长江科学院院报 ›› 2022, Vol. 39 ›› Issue (2): 56-62.DOI: 10.11988/ckyyb.20201075

• 水土保持与生态修复 • 上一篇    下一篇

黄河流域1982—2015年不同气候区植被时空变化特征及其影响因素

陈晨, 王义民, 黎云云, 周帅   

  1. 西安理工大学 省部共建西北旱区生态水利国家重点实验室,西安 710000
  • 收稿日期:2020-10-23 修回日期:2021-02-09 出版日期:2022-02-01 发布日期:2022-02-11
  • 通讯作者: 王义民(1972-),男,山西新绛人,教授,博士,主要从事水文学及水资源研究。E-mail:wangyimin@xaut.edu.cn
  • 作者简介:陈 晨(1995-),女,安徽合肥人,硕士,主要从事水文学及水资源研究。E-mail:1142471760@qq.com
  • 基金资助:
    国家自然科学基金项目(51879214,51909207)

Vegetation Changes and Influencing Factors in Different Climatic Regions of Yellow River Basin from 1982 to 2015

CHEN Chen, WANG Yi-min, LI Yun-yun, ZHOU Shuai   

  1. State Key Laboratory of Eco-hydraulics in Northwest Arid Region of China, Xi'an University of Technology, Xi'an 710000, China
  • Received:2020-10-23 Revised:2021-02-09 Published:2022-02-01 Online:2022-02-11

摘要: 研究不同气候区植被覆盖的时空变化及气候因子与植被生长的关系,对生态环境建设与治理具有重要意义。基于1982—2015年GIMMS NDVI 3g数据集,运用均值法、Sen+Mann-Kendall趋势分析、偏相关系数、多元线性回归模型+残差法等方法,分析了黄河流域不同气候区生长季植被时空变化特征及气候因子与人类活动对植被变化的影响。结果表明:①1982—2015年黄河流域及不同气候区归一化植被指数(NDVI)年际变化呈缓慢上升趋势,干旱区变化波动平稳,半湿润区变化较明显。②34 a来各气候区大部分地区植被呈显著增加,半干旱区所占面积比例最大,不显著减少主要分布在半湿润区西南部及南部。③各气候区降水、气温、日照时数对NDVI表现出正影响,且日照影响最大;在半干旱区降水对NDVI影响最大,在半湿润区影响最小,在半湿润区气温对NDVI影响最大,在干旱区影响最小。④34 a来,人类活动对各气候区植被的积极影响明显大于消极影响。

关键词: 归一化植被指数, 时空变化, 不同气候区, 气候因子, 人类活动, 黄河流域

Abstract: Studying the temporal and spatial changes of vegetation coverage in different climatic regions and the relation between climatic factors and vegetation growth is of great significance to the construction and governance of ecological environment. Based on the GIMMS NDVI 3g dataset from 1982 to 2015, we examined the temporal and spatial changes of vegetation coverage in growth season in different climatic regions of the Yellow River Basin using the mean method, Sen+Mann Kendall trend analysis, partial correlation coefficient, multiple linear regression model plus residual method. We also analyzed the impacts of climatic factors and human activities on vegetation changes. Results demonstrated that: 1) The interannual change of NDVI in the Yellow River Basin and different climatic regions showed a slow upward trend from 1982 to 2015. The changes in arid region were steady, while the changes in semi-humid areas were more obvious. 2) In the past 34 years, vegetation increased remarkably in most of the climatic regions, of which the semi-arid region accounted for the largest proportion, whereas the southwest and south part of the semi-humid region mainly subjected to slight reduce. 3) Precipitation, temperature, and sunshine time in various climatic regions had positive impacts on NDVI, among which sunshine time had the greatest impact; in semi-arid region precipitation had the greatest impact on NDVI, whereas in semi-humid region the least impact; in semi-humid region temperature had the greatest impact on NDVI, while in arid region the least impact. 4) In the past 34 years, human activities exerted far more positive impact on vegetation than negative impact.

Key words: Normal Difference Vegetation Index(NDVI), spatiotemporal changes, different climate zones, climate factors, human activities, Yellow River Basin

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