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1982—2009年青藏高原草地覆盖度时空变化特征

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  • 1. 中国科学院 地理科学与资源研究所, 北京 100101;
    2. 鄱阳湖湿地与流域研究教育部重点实验室(江西师范大学), 南昌 330028
丁明军(1979- ),男,湖北谷城人,副教授,主要从事生物地理学、土地利用/覆被变化及其环境效应。E-mail: dingmingjun1128@163.com

收稿日期: 2010-03-29

  修回日期: 2010-07-07

  网络出版日期: 2010-12-20

基金资助

国家重点基础研究发展计划(2010CB951704,2005CB422006);国家科技支撑计划项目(2007BAC06B08);国家自然科学基金项目(40771206)。

Temporal and Spatial Distribution of Grassland Coverage Change in Tibetan Plateau since 1982

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  • 1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    2. Key Lab of Poyang Lake Wetland and Watershed Research, Ministry of Education(Jiangxi Normal University), Nanchang 330022, China

Received date: 2010-03-29

  Revised date: 2010-07-07

  Online published: 2010-12-20

摘要

利用GIMMS和SPOT VGT两种归一化植被指数(NDVI)数据对青藏高原地区1982—2009年期间草地覆盖的时空变化进行研究,结果如下:①青藏高原草地植被覆盖的年际变化存在着显著的空间差异。趋于升高的区域主要分布在西藏的北部和新疆的南部;趋于下降的地区主要分布在青海的柴达木盆地、祁连山、共和盆地、江河源地区及川西地区。②青藏高原草地覆盖度年际变化趋势分析表明,在90%的显著性检验水平上,降低和增加面积的比率为0.31,草地植被覆盖水平总体趋于升高态势。③以10 a为步长的分析表明:草地盖度呈现持续增加的区域主要分布在西藏北部;阿里地区草地盖度表现为先减少后增加;雅鲁藏布江流域草地盖度呈现先增加而后减少;而持续减少的区域主要分布在青海省以及川西地区,其中青海省分布最广;统计结果显示,高原大部分地区草地盖度具有升高的态势。

本文引用格式

丁明军, 张镱锂, 刘林山, 王兆锋 . 1982—2009年青藏高原草地覆盖度时空变化特征[J]. 自然资源学报, 2010 , 25(12) : 2114 -2122 . DOI: 10.11849/zrzyxb.2010.12.012

Abstract

Based on the remote sensing data such as NDVI data from GIMMS and SPOT VGT, the paper analyzed temporal and spatial distribution of grassland cover change from 1982 to 2009. The results showed that: 1) There was significant spatial difference in grassland coverage change. The area with grassland coverage increasing was mainly distributed in northern Tibet and southern Xinjiang; the area with grassland decreasing was mainly distributed in the headwaters of the Yangtze River, Yellow River, Lancang River, and Nujiang River, the Qaidam Basin and Gonghe Basin, Qilian Mountains and western Sichuan Province. 2) Statistics of grassland coverage inter-annual change showed that at significance test level of 90%, the rate of the area with coverage decreasing and increasing was 0.31, and the grassland coverage on Tibetan Plateau tends to be increased. 3) Analysis with ten years showed that: the grassland coverage with continuous increase was mainly distributed in northern Tibet; the grassland coverage in Ngari of Tibet decreased firstly and then increased; nevertheless, the Brahmaputra Valley increased firstly and then decreased; the area with continuous decreasing tendency was mainly distributed in Qinghai Province and western Sichuan Province; the statistics showed that most of the grassland coverage on Tibetan Plateau displayed an increasing tendency.

