地理学报 ›› 1998, Vol. 53 ›› Issue (s1): 52-60.doi: 10.11821/xb1998s1007

• 论文 • 上一篇    下一篇

基于季相及经度特征的中国土地覆盖变化遥感研究

布和敖斯尔1, 刘纪远1, 吴祖南2   

  1. 1. 中国科学院遥感应用研究所,北京100101;
    2. 香港城市大学物理与材料学系,香港九龙堂
  • 收稿日期:1997-06-05 修回日期:1998-09-10 出版日期:1998-12-15 发布日期:1998-12-15
  • 作者简介:布和敖斯尔,男,1964年生,副研究员。1995年8月毕业于中国科学院地理研究所资源与环境信息系统国家重点实验室自然地理专业博士。1995年8月至1997年8月在中国科学院遥感应用研究所博士后流动站做博士后研究,现在中国科学院遥感应用研究所工作,主要从事了土地覆盖变化的遥感研究。在国内外发表“Study on the distribution model of Land-cover change in China using remotely sensed data"(在澳大利亚Griffith大学IGU一LUCC会议上发表〕等10余篇论文。
  • 基金资助:

    国家自然科学基金青年基金资助项目,编号49701017

STUDY ON LAND COVER CHANGE IN CHINA BASED ON SEASONAL & LONGITUDINAL CHARACTERISTICS USING REMOTELY SENSED DATA

Buheaosier1, Liu Jiyuan1, C. N.Ng2   

  1. 1. Institute of Remote Sensing Applications, Chinese Academy of Sciences, Beijing 100101;
    2. Department of Physics and MATERIALS Sciences, City University of Hong Kong
  • Received:1997-06-05 Revised:1998-09-10 Online:1998-12-15 Published:1998-12-15
  • Supported by:

    Supported by National Natural Science Foundation of China, No.49701017

摘要: 本研究从南到北,在季风区域沿经线选择了3个典型样地;从东到西,在北方草原区域(非季风区域)沿纬线方向选择了;个典型区域,用其每周一次接收的共两年的NOAAAVHRR图像和已有陆地卫星数据(仅在环境背景值计算时使用过)计算了每月一次最大的NDVI值,并输入同期月平均的气温、降水和风力等环境参数,在季风区域和非季风区域间进行比较,研究了环境参数与NDVI值相关关系和各样地土地覆盖变化的脆弱季相及其分布模型。

关键词: 土地覆盖变化, 季相及经度特征, 遥感数据

Abstract: In this study, three test sites with the same longitude, have been selected form south to north in wetland area of East China. Five test sites with the same latitude have been selected in arid or semi-arid area of north China, (the former three test sites located in Eastern Asian Mon-soon Area and the latter five test sites located in transition area or Non-Monsoon Area). Pro-duction of 24-month time series of one month maximum NDVI composites have been accom-plished based on NOAA AVHRR and Landsat-TM Data. Average temperature, precipitation and wind-speed data in each average of the month to be synchronous have also been put into computer for analyzing the dynamically correlated model of driving forces of land-cover changes. Conclusion have been made that land-cover change in China has distinct seasonal fragileness in each test site and their relationship has been found.In the study, we draw the following conclusion:(1)Vegetation is the connection of soil, atmosphere and precipitation.When using vegeta-tion as an indicator of land cover change, not only seasonal but also spatial change have been found in the land cover change. In addition, some unstable phase have also been identified.We conclude that the unstable phase in land cover was related to the seasonal and longitudinal change.(2)The zone and coastal plain of east of China belong to East Asian monsoon. The climateis rather wet. The correlation between NDVI and temperature is obvious. But the correlation between NDVI and precipitation is not so good. Therefore, we conclude that in a region of high precipitation, temperature is the key affecting factor for growth of vegetation.(3) In northern China, the Daxinganling forest area, the typical grassland area and arid desert area almost lie on the same latitude. From east to west, the land cover types are forest, forest-grassland, typical grassland, desert-grassland and arid desert. In the line, as the distance from coastal line increase. the monthly average NDVI value depend more on precipitation. Thus, compared with temperature, precipitation is the key affecting factor for vegetation growth arid area.( 4) From south to north, under the limitation of temperature. the deviation of average NDVI is not obvious. However, the seasonal deviation is high. From east to west, under the limitation of precipitation, the regional deviation of NDVI coincide with the productivity of veg-etation. It implies that temperature affect the budding, flowering, fruiting of vegetation. On the other hand, precipitation affect the productivity of vegetation.(5)Wind is one of the driving force causing desertification in dry and semi-dry region. The period of lasting of strong wind seems to be coincident with the degradation of vegetation for each test sites. In contrast, when the cover of vegetation was at maximum, wind speed was found to be minimum, because of the inverse relationship between wind speed and NDVI, de-sertifiction and land degradation happen in the grassland and cultivation land in northern China. Some research show that desertification and land degradation happened on winter and spring which coincide with the unstable stage found in our study.(6)Our study shows further that desertification and land degradation in northern China is caused by natural factor, it also relates to the seasonal degradation of vegetation. The most suitable method to prevent land degradation is to build cultivates land or grassland.

Key words: land cover change, seasonal &, - longitudinal characteristics, remotely sensed data

中图分类号: 

  • X144