草地学报 ›› 2021, Vol. 29 ›› Issue (11): 2513-2522.DOI: 10.11733/j.issn.1007-0435.2021.11.017

• 研究论文 • 上一篇    下一篇

1998-2018年藏北申扎县植被NDVI时空变化及其影响因素

张晓克1,2, 孟宏志1   

  1. 1. 河海大学公共管理学院, 江苏 南京 211100;
    2. 河海大学环境与社会研究中心, 江苏 南京 211100
  • 收稿日期:2021-05-10 修回日期:2021-07-25 出版日期:2021-11-15 发布日期:2021-12-06
  • 作者简介:张晓克(1984-),女,河北邢台人,博士,副教授,主要从事生态遥感与GIS研究,E-mail:xkzhang@hhu.edu.cn
  • 基金资助:
    国家自然科学基金项目(41601435);国家重点研发计划项目(2016YFC0502002);中央高校基本科研业务费专项资金项目(2018B21414)资助

Spatial-temporal variation of NDVI and its influencing factors in Xainza County from 1998 to 2018

ZHANG Xiao-ke1,2, MENG Hong-zhi1   

  1. 1. School of Public Administration, Hohai University, Nanjing, Jiangsu Province 211100, China;
    2. Center for Environmental and Social Studies, Hohai University, Nanjing, Jiangsu Province 211100, China
  • Received:2021-05-10 Revised:2021-07-25 Online:2021-11-15 Published:2021-12-06

摘要: 为研究1998-2018年申扎县归一化植被指数(Normalized difference vegetation index,NDVI)的变化及其驱动力,本研究基于申扎县NDVI、地形和气象等数据,采用线性回归和残差分析等研究方法分析申扎县NDVI年际时空变化特征及其影响因子。结果表明:申扎县NDVI整体呈波动上升趋势,年均增长率为1.595%;年均NDVI随高程和坡度的增加呈现单峰曲线状的变化趋势,峰值分别位于4 900~5 200 m和10°~15°;NDVI与气温的正相关性(r=0.556,P=0.009)较降水(r=0.271,P=0.234)高;气温每升高1℃,NDVI增加0.291;降水量每增加100 mm,NDVI增加0.224;2012年后人类活动总体上开始对植被生长产生正作用;NDVI与人类活动成正、负显著相关的区域占比为24.13%,20.01%。总体上,NDVI增加主要是由于气候暖湿化和地方生态工程的有效实施等共同作用导致的。

关键词: NDVI, 时空变化, 气候变化, 人类活动, 申扎县

Abstract: This study was aimed to study the variation of vegetation NDVI (Normalized difference vegetation index) and its driving forces in Xainza County from 1998 to 2018. Based on NDVI,topographic and meteorological data,this study analyzed the interannual temporal and spatial variation characteristics of NDVI in Xainza County and its influencing factors by using linear regression and residual analysis and other methods. The results showed that:NDVI in Xainza county showed an upward trend of fluctuation with an average annual growth rate of 1.595%. The average annual NDVI showed a single peak curve trend with the increase of elevation and slope,with the peak value of 4 900~5 200 m and 10°~15°. The vegetation growth was positively correlated with precipitation and air temperature,and the correlation and significance with air temperature (r=0.556,P=0.009) was higher than that with precipitation (r=0.271,P=0.234). For every 1℃ increase in temperature,NDVI increased by 0.291,for every 100 mm increase in precipitation,NDVI increased by 0.224. After 2012,human activities had a positive impact on vegetation growth. On the whole,the increase of NDVI was mainly due to the combined effects of climate warming and humidity and the effective implementation of local ecological engineering.

Key words: NDVI, Spatial-temporal variation, Climate change, Human activities, Xainza County

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