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1982—2015年黄土高原NDVI时空演变及其对气候变化的季节响应


范倩倩1,赵安周2,3*,王金杰1,张安兵2,裴韬3   

  1. (1河北工程大学地球科学与工程学院, 河北邯郸 056038; 2河北工程大学矿业与测绘工程学院, 河北邯郸 056038; 3中国科学院地理科学与资源研究所, 资源与环境信息系统国家重点实验室, 北京 100101)
  • 出版日期:2020-05-10 发布日期:2020-05-10

Spatiotemporal evolution of NDVI and its seasonal response to climate change in the Loess Plateau from 1982 to 2015.

FAN Qian-qian1, ZHAO An-zhou2,3*, WANG Jin-jie1, ZHANG An-bing2, PEI Tao3   

  1. (1School of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, Hebei, China; 2School of Mining and Geomatics, Hebei University of Engineering, Handan 056038, Hebei, China; 3State Key Laboratory of Resources and Environmental Information System, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China).
  • Online:2020-05-10 Published:2020-05-10

摘要: 基于GIMMS NDVI、温度和降水数据,利用集合经验模态分解(EEMD)、线性回归分析、偏相关分析等方法分析了1982—2015年黄土高原植被覆盖时空变化及其对气候变化的季节响应。结果表明:年际变化趋势上,1982—2015年黄土高原生长季、春、夏、秋季NDVI均呈显著增长趋势,且各个季节NDVI增加速率逐年升高,尤其以夏季增加速率的变化最为明显;空间上,生长季、春、夏、秋季NDVI均呈由西北向东南递增的趋势,且在大部分地区呈显著上升趋势;线性回归表明,生长季、春、夏、秋季温度均呈显著上升趋势;生长季、秋季降水呈增加趋势,春、夏季降水呈减少趋势。EEMD分析进一步表明,生长季、春、夏、秋季温度均先升高后降低,降水均呈先减少后增加的趋势;空间变化趋势上,温度在生长季、春、夏、秋季大部分地区呈显著上升趋势,降水仅秋季有部分区域呈显著上升趋势;NDVI与温度在黄土高原东北部及西南部地区呈显著正相关,与降水在黄土高原北部及西北部地区呈显著正相关。

关键词: 弃耕农田, 鄂尔多斯高原, 灌丛化, 土壤物理性质

Abstract: Based on data of GIMMS (Global Inventory Modelling and Mapping Studies) NDVI (Normalized Difference Vegetation Index), temperature, and precipitation, we analyzed the spatiotemporal variation of vegetation cover and its seasonal response to climate change in the Loess Plateau from 1982 to 2015, using the Ensemble Empirical Mode Decomposition (EEMD), linear regression analysis, and partial correlation analysis. In the interannual variation trend from 1982 to 2015, NDVI on the Loess Plateau increased significantly in the growing season, spring, summer, and autumn. The increasing rate of NDVI in each season also increased during 1982 and 2015, with the most obvious change in summer. Spatially, NDVI gradually increased from northwest to southeast in the growing season, spring, summer and autumn, which was statistically significant in most areas. As shown by the linear regression analysis, temperature had a significant increase trend in the growing season, spring, summer, and autumn, while precipitation increased in the growing season and autumn and decreased in spring and summer. The results of EEMD analysis further showed that in the growing season, spring, summer, and autumn, temperature first increased and then decreased, and precipitation first decreased and then increased. In terms of spatial variation, temperature had a significant increase trend in most areas during the growing season, spring, summer, and autumn, while precipitation had a significant increase trend only in some areas during autumn. There was a significant positive correlation between NDVI and temperature in the northeast and southwest of the Loess Plateau, and a significant positive correlation between NDVI and precipitation in the north and northwest of the Loess Plateau.

Key words: abandoned cropland, soil physical property, Ordos Plateau., shrub encroachment