Sinica,2011,31(8):2169-2177.]
    [28]张谦.中国北方典型草原水分利用效率对昼夜不对称性增温的特异性响应[D].开封:河南大学,2013.[Zhang Q.The Effects of Day and Night Warming on Water-Use Efficiency in a Typical Steppe in Northern China[D].Kaifeng:Henan University,2013.]
    [29]Wan S,Xia J,Liu W,et al.Photosynthetic overcompensation under nocturnal warming enhances grassland carbon sequestration[J].Ecology,2009,90(10):2700-2710.
    [30]赵杰,刘雪佳,杜自强,等.昼夜增温速率的不对称性对新疆地区植被动态的影响[J].中国环境科学,2017,37(6):2316-2321.[Zhao J,Liu X J,Du Z Q,et al.Effects of the asymmetric diurnalwarming on vegetation dynamics in Xinjiang[J].China Environmental Science,2017,37(6):2316-2321.]
    [31]梁春玲,于泉洲,刘煜杰,等.昼夜增温对南四湖湿地植被NDVI的影响差异[J].热带地理,2015,35(3):422-426.[Liang C L,Yu Q Z,Liu Y J,et al.Effects of air temperature circadian on the ND-VI of Nansi Lake wetland vegetation[J].Tropical Geography,2015,35(3):422-426.]
    [32]晏利斌.1961-2014年黄土高原气温和降水变化趋势[J].地球环境学报,2015,6(5):276-282.[Yan L B.Characteristics of temperature and precipitation on the Loess Plateau from 1961 to 2014[J].Journal of Earth Environment,2015,6(5):276-282.]
    [33]张翀,任志远.黄土高原地区植被覆盖变化的时空差异及未来趋势[J].资源科学,2011,33(11):2143-2149.[Zhang C,Ren ZY.Temporal and spatial differences and its trends in vegetation cover change over the loess plateau[J].Resources Science,2011,33(11):2143-2149.]
    [34]钟莉娜,赵文武.基于NDVI的黄土高原植被覆盖变化特征分析[J].中国水土保持科学,2013,11(5):57-62.[Zhong L N,Zhao W W.Detecting the dynamic changes of vegetation coverage in the Loess Plateau of China using NDVI data[J].Science of Soil and Water Conservation,2013,11(5):57-62.]
    [35]中国气象科学数据共享服务网.中国地面气象站逐小时观测资料[EB/OL].(2017-11-20)[2018-04-21].http://data.cma.cn/data/detail/Data Code/A.0012.0001.html.[China Meteorological Data Service Center.Hourly Observation Data from China Ground Weather Station[EB/OL].(2017-11-20)[2018-04-21].http://data.cma.cn/data/detail/Data Code/A.0012.0001.html.
    [36]张含玉,方怒放,史志华.黄土高原植被覆盖时空变化及其对气候因子的响应[J].生态学报,2016,36(13):3960-3968.[Zhang H Y,Fang N F,Shi Z H.Spatio-temporal patterns for the NDVIand its responses to climatic factors in the Loess Plateau,China[J].Acta Ecologica Sinica,2016,36(13):3960-3968.]
    [37]Nemani R,Votava P,Michaelis A,et al.Global Inventor Modeling and Mapping Studies,GIMMS[EB/OL].(2016-03-04)[2017-10-20].https://ecocast.arc.nasa.gov/data/pub/gimms.
    [38]中科院资源环境科学数据中心.资源环境数据云平台[EB/OL].(2017-11-22)[2018-04-21].http://www.resdc.cn.[Data Center for Resources and Environmental Sciences,Chinese Academy of Sciences(RESDC).Resource and Environment Data Cloud Platform[EB/OL].(2017-11-22)[2018-04-21].http://www.resdc.cn.]
    [39]Mann H B.Non-parametric tests against trend[J].Econometrics,1945,12(2):245-249.
    [40]Kendall M G.Rank correlation methods[J].British Journal of Psychology,1955,25(1):86-91.
    [41]Zar J H.Significance testing of the Spearman rank correlation coefficient[J].Journal of the American Statistical Association,1972,67(339):578-580.
    [42]Mahajan D R,Dodamani B M.Trend analysis of drought events over upper Krishna basin in Maharashtra[J].Aquatic Procedia,2015,4:1250-1257.
    [43]Kisi O,Ay M.Comparison of Mann-Kendall and innovative trend method for water quality parameters of the Kizilirmak River,Turkey[J].Journal of Hydrology,2014,513(5):362-375.
    [44]Cleophas T J,Zwinderman A H.Partial Correlations[A].Cleophas T J,Zwinderman A H.Regression Analysis in Medical Research[M].Cham:Springer International Publishing,2018.
    [45]赵安周,刘宪锋,朱秀芳,等.1965-2013年黄土高原地区极端气温趋势变化及空间差异[J].地理研究,2016,35(4):639-652.[Zhao A Z,Liu X F,Zhu X F,et al.Trend variations and spatial difference of extreme air temperature events in the Loess Plateau from 1965 to 2013[J].Geographical Research,2016,35(4):639-652.]
    [46]Tan J G,Piao S L,Chen A,et al.Seasonally different response of photosynthetic activity to daytime and night-time warming in the Northern Hemisphere[J].Global Change Biology,2015,21(1):377-387.
    [47]Atkin O K,Turnbull M H,Zaragoza-Castells J,et al.Light inhibition of leaf respiration as soil fertility declines along a post-glacial chronosequence in New Zealand:an analysis using the Kok method[J].Plant and Soil,2013,367(1):163-182.
    [48]Hobbie S E.Temperature and plant species control over litter decomposition in Alaskan Tundra[J].Ecological Monographs,1996,66(4):503-522.
    [49]信忠保,许炯心.黄土高原地区植被覆盖时空演变对气候的响应[J].自然科学进展,2007,17(6):770-778.[Xin Z B,Xu J X.Response of spatial-temporal evolution of vegetation cover to climate in the loess plateau[J].Progress in Natural Science,2007,17(6):770-778.]
    [50]赵安周,张安兵,刘海新,等.退耕还林(草)工程实施前后黄土高原植被覆盖时空变化分析[J].自然资源学报,2017,32(3):449-460.[Zhao A Z,Zhang A B,Liu H X,et al.Spatiotemporal variation of vegetation coverage before and after implementation of grain for Green Project in the Loess Plateau[J].Journal of Natural Resources,2017,32(3):449-460.]
    [51]刘秀丽,张勃,郑庆荣,等.黄土高原土石山区退耕还林对农户福祉的影响研究-以宁武县为例[J].资源科学,2014,36(2):397-405.[Liu X L,Zhang B,Zheng Q R,et al.Impacts of converting farmland into forests on farmer well-being in the EarthRock Mountain Areas of the Loess Plateau[J].Resources Science,2014,36(2):397-405.]

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