globalchange  > 气候变化与战略
CSCD记录号: CSCD:5811991
论文题名:
喀斯特地区不同植被类型NDVI 变化及驱动因素分析以贵州为例
其他题名: The Analysis of the Difference Vegetation Variation and Driver Factors on NDVI Change in Karst Region: A Case on Guizhou
作者: 马士彬1; 安裕伦1; 杨广斌1; 张勇荣2
刊名: 生态环境学报
ISSN: 1674-5906
出版年: 2016
卷: 25, 期:7, 页码:237-242
语种: 中文
中文关键词: 喀斯特 ; 植被类型 ; 气候变化 ; 人为作用
英文关键词: NDVI ; karst ; vegetation type ; NDVI ; climate change ; human factors
WOS学科分类: REMOTE SENSING
WOS研究方向: Remote Sensing
中文摘要: 以SPOT-VEG NDVI数据为基础结合植被类型、气象和石漠化数据,通过NDVI变化趋势倾斜率及逐像元相关分析,分析不同植被类型NDVI变化趋势及驱动因素。结果表明,(1)20002013年贵州省植被NDVI呈增加趋势,其中20002007年为快速增加期,变化率为0.25/10 a(r~2=0.923);20082013年增速减缓,变化率为0.02/10 a(r~2=0.381)。(2)人工植被NDVI增速最大为0.17/10 a(r~2=0.813),灌丛灌草丛次之,为0.13/10 a(r~2=0.85),乔木类植被(常绿阔叶林、落叶阔叶林、常绿和落叶阔叶混交林、针叶林、针阔混交林)和竹林的NDVI基本保持不变。(3)贵州省气候变化呈不显著冷干趋势,其中降水对植被变化的影响力大于温度,植被NDVI与年降水量和年均温均呈现不显著负相关关系。(4)人工植被与降水和气温的逐像元分析中,显著负相关比重较大,分别达到20%和15%;灌丛灌草丛的显著负相关比重也大于正相关,分别达到16%和17%;乔木类植被则相反,显著正相关比重较大,其中河谷季雨林达到48%。(5)人类活动强度较高的区域,NDVI变化与城市扩展、植树造林及石漠化治理面积有显著正相关性。由此得出,在人类活动强度较大的区域,如城镇周边、生态治理与修复措施的实施区域,植被变化主要受人为作用制约;但当人类活动或干扰较少时,气候变化限制植被的变化趋势。所以,从宏观角度分析植被变化与气候变化的关系时,必须权衡人为作用和气候变化对植被变化的影响。
英文摘要: In order to indicate the trend of vegetation change and the driving factors in Karst region, the slope of normalized difference value index (NDVI) change trend and the correlation analysis of pixel by pixel were used to analyze the NDVI change trend and driving factors of different vegetation based on the SPOT-VEG NDVI data and combined with vegetation type, meteorological data and rocky desertification data. The results showed that: (1) The NDVI of Guizhou Province presented an increase trend from 2000 to 2013, in which it presented a significant increase during 2000 to 2007 and the ratio of change was 0.25/10 a (r~2=0.923); while the growth slowed from 2008 to 2013 and the ratio of change was 0.02/10 a (r~2=0.381). (2) The NDVI of artificial vegetation grew fastest with the speed of 0.17/10 a (r~2=0.813), the secondly was the shrub land and grass with the speed of 0.13/10 a (r~2=0.85). The NDVI of trees and bamboo forest was almost invariant. (3) The climate change in Guizhou was dry-cool and precipitation influenced more than temperature. There was no significant negative correlation between NDVI and the annual precipitation and the annual mean temperature. (4) By pixel and pixel analyzing the artificial vegetation, precipitation and temperature, the ratio of negative correlation was bigger which reached to 20% and 15% respectively. The negative correlation ratio of shrub land and grass was bigger than positive correlation which reached to 16% and 17% respectively. On contrast, the tree's positive correlation ratio was bigger in which that of river valley monsoon forest reached to 48%. And (5) in those areas of higher intensity human activities such as urban periphery and rocky desertification management regions, the NDVI change was significant correlated with urban expanding, afforestation and rocky desertification restoration areas. Therefore, in these areas, the vegetation change was mainly attributed to human activities. However when human activities induced less, the climate change restricted the trend of vegetation change. To analyze the relationship between vegetation change and the climate change from the macroscopic angle, the influence weight of human action and climate change must be identified.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/151264
Appears in Collections:气候变化与战略

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作者单位: 1.贵州师范大学地理与环境科学学院, 贵州省山地资源与环境遥感应用重点实验室, 贵阳, 贵州 550001, 中国
2.六盘水师范学院环境与资源科学系, 六盘水, 贵州 553004, 中国

Recommended Citation:
马士彬,安裕伦,杨广斌,等. 喀斯特地区不同植被类型NDVI 变化及驱动因素分析以贵州为例[J]. 生态环境学报,2016-01-01,25(7):237-242
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