Application of multitemporal CBERS/CCD data for evaluating the vegetation change trends in the Lower

来源 :干旱半干旱环境对地观测国际会议 | 被引量 : 0次 | 上传用户:Cecil1119
下载到本地 , 更方便阅读
声明 : 本文档内容版权归属内容提供方 , 如果您对本文有版权争议 , 可与客服联系进行内容授权或下架
论文部分内容阅读
The Tarim River is the principal and recognized longest continental river of the Xinjiang Uygur Autonomous Region in the Peoples Republic of China.The riparian ecosystem in the well-known ‘Green Corridor’ of the lower reach of Tarim river ebbed constantly from 1950s as results of both developing agricultural cropland in the upper,middle and some part of lower reaches of the river and construction of the Dashkol Reservoir by blocking the stream in 1972.In 2000,the “Green Corridor” riparian ecosystem was temporally re-linked to its original water sources by initiating an “emergency ecological water transfusion project” after continuous disruption for 28 years.This paper analysed the process and trends of the vegetation changes during the period of intermittent water transfusion,based on multi-temporal remote sensing data.According to the acquisition time and quality of remote sensing images,the optimal China Brazil Earth Resource Satellite (CBERS) CCD images of each year have been chosen; the land-cover in each year was classified into vegetation and non-vegetation by the SAVI threshold respectively; then the change trajectory of each pixel for was constructed through image calculation between previous classified imageries.Based on the change trends of all potential 64 trajectories were characterized into five trends class as a) stable non-vegetation,b) stable vegetation,c) change into vegetation,d) change into non-vegetation and e)unstable changes.Based on the analysis of the spatial distribution of different change tendencies,and the change process discovered by the change trajectory; integrating the ground investigation,we inferred the vegetation composition during the study period and the reason of change.The result indicated that 7.94% of the study region shows the trends of changing to vegetation,resulted from the growth of herbage and refresh of weakened shrub; and only 2.66% change into non-vegetation; at the same time,10.43% present unstable change,due to the frangibility of vegetation.
其他文献
Tectonic-geomorphological methods are effective in studying crustal deformation in recent geologic time,which gives a link between ongoing tectonic processes and orogenesis.Recent GPS observations hav
Integrated Research on Disaster Risk (IRDR) Programme,co-sponsored by the International Council for Science (ICSU),the International Social Science Council (ISSC),and the United Nations International
Winter drought of wheat in North China is becoming more frequent due to climate change.In the winter of 2008/2009 and 2010/2011,there was serious drought in few parts of the North China Plain.But wint
Existing seismic hazard map (the map of seismic zonation) of the territory of Tajikistan was produced in 1978 (Babaev et al.,1978),renovated in 1984 (Seismic zonation…,1984),and has the seismic hazard
会议
The region from the northeastern margin of the Pamir to the West Kunlun range is an important part of the northwestern Tibetan Plateau,which is surrounded by the Kongur Shan normal fault,Main Pamir Th
会议
This paper looks at the status of earth observation data continuity issues.There are several factors affecting the continuity of global data sets which will impact our ability to monitor global change
As economic development and population increase,there is a severe shortage of water resources in Beijing,which restrict the rapid development of social economy.It is the base of sustainable developmen
Desertification is one of the most serious current environmental challenges in the context of global change and China is among those countries that are most severely affected.One hotspot of desertific
It is promising way to analyze large scale surface energy balance from two source model,which widely used to map local evapotranspiration pattern,detect regional drought and climate change study.Based
Lop Nur Lake was a huge lake located at the eastern end of the Tarim Basin,Xinjiang Uygur Autonomous region,northwest China.According to the aerial photography taken in 1958,there was obvious water ob