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学院教育部水土保持与生态环境研究中心),2019 .
[ 24] 范倩倩,赵安周,王金杰,等 . 1982—2015 年黄土高原 NDVI 时空演变及其对气候变化的季节响应[J]. 生
态学杂志,2020,39(5):1164-1675 .
[ 25] MAO D,WANG Z,LUO L,et al . Integrating AVHRR and MODIS data to monitor NDVI changes and their rela⁃
tionships with climatic parameters in Northeast China[J]. International Journal of Applied Earth Observation and
Geoinformation,2012,18(1):528-536 .
[ 26] BRUNSDON C,FOTHERINGHAM A S,CHARLTON M E . Geographically weighted regression:A method for ex⁃
ploring spatial nonstationarity[J]. Geographical Analysis,1996,28(4):281-298 .
[ 27] LI D,PAN M,CONG Z,et al . Vegetation control on water and energy balance within the Budyko framework[J].
Water Resources Research,2013,49(2):969-976 .
[ 28] 金凯,王飞,韩剑桥,等 . 1982—2015 年中国气候变化和人类活动对植被 NDVI 变化的影响[J]. 地理学
报,2020,75(5):75-88 .
[ 29] 张建云,贺瑞敏,齐晶,等 . 关于中国北方水资源问题的再认识[J]. 水科学进展,2013,24(3):303-310 .
[ 30] 张树磊,杨大文,杨汉波,等 . 1960—2010 年中国主要流域径流量减小原因探讨分析[J]. 水科学进展,
2015,26(5):605-613 .
[ 31] DONOHUE R J,RODERICK M L,MCVICAR T R . Assessing the differences in sensitivities of runoff to changes
in climatic conditions across a large basin[J]. Journal of Hydrology,2011,406(3/4):234-244 .
[ 32] ZHOU G,WEI X,CHEN X,et al . Global pattern for the effect of climate and land cover on water yield[J] . Na⁃
ture Communications,2015(3):40-40 .
[ 33] 周国逸,夏军,周平,等 . 不恰当的植被恢复导致水资源减少[J] . 中国科学(地球科学),2021,51(2):
175-182 .
[ 34] 何小武,刘广全,郭孟华 . 黄土高原植被建设的水资源环境及对策[J]. 水利学报,2008,39(7):843-847 .
Analysis of vegetation change and its impact on natural runoff in the mountain area of the
Yongding River Basin from 1982 to 2015
1
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3
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DU Yong 1,2 ,LI Jianzhu ,NIU Kaijie ,FENG Ping ,HU Qingfang ,ZHENG Yanchen 1
(1. State Key Laboratory of Hydraulic Engineering Simulation and Safety,Tianjin University,Tianjin 300072,China;
2. Yongding River Basin Investment Co.,Ltd.,Beijing 100193,China;
3. State Key Laboratory of Hydrology Water Resources and Hydraulic Engineering,
Nanjing Hydraulic Research Institute,Nanjing 210029,China)
Abstract:Based on the monitoring data of NDVI,temperature,precipitation,and runoff,the spatial relationship between
NDVI and temperature,precipitation and residual was studied respectively by constructing geographically weighted regres⁃
sion model,then the influence of NDVI change on natural runoff attenuation was quantitatively estimated. The result
showed that: the overall change of land use pattern was minimum from 1982 to 2015 in the mountain area of Yongding Riv⁃
er,and NDVI of vegetation increased significantly at both annual and seasonal scales. The mean and trend values of spatial
regression parameters,residual of NDVI and precipitation or average temperature had obvious spatial heterogeneity. The
mean values of regression parameters and residual were positive at different time scales,while their trends fluctuated obvi⁃
ously. It indicated that precipitation,temperature and human activities all can increase NDVI value,while the trend of
each factor had significant difference. The natural runoff had a significant attenuation trend. Due to underlying surface
change with the increase of NDVI,the contribution rate of the natural runoff attenuation of typical section was about 80%,
which indicated that the natural runoff was highly sensitive to vegetation change by Budyko equation. Great attention should
be paid to the impact of vegetation conservation in the watershed on the attenuation of natural runoff.
Keywords: NDVI;GWR model;precipitation;average temperature;natural runoff;the mountainous area of Yongding
River
(责任编辑:耿庆斋)
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