陕西师范大学旅游与环境学院,陕西,西安,710062
纸质出版:2014
移动端阅览
刘栎杉, 延军平, 李双双. 2000-2009年青海省植被覆盖时空变化特征[J]. 水土保持通报, 2014,33(1):263-267.
LIU Li-shan, YAN Jun-ping, LI Shuang-shuang. Spatial-temporal Characteristics of Vegetation Restoration in Qinghai Province from 2000 to 2009[J]. Bulletin of Soiland Water Conservation, 2014, 33(1): 263-267.
刘栎杉, 延军平, 李双双. 2000-2009年青海省植被覆盖时空变化特征[J]. 水土保持通报, 2014,33(1):263-267. DOI: 10.13961/j.cnki.stbctb.2014.01.007.
LIU Li-shan, YAN Jun-ping, LI Shuang-shuang. Spatial-temporal Characteristics of Vegetation Restoration in Qinghai Province from 2000 to 2009[J]. Bulletin of Soiland Water Conservation, 2014, 33(1): 263-267. DOI: 10.13961/j.cnki.stbctb.2014.01.007.
基于2000-2009年MODIS-NDVI植被覆盖指数
采用线性趋势分析、标准差等数理分析方法
对青海省"退耕还林还草"实施10 a来植被覆盖时空变化特征进行分析。结果表明:(1) 2000-2009年青海省植被覆盖呈明显增加趋势为0.018/10 a
远快于三北防护林工程区1982-2006年植被覆盖平均增速0.007/10 a; (2) 2000-2009年青海省植被恢复具有阶段性
"退耕还林还草"实施前6 a
植被覆盖呈现快速上升
2005年后呈波动下降趋势; (3)青海省植被恢复以轻微改善为主(32.66%)
中度改善次之(13.32%)
明显改善区主要分布在柴达木盆地东南边缘、青海湖盆地、茶卡-共和盆地、河湟谷地及黄南低地; (4)青海省植被呈退化趋势区域比重为18.40%
主要分布于青南高原三江源地区和祁连山中东段;(5)青海省2000-2009年植被稳定性存在明显地域差异。空间格局主要表现为"东南波动
西北稳定
高原温带波动
高原寒带、亚寒带稳定"。青海东部中低山地、丘陵、盆地地区变化幅度最为明显。
In order to monitor the dynamic variation of vegetation in Qinghai Province
based on the MODIS-NDVI data from 2000 to 2009
characteristics of spatial and temporal variation were analyzed using statistical methods such as linear trend analysis and standard deviation. Results show that:(1) From 2000 to 2009
vegetation of the study area was improved progressively
with a linear tendency of 0.018/10 a which was faster than the growth rate of the Three North Shelter Forest Program(0.007/10 a) from 1982 to 2006. (2) Vegetation restoration experienced several stages
a rapid increase in vegetation coverage during the first five years of "Grain-for-Green" project and a significantly fluctuated decline after 2005. (3) Slight improvement(32.66%) accounted for the largest proportion of vegetation restoration
followed by moderate improvement(13.32%)
and the significant improvement area was mainly distributed in the southeast edge of the Qaidam Basin
Qinghai Lake basin
Chaka-Gonghe basin
Hehuang Valley and the south Yellow River lowland. (4) The proportion of degradation tendency was 18.40%
which was distributed in the three rivers headwater and the eastern section of the Qilian Mountain. (5) Vegetation stability manifested significant regional difference
which was low in southeast and temperate zones
but high in northwest
frigid and sub-frigid zones. The changing magnitude was most obvious in the low mountains
hills and basins in eastern Qinghai Province.
国家林业局.第五次中国荒漠化和沙漠化公报[Z].2011.
王涛,吴薇,薛娴,等.近50年来中国北方沙漠化土地的时空变化[J].地理学报,2004,59(2):203-212.
王涛,陈广庭,赵哈林,等.中国北方沙漠化过程及其防治研究的新进展[J].中国沙漠,2006,26(4):507-516.
许端阳,李春蕾,庄大方,等.气候变化和人类活动在沙漠化过程中相对作用评价综述[J].地理学报,2011,66(1):68-76.
黄森旺,李晓松,吴炳方,等.近25年三北防护林工程区土地退化及驱动力分析[J].地理学报,2012,67(5):589-598.
李辉霞,刘国华,傅伯杰.基于NDVI的三江源地区植被生长对气候变化和人类活动的响应研究[J].生态学报,2011,31(19):5495-5504.
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.
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.
董立新,王文科,孔金玲,等.黄河上游玛多县生态环境变化遥感监测及成因分析[J].水土保持通报,2005,25(4):68-72.
孙鸿烈,郑度,姚檀栋,等.青藏高原国家生态安全屏障保护与建设[J].地理学报,2012,67(1):3-12.
张戈丽,欧阳华,张宪洲,等.基于生态地理分区的青藏高原植被覆被变化及其对气候变化的响应[J].地理研究,2010,29(11):2004-2016.
Lean J L, Rind D H. How natural and anthropogenic influences alter global and regional surface temperatures:1889 to 2006[J]. Geophys. Res. Lett., 2008, 35, L18701, doi:10.1029/2008 GL 034864.
王绍武,罗勇,唐国利,等.近10年全球变暖停滞了吗?[J].气候变化研究进展,2010,6(2):95-99.
唐国利,罗勇,黄建斌,等.气候变暖在继续[J].气候变化研究进展,2012,8(4):235-242.
张忠孝.青海地理[M].西宁:青海人民出版社,2004.
马明国,王建,王雪梅.基于遥感的植被年际变化及其与气候关系研究进展[J].遥感学报,2006,10(3):421-431.
宋怡,马明国.基于SPOT VEGETATION数据的中国西北植被覆盖变化分析[J].中国沙漠,2007,27(1):89-93.
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.
王强,张勃,戴声佩,等.基于GIMMS AVHRR NDVI数据的三北防护林工程区植被覆盖动态变化[J].资源科学, 2011,33(8):1613-1620.
李双双,延军平,万佳.近10年陕甘宁黄土高原区植被覆盖时空变化特征[J].地理学报,2012,67(7):960-970.
0
浏览量
1391
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621