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王筝, 赵天保, 侯美亭, 延晓冬. 21世纪初中国北方地区植被变化特征分析[J]. 气候与环境研究, 2013, 18(2): 156-164. DOI: 10.3878/j.issn.1006-9585. 2012.11026
引用本文: 王筝, 赵天保, 侯美亭, 延晓冬. 21世纪初中国北方地区植被变化特征分析[J]. 气候与环境研究, 2013, 18(2): 156-164. DOI: 10.3878/j.issn.1006-9585. 2012.11026
WANG Zheng, ZHAO Tianbao, HOU Meiting, YAN Xiaodong. Vegetation Index Trends for the Northern Part of China at the Beginning of the 21st Century[J]. Climatic and Environmental Research, 2013, 18(2): 156-164. DOI: 10.3878/j.issn.1006-9585. 2012.11026
Citation: WANG Zheng, ZHAO Tianbao, HOU Meiting, YAN Xiaodong. Vegetation Index Trends for the Northern Part of China at the Beginning of the 21st Century[J]. Climatic and Environmental Research, 2013, 18(2): 156-164. DOI: 10.3878/j.issn.1006-9585. 2012.11026

21世纪初中国北方地区植被变化特征分析

Vegetation Index Trends for the Northern Part of China at the Beginning of the 21st Century

  • 摘要: 利用增强型植被指数(EVI)作为植被活动的指标, 用MODIS-EVI时间序列数据定量分析了2000~2009年间中国北方地区EVI的变化规律。结果表明:1)21世纪初中国北方地区植被覆盖总体改善, 局部退化, 10年来区域年平均EVI增加5.97%;2)逐季节平均EVI均呈现上升趋势, 春季、秋季上升幅度小, 夏季、冬季上升幅度大;3)中国北方地区植被稀少的区域呈减少趋势, 同时单位面积EVI增加, 植被生长更加茂盛;4)中国北方地区EVI变化空间异质性大。东北平原、华北平原、黄土高原和新疆农业区显著增加, 东北和西部部分地区植被退化。

     

    Abstract: Moderate-resolution Imaging Spectroradiometer (MODIS)-Enhanced Vegetation Index (EVI) data reported during 2000-2009 have been analyzed to study recent trends in vegetation greenness over the northern part of China at the beginning of the 21st century. The results showed that the afforestation area was larger than the degraded area in the northern part of China during the last 10 years, and the regional total mean annual EVI increased by 5.97%. Seasonal EVI increased significantly, and trends in summer and winter were larger than those in spring and autumn. The sparsely vegetated area declined, unit area EVI increased, and vegetation activity rose during the study period. In addition, EVI changes in the northern part of China exhibited relatively large spatial heterogeneity. The Northeast China Plain, North China Plain, Loess Plateau, and Xinjiang agriculture regions experienced marked increases, and part of Northeast China and West China experienced declining trends. Such patterns are attributed primarily to regional climate changes and human activities such as ecological construction and urbanization.

     

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