Special Column:Celebration of the 70th Anniversary of IGSNRR, CAS

Spatial-temporal Changes of Vegetation Index and Its Responses to Regional Temperature in Taibai Mountain

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  • College of Urban and Environment, Northwest University, Xi'an 710127, China

Received date: 2011-01-21

  Revised date: 2011-03-29

  Online published: 2011-08-20

Abstract

Taibai Mountain, the peak of Qinling Mountains, is located in the middle hinterland of Qinling Mountains. Based on NDVI data of Taibai Mountains Nature Reserve in May which were derived from remote sensing and in site survey, we analyzed the spatial-temporal changes of vegetation index for different vegetation zones during 1979 to 2009, as well as their responses to temperature. The results showed that the area where the average NDVI in May was higher than 0.2 accounts for 89.5% of the total Taibai Mountain, which indicates a good vegetation cover in the mountain nowadays. However, the significant vertical deviation was found in NDVI. The value of NDVI is generally over 0.2 for the low altitude regions while ranges from 0.2 to 0.5 for the high altitude regions. The pixles where NDVI increased and decreased significantly during the past three decades account for 4.88% and 3.92%, respectively, and no change was found in about 56% of the total pixles. The annual mean temperature in the study area tends to increase with a slope of 0.35℃/10 a during the last 30 years. The vegetation changes became more sensitive to temperature with the increase of altitude, which indicates that the ecosystem of Taibai Mountain that is characterized by a small human disturbance and a high elevation deviation has become a sensitive place responding to climate change.

Cite this article

ZHANG Shan-hong, BAI Hong-ying, GAO Xiang, HE Ying-na, REN Yuan-yuan . Spatial-temporal Changes of Vegetation Index and Its Responses to Regional Temperature in Taibai Mountain[J]. JOURNAL OF NATURAL RESOURCES, 2011 , 26(8) : 1377 -1386 . DOI: 10.11849/zrzyxb.2011.08.024

References

[1] 张金屯. 植被资源与可持续发展[J]. 山西大学学报: 自然科学版, 1998, 17(4): 80-84. [2] 信忠保, 许炯心. 黄土高原地区植被覆盖时空演变对气候的响应[J]. 自然科学进展, 2007, 17(6): 770-778. [3] 马明国, 董立新, 王雪梅. 过去21a中国西北植被覆盖动态监测与模拟[J]. 冰川冻土, 2003, 25(2): 232-236. [4] 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, 2003, 33(6): 554-567. [5] 郑有飞, 牛鲁燕, 吴荣军, 等. 1982—2003年贵州省植被覆盖变化及其对气候变化的响应[J]. 生态学杂志, 2009, 28(9): 1773-1778. [ZHENG You-fei, NIU Lu-yan, WU Rong-jun, et al. Vegetation cover change in Guizhou of Southwest China in 1982-2003 in response to climate change. Chinese Journal of Ecology, 2009, 28(9): 1773-1778.] [6] 陈操操, 谢高地, 甄霖, 等. 泾河流域植被覆盖动态变化特征及其与降雨的关系[J]. 生态学报, 2008, 28(3): 925-938. [7] 任毅, 刘明时, 田联会, 等. 太白山自然保护区生物多样性研究与管理[M]. 北京: 中国林业出版社, 2006. [8] 高丽敏, 陈兴鹏, 黄艳, 等. 基于RS和GIS的中国西北不同生态类型区生态环境时空变化研究[J]. 中国沙漠, 2007, 27(1): 65-71. [9] 陈隆陨, 朱文琴, 王文, 等. 中国近45年来气候变化的研究[J]. 气象学报, 1998, 56(3): 257-271. [10] 郭志梅, 缪启龙, 李雄, 等. 中国北方地区近50年来温度变化特征的研究[J]. 地理科学, 2005, 25(4): 448-454. [11] 《气候变化国家评估报告》编写委员会. 气候变化国家评估报告[M]. 北京: 科学出版社, 2007. [12] 任国玉, 郭军, 徐铭志, 等. 近50年来中国地面气候变化基本特征[J]. 气象学报, 2005, 63(6): 942-956. [13] 雒新萍. 近25年来秦巴山区植被NDVI时空变化及对区域气候的响应. 西安: 西北大学, 2009. [LUO Xin-ping. Spatial-temporal Change of NDVI and the Response to the Regional Climate in the Qinling-Daba Mountains for 25 Years. Xi'an: Northwest University, 2009.] [14] 孙华. 近30年来秦岭南北坡植被指数时空差异及其与区域气候的响应. 西安: 西北大学, 2010. [15] 孙杰. 1982~2000年中国植被覆盖变化及典型区域与气候因子的响应关系. 南京: 南京信息工程大学, 2007. [SUN Jie. Vegetation Change in China and the response of Typical Areas with Climatic Factors during 1982-2000. Nanjing: Nanjing University of Information Science & Teehnology, 2007.] [16] Nemani Ramakrishna, Steve Running. Land cover characterixation using multitemporal red, near-infrare and the mal-infare data fron NOAA/ARHRR[J].Ecological Applications, 1997,7(1):77-90. [17] 《陕西省太白山国家级自然保护区管理计划》编写小组. 秦岭自然保护区群陕西省太白山国家级自然保护区管理计划[M]. 2001.
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