首页 | 本学科首页   官方微博 | 高级检索  
   检索      

2006-2016年岷江上游植被覆盖度时空变化及驱动力
引用本文:祝聪,彭文甫,张丽芳,罗瑶,董永波,王梅芳.2006-2016年岷江上游植被覆盖度时空变化及驱动力[J].生态学报,2019,39(5):1583-1594.
作者姓名:祝聪  彭文甫  张丽芳  罗瑶  董永波  王梅芳
作者单位:四川师范大学地理与资源科学学院, 成都 610068;四川师范大学 西南土地资源评价与监测教育部重点实验室, 成都 610068,四川师范大学地理与资源科学学院, 成都 610068;四川师范大学 西南土地资源评价与监测教育部重点实验室, 成都 610068,四川师范大学地理与资源科学学院, 成都 610068;四川师范大学 西南土地资源评价与监测教育部重点实验室, 成都 610068,四川师范大学地理与资源科学学院, 成都 610068;四川师范大学 西南土地资源评价与监测教育部重点实验室, 成都 610068,四川师范大学地理与资源科学学院, 成都 610068;四川师范大学 西南土地资源评价与监测教育部重点实验室, 成都 610068,贵州师范大学地理与环境科学学院, 贵阳 550001
基金项目:国家自然科学基金项目(No.41371125);教育部人文社科研究规划基金项目(No.17YJA850007)
摘    要:基于MODIS NDVI遥感数据,采用像元二分模型估算岷江上游植被覆盖度,运用一元线性回归分析和稳定性分析方法,研究2006-2016年岷江上游植被覆盖度时空变化格局及稳定性,并分段讨论2008年"5.12汶川地震"对岷江上游植被的破坏程度以及震后植被恢复情况,利用地理探测器模型对岷江上游植被覆盖度影响因子及影响力进行探测,分析岷江上游植被覆盖度变化驱动力。结果表明:(1)2006-2016年岷江上游植被覆盖整体状况良好,植被覆盖总体情况较为稳定,多年平均植被覆盖度为0.79,植被覆盖度大于0.8的区域占整个岷江上游地区面积的69%。(2)2008年"5.12汶川地震"给整个岷江上游植被造成了严重的破坏,植被覆盖度退化区域面积为14013.41 km2,占整个岷江上游面积的57%,2008-2016年岷江上游植被恢复状况良好,植被覆盖度改善区域面积为17390.69 km2,占整个岷江上游面积的71%,岷江上游植被覆盖度已经超过震前水平。(3)岷江上游植被覆盖度主要受海拔、气温、土壤类型、降水4个因子的影响,其解释力均在40%以上;地貌类型、植被类型的解释力在20%-40%之间;坡度、坡向的解释力均小于1%。

关 键 词:岷江上游  植被覆盖度  像元二分模型  时空变化  地理探测器
收稿时间:2018/5/4 0:00:00
修稿时间:2019/1/11 0:00:00

Study of temporal and spatial variation and driving force of fractional vegetation cover in upper reaches of Minjiang River from 2006 to 2016
ZHU Cong,PENG Wenfu,ZHANG Lifang,LUO Yao,DONG Yongbo and WANG Meifang.Study of temporal and spatial variation and driving force of fractional vegetation cover in upper reaches of Minjiang River from 2006 to 2016[J].Acta Ecologica Sinica,2019,39(5):1583-1594.
Authors:ZHU Cong  PENG Wenfu  ZHANG Lifang  LUO Yao  DONG Yongbo and WANG Meifang
Institution:The Institute of Geography and Resources Science, Sichuan Normal University, Chengdu 610068, China;Key Lab of Land Resources Evaluation and Monitoring in Southwest, Ministry of Education, Sichuan Normal University, Chengdu 610068, China,The Institute of Geography and Resources Science, Sichuan Normal University, Chengdu 610068, China;Key Lab of Land Resources Evaluation and Monitoring in Southwest, Ministry of Education, Sichuan Normal University, Chengdu 610068, China,The Institute of Geography and Resources Science, Sichuan Normal University, Chengdu 610068, China;Key Lab of Land Resources Evaluation and Monitoring in Southwest, Ministry of Education, Sichuan Normal University, Chengdu 610068, China,The Institute of Geography and Resources Science, Sichuan Normal University, Chengdu 610068, China;Key Lab of Land Resources Evaluation and Monitoring in Southwest, Ministry of Education, Sichuan Normal University, Chengdu 610068, China,The Institute of Geography and Resources Science, Sichuan Normal University, Chengdu 610068, China;Key Lab of Land Resources Evaluation and Monitoring in Southwest, Ministry of Education, Sichuan Normal University, Chengdu 610068, China and The Institute of Geography and Environmental Science, Guizhou Normal University, Guiyang 550001, China
Abstract:Based on moderate resolution imaging spectroradiometer (MODIS) normalized difference vegetation index (NDVI) remote sensing data, the fractional vegetation cover in the upper reaches of Minjiang River was estimated using a pixel dichotomy model. Furthermore, the temporal and spatial variation pattern and stability of the fractional vegetation cover in the upper reaches of Minjiang River from 2006 to 2016 were studied using univariate linear regression and stability analyses. The damage degree of the vegetation in the upper reaches of Minjiang River and the vegetation restoration after the earthquake are discussed in sections. The influencing factors of fractional vegetation cover in the upper reaches of Minjiang River were detected using the Geographic detector model. The driving force of vegetation cover change in the upper reaches of Minjiang River was analyzed. The results showed the following. (1) The fractional vegetation cover in the upper reaches of Minjiang River from 2006 to 2016 was good, and the overall fractional vegetation cover was stable. The annual average fractional vegetation cover was 0.79, and the area with fractional vegetation cover > 0.8 accounted for 69% of the total area of the upper reaches of the Minjiang River. (2) The "5.12 Wenchuan earthquake" in 2008 seriously damaged the vegetation in the upper reaches of Minjiang River. The degraded area of fractional vegetation cover was 14013.41 km2, which accounted for 57% of the total area of the upper reaches of the Minjiang River.The vegetation restoration condition in the upper reaches of Minjiang River from 2008 to 2016 was good.The area of fractional vegetation cover improvement was 17390.69 km2, which accounted for 71% of the total area of the upper reaches of the Minjiang River. The fractional vegetation cover in the upper reaches of Minjiang River exceeded the pre-earthquake level. (3) The fractional vegetation cover in the upper reaches of Minjiang River was mainly affected by four factors:altitude, temperature, agrotype, and precipitation. Its explanatory power was > 40%, the interpretation of the Geomorphic type and vegetation types was between 20% and 40%, and the interpretation of slope and aspect was < 1%.
Keywords:upper reaches of Minjiang River  fractional vegetation cover  pixel dichotomy model  space-time variation  geographic detector
点击此处可从《生态学报》浏览原始摘要信息
点击此处可从《生态学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号