参考文献

[1] 张镱锂, 李炳元, 郑度. 论青藏高原范围与面积[J]. 地理研究, 2002, 21(1): 1-8. [2] 崔庆虎, 蒋志刚, 刘季科. 青藏高原草地退化原因述评[J]. 草业科学, 2007, 24(2): 20-26. [3] 杨汝荣. 西藏阿里地区草地退化现状与防治措施[J]. 中国草地, 2002, 24(1): 62-67. [4] 邵伟, 蔡晓布. 西藏高原草地退化及其成因分析[J]. 中国水土保持科学, 2008, 6(1): 112-116. [5] 刘纪远, 徐新良, 邵全琴. 近30年来青海三江源地区草地退化的时空特征[J]. 地理学报, 2008, 63(4): 364-376. [6] 高清竹, 李玉娥, 林而达, 等. 藏北地区草地退化的时空分布特征[J]. 地理学报, 2005, 60(6): 965-973. [7] 梁四海, 陈江, 金晓媚, 等. 近21年青藏高原植被覆盖变化规律[J]. 地球科学进展, 2006, 22(1): 33-40. [8] 向波, 缪启龙, 高庆先. 青藏高原气候变化与植被指数的关系研究[J]. 四川气象, 2001, 75(1): 29-36. [9] 杨元合, 朴世龙. 青藏高原草地植被覆盖变化及其与气候因子的关系[J]. 植物生态学报, 2006, 30(1): 1-8. [10] Pinzon J. Using HHT to successfully uncouple seasonal and inter-annual components in remotely sensed data . SCI 2002. Conference Proceedings July 14-18. Orlando, Florida. 2002. [11] Tucker C J, Pinzon J E, Brown M E, et al. An Extended AVHRR 8 km NDVI data set compatible with MODIS and SPOT vegetation NDVI data [J]. Int. J. Remote Sensing, 2005, 26(20): 4485-4498. [12] Chen X Q, Tan Z J, SchwartzM D, et al. Determining the growing season of land vegetation on the basis of plant phenology and satellite data in Northern China [J]. International Journal of Biometeorology, 2000, 44: 97-101. [13] 张玮. 土地利用/覆被分类与碳储量研究——以青藏高原为例. 北京: 中国科学院研究生院, 2007. [14] Eastwood J A, M G Yates, A G Thomson, et al. The reliability of vegetation indices for monitoring saltmarsh vegetation cover [J]. Int. J. Remote Sensing, 1997, 18(18): 3901-3907. [15] Purevdorj Ts, Tateishi R, Ishiyama T, et al. Relationships between percent vegetation cover and vegetation indices [J]. Int. J. Remote Sensing, 1998, 19(18): 3519-3535. [16] Leprieur C, Y H Kerr, S Mastorchio, et al. Monitoring vegetation cover across semi-arid regions: comparison of remote observations from various scales [J]. Int. J. Remote Sensing, 2000, 21(2): 281-300. [17] Toby N Carlson, David A Ripley. On the relation between NDVI, fractional vegetation cover, and leaf area index [J]. Remote Sense. Environ., 1997, 62: 241-252. [18] Wittich K P, Hansing O. Area-averaged vegetative cover fraction estimated from satellite data [J]. International Journal of Biometereology, 1995, 38: 209-215. [19] 陈云浩, 李晓兵, 史培军, 等. 北京海淀区植被覆盖的遥感动态研究[J]. 植物生态学报, 2001, 25(5): 588-593. [20] 刘玉洁, 杨忠东. MODIS遥感数据的原理及算法[M]. 北京: 科学出版社, 2001: 229-301. [21] 毛飞, 张艳红,侯英雨. 藏北那曲地区草地退化动态评价[J]. 应用生态学报, 2008, 19(2): 278-284. [22] Micael C Runnstrm. Is Northern China winning the battle against desertification-Satellite remote sensing as a tool to study biomass trends on the Ordoas Plateau in semiarid China [J]. AMBIO, 2000, 29(8): 468-476. [23] 杨建平, 丁永建, 陈仁升. 长江、黄河源区高寒植被变化的NDVI记录[J]. 地理学报, 2005, 60(3): 468-478. [24] 张镱锂, 刘林山, 摆万奇, 等. 黄河源地区草地退化空间特征[J]. 地理学报, 2006, 61(1): 4-12. [25] 张镱锂, 丁明军, 张玮, 等. 三江源地区植被指数下降趋势的空间特征及其地理背景[J]. 地理研究, 2007, 26(3): 500-507. [26] DING Ming-jun, ZHANG Yi-li, LIU Lins-han, et al. The relationship between NDVI and precipitation on the Tibetan Plateau [J]. Journal of Geographical Sciences, 2007, 17(3): 259-268. [27] Zhong Lei, Ma Yao-ming, Salama M M. Assessment of vegetation dynamics and their response to variations in precipitation and temperature in the Tibetan Plateau [J]. Climatic Change, 2010, DOI: 10. 1007/s10584-009-9787-8. [28] 中华人民共和国国家标准GB19377: 天然草地退化、沙化、盐泽化的分级指标[S]. 中华人民共和国国家质量监督检验检疫总局, 2003.
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