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JOURNAL OF DESERT RESEARCH  2014, Vol. 34 Issue (6): 1665-1670    DOI: 10.7522/j.issn.1000-694X.2014.00032
    
Response of Vegetation Cover to Climate Change and Human Activities in Northwest China During 1999-2010
Wei Zhenfeng1,2, Wang Deguang2, Zhang Chong1, Liu Xianfeng3, Zhang Han1
1. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062, China;
2. Guangxi University of Finance and Economics, Nanning 530003, China;
3. State Key Laboratory of Earth Surface Processes and Resources Ecology/College of Resources Science & Technology, Beijing Normal University, Beijing 100875, China
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Abstract  As a typical ecological fragile area, Northwest China is marked by drought and dust climate. Vegetation is known as an indicator of the terrestrial ecosystems response to climate change. In th paper, the normalized difference vegetation index (NDVI) from 1999 to 2010 and meteorological data are employed to investigate the spatiotemporal variation of vegetation cover over Northwest China, and the effects of human activities and climate change on vegetation cover change were also analyzed by using Sen-trend combined with the Mann-Kendall test, correlation and partial correlation analysis and residual method. The results showed that the vegetation coverage presented an increasing trend over Northwest China, but the vegetation growth was still hindered in some areas. The spatial difference of vegetation cover change may be the results of the interaction between human activities and climate change. Vegetation cover was significantly correlated with climatic factors in most area. What's more, the response of vegetation cover change to temperature and precipitation had a lag time. Evapotranspiration was greater than precipitation, and human irrigation had to make up for the lack of water, which made agricultural vegetation area increase. The vegetation cover decreased in Northern Xinjiang due to drought and desertification, human activities and urban expansion also inhibited the growth of vegetation seriously.
Key words:  Northwest China      vegetation cover      climate change      human activity      response     
Received:  31 December 2013      Published:  20 November 2014
ZTFLH:  Q948.2  
Corresponding Authors:  王德光(Email:wanwanshun@qq.com)     E-mail:  wanwanshun@qq.com

Cite this article: 

Wei Zhenfeng, Wang Deguang, Zhang Chong, Liu Xianfeng, Zhang Han. Response of Vegetation Cover to Climate Change and Human Activities in Northwest China During 1999-2010. JOURNAL OF DESERT RESEARCH, 2014, 34(6): 1665-1670.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2014.00032     OR     http://www.desert.ac.cn/EN/Y2014/V34/I6/1665

[1] 孙红雨,王长耀,牛铮,等.中国植被覆盖变化及其与气候因子关系——基于NOAA时间序列数据[J].遥感学报,1998,2(3):204-210.
[2] Myneni R B,Keeling C D,Tucker C J,et al.Increased plantgrowth in the northern high latitudes from 1981 to 1999[J].Nature,1997,386:698-702.
[3] Myneni R B,Tucker C J,Asar G,et al.Interannual variations in satellite-sensed vegetation index data from 1981 to 1991[J].Journal of Geophysical Research,1998,103(6):6145-6160.
[4] Zhou L,Tucker C J,Kaufmann R K,et al.Variations in northern vegetation activity inferred from satellite data of vegetation index during 1981-1999[J].Journal of Geophysical Research,2001,106(17):20069-20083.
[5] Nemani R,Keeling C,Hashimoto H,et al.Climate-driven increases in global terrestrial net primary production from 1982 to 1999[J].Science,2003,300:1560-1563.
[6] 方精云,朴世龙,贺金生,等.近 20 年来中国植被活动在增强[J].中国科学C辑:生命科学,2003,33(6):554-565.
[7] 朴世龙,方精云.最近 18 年来中国植被覆盖的动态变化[J].第四纪研究,2001,21(4):294-302.
[8] 朴世龙,方精云.1982-1999年我国陆地植被活动对气候变化响应的季节差异[J].地理学报,2003,58(1):119-125.
[9] 陈效逑,喻蓉.1982-1999年我国东部暖温带植被生长期节的时空变化[J].地理学报,2007,62(1):41-51.
[10] 黄磊,张志山,陈永乐.干旱人工固沙植被区土壤水分动态随机模拟[J].中国沙漠,2013,33(2):568-573.
[11] 包刚,覃志豪,包玉海,等.1982-2006年蒙古高原植被覆盖时空变化分析[J].中国沙漠,2013,33(3):918-927.
[12] 蒋冲,王文丽,陈爱芳,等.近52年渭河流域气候变化对植被净第一性生产力的影响[J].中国沙漠,2013,33(3):952-957.
[13] 刘宪锋,杨勇,任志远,等.2000-2009年黄土高原地区植被覆盖度时空变化[J].中国沙漠,2013,33(4):1244-1249.
[14] 刘绿柳,肖风劲.黄河流域植被 NDVI 与温度、降水关系的时空变化[J].生态学杂志,2006,25(5):477-481.
[15] Beck H E,McVicar T R,van Dijk A I J M,et al.Global evaluation of four AVHRR-NDVI data sets:intercomparison and assessment against Landsat imagery[J].Remote Sensing of Environment,2011,115(10):2547-2563.
[16] Goetz S J,Fiske G J,Bunn A G.Using satellite time-series data sets to analyze fire disturbance and forest recovery across Canada[J].Remote Sensing of Environment,2006,101(3):352-365.
[17] Yue S,Pilon P,Cavadias G.Power of the Mann-Kendall and Spearman's rho tests for detecting monotonic trends in hydrological series[J].Journal of Hydrology,2002,259:254-271.
[18] 徐建华.现代地理学中的数学方法[M].北京:高等教育出版社,2002.
[19] Envans J,Geerken R. Discrimination between climate and human-induced dryland degradation[J].Journal of Arid Environments,2004,57(4):535-554.
[20] Wesscls K J,Prince S D,Malherbe J,et al.Can human-induced land degradation be distinguished from the effects of rainfall variability?a case study in South Africa[J].Journal of Arid Environments,2007,68(2):271-297
[21] 蔡两峰.基于遥感的林业生态工程监测和评价研究[D].北京:中国科学院遥感应用研究所,2003.
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