长江流域资源与环境 >> 2017, Vol. 26 >> Issue (12): 2146-.doi: 10.11870/cjlyzyyhj201712024

• 生态环境 • 上一篇    

基于MODISEVI的2000~2015年重庆植被覆盖季节变化

朱林富1,2,谢世友1,2*,杨华3,马明国1,2   

  1. (1. 西南大学地理科学学院,重庆 400715;2. 西南大学三峡库区生态环境教育部重点实验室,重庆 400715;
    3. 重庆师范大学GIS应用研究重庆市高校重点实验室,重庆 401331)
  • 出版日期:2017-12-20

#br# SEASONAL VARIATION OF VEGETATION COVERAGE BASED ON #br# MODISEVI DATA IN CHONGQING DURING 2000-2015

ZHU Linfu1,2, XIE Shiyou1,2, YANG Hua3, MA Mingguo1,2   

  1. (1. School of Geographic Sciences, Southwest University, Chongqing 400715, China; 2. Key Laboratory of the Three Gorges
     Reservoir Region’s Ecoenvironment, Ministry of Education, Southwest University, Chongqing 400715, China;
    3. Key Laboratory of GIS Application, Chongqing Normal University, Chongqing 401331, China)
  • Online:2017-12-20

摘要: 基于2000~2015年的MODISEVI数据,采用MVC、趋势分析和分布指数法,分析了重庆近16 a来植被的季节变化趋势和空间分布特征。结果表明:(1)植被减少类型冬季比例最高(6.33%),主要分布于受库区蓄水和建设用地扩张影响的河谷、城镇及其周边地区;植被不变类型秋季比例最高(88.23%);植被增加类型春季比例最高(31.50%),主要分布于农业种植的西部丘陵区和中部平行岭谷地区。(2)植被变化类型优势分布区域各异,植被减少主要分布于小于400 m、小于 6°区域,植被增加主要分布于400~1 000 m、6°~15°区域,在大于1 000 m、大于15°区域植被相对稳定。(3)从春季到夏季,植被减少类型向低地形区(< 800 m,< 6°)移动,而植被增加类型则向高地形区(> 800 m,> 6°)移动;从夏季到秋季,植被减少类型向高地形区(> 500 m,> 6°)移动,而植被增加类型则向低地形区(< 500 m,< 6°)移动;从秋季到冬季,植被减少和增加类型均在向高地形区移动,在高地形区,植被减少(> 1 300 m,> 15°)分布强于植被增加(> 500 m,> 6°),在低地形区则是植被减少(< 1 300 m,< 15°)分布弱于植被增加(< 500 m,< 6°)。(4)在坡向的分布上,除了平地区域外,植被变化幅度在北、东、南、西坡向上随季节变化不明显。
关键词: 植被覆盖度;MODISEVI;趋势分析;地形分布指数;季节变化

Abstract: Seasonal change and spatial distribution pattern of vegetation in the Chongqing region was studied using the distribution index method and the MODISEVI data during 2000-2015. The results showed that:(1) vegetation reduction presented the highest proportion(6.33%) in winter. The reduction was mainly distributed in the valleys, towns and surrounding areas influenced by the reservoir construction and builtup expansion. Stable vegetation presented the highest proportion(88.23%) in autumn. Vegetation increase presented the highest proportion(31.50%) in spring. The increase was mainly distributed in the west hilly region and farming areas in the middle parallelism valley.(2) The areas with dominant vegetation changes are different. Vegetation reduction was mainly distributed in the areas below 400 m elevation and below 6° slope. Vegetation increase was mainly distributed in the areas between 400 and 1 000 m elevation and between 6° and 15° slope. Stable vegetation was mainly distributed in the areas above 1 000 m elevation and above 15° slope.(3) From spring to summer, vegetation reduction moved to lower terrains(< 800 m elevation, < 6° slope), but vegetation increase moved to higher terrains(> 800 m elevation, > 6° slope). From summer to autumn, vegetation reduce moved to higher terrains(> 500 m elevation, > 6° slope), but vegetation increase moved to lower terrains(< 500 m elevation, <6° slope). From autumn to winter, vegetation reduction(> 1 300 m elevation, > 15° slope) was stronger than vegetation increase(> 500 m elevation, > 6° slope) on the high terrains. Vegetation reduction(< 1 300 m, <15°) was weaker than vegetation increase(< 500 m, < 6°) on the low terrains.(4) On the distribution of aspect, vegetation change extent did not present significant seasonal variation across the North, East, South and West directions.
Key words:vegetation coverage; MODISEVI; trend analysis; distribution index; seasonal change

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 宋玉芝,秦伯强, 高光. 附着生物对富营养化水体氮磷的去除效果[J]. 长江流域资源与环境, 2009, 18(2): 180 .
[2] 杨 选. 国内外典型水治理模式及对武汉水治理的借鉴[J]. 长江流域资源与环境, 2007, 16(5): 584 .
[3] 刘滨谊,刘 琴. 服务于城市旅游形象的景观规划——以南京市为例[J]. 长江流域资源与环境, 2006, 15(2): 164 -168 .
[4] 李恒鹏,杨桂山,刘晓玫,万荣荣. 流域土地利用变化的长周期水文效应及管理策略[J]. 长江流域资源与环境, 2005, 14(4): 450 -455 .
[5] 梁常德,龙天渝,李继承,刘腊美. 三峡库区非点源氮磷负荷研究[J]. 长江流域资源与环境, 2007, 16(1): 26 -30 .
[6] 廖顺宝,李泽辉. 四川省人口分布与土地利用的关系及人口数据空间化试验[J]. 长江流域资源与环境, 2004, 13(6): 557 -561 .
[7] 吴丰林,周德民,胡金明. 基于景观格局演变的城市湿地景观生态规划途径[J]. 长江流域资源与环境, 2007, 16(3): 368 .
[8] 屈 璠,刘 敏,侯立军,许世远,刘巧梅,欧冬妮. 潮汐循环影响下上覆水环境因子和氮营养盐的变化及其相关关系[J]. 长江流域资源与环境, 2007, 16(3): 345 .
[9] 董林水, 张旭东, 周金星, 李冬雪. 青藏铁路沿线北段植被物种丰富度及盖度的动态变化[J]. 长江流域资源与环境, 2008, 17(4): 551 .
[10] 胡贤辉,张 霞,杨钢桥. 湖北省土地利用结构变化及其驱动机制分析[J]. 长江流域资源与环境, 2008, 17(1): 43 .