桂林理工大学学报
桂林理工大學學報
계림리공대학학보
JOURNAL OF GUILIN UNIVERSITY OF TECHNOLOGY
2014年
2期
260-265
,共6页
TM/ETM+%漓江流域%像元二分模型%植被覆盖度
TM/ETM+%巑江流域%像元二分模型%植被覆蓋度
TM/ETM+%리강류역%상원이분모형%식피복개도
TM/ETM+%Lijiang river basin%dimidiate pixel model%vegetation coverage
为研究漓江流域近15年植被覆盖度变化情况,以1991、2000、2006年3个时相的TM/ETM+影像为基础,采用基于归一化植被指数(NDVI)的像元二分模型对漓江流域植被覆盖度进行估算,分析了植被覆盖度时空变化特征;结合研究区地质数据,进一步分析地质条件对植被覆盖度的影响。结果表明:①受气候和人类活动的影响,1991-2000年漓江流域植被覆盖度有所增加,表现为高和较高植被覆盖区面积增加,中度、较低和低植被覆盖区面积减少;2000-2006年漓江流域植被覆盖度略有降低,表现为高植被覆盖区面积减少,较高和中度植被覆盖区增加,较低和低植被覆盖区面积减少;②由于地质条件的影响,非岩溶区的平均植被覆盖度高于岩溶区,两者的变化趋势与流域整体变化基本一致;③从空间分布上看,1991-2006年漓江流域植被覆盖度的变化较显著。
為研究巑江流域近15年植被覆蓋度變化情況,以1991、2000、2006年3箇時相的TM/ETM+影像為基礎,採用基于歸一化植被指數(NDVI)的像元二分模型對巑江流域植被覆蓋度進行估算,分析瞭植被覆蓋度時空變化特徵;結閤研究區地質數據,進一步分析地質條件對植被覆蓋度的影響。結果錶明:①受氣候和人類活動的影響,1991-2000年巑江流域植被覆蓋度有所增加,錶現為高和較高植被覆蓋區麵積增加,中度、較低和低植被覆蓋區麵積減少;2000-2006年巑江流域植被覆蓋度略有降低,錶現為高植被覆蓋區麵積減少,較高和中度植被覆蓋區增加,較低和低植被覆蓋區麵積減少;②由于地質條件的影響,非巖溶區的平均植被覆蓋度高于巖溶區,兩者的變化趨勢與流域整體變化基本一緻;③從空間分佈上看,1991-2006年巑江流域植被覆蓋度的變化較顯著。
위연구리강류역근15년식피복개도변화정황,이1991、2000、2006년3개시상적TM/ETM+영상위기출,채용기우귀일화식피지수(NDVI)적상원이분모형대리강류역식피복개도진행고산,분석료식피복개도시공변화특정;결합연구구지질수거,진일보분석지질조건대식피복개도적영향。결과표명:①수기후화인류활동적영향,1991-2000년리강류역식피복개도유소증가,표현위고화교고식피복개구면적증가,중도、교저화저식피복개구면적감소;2000-2006년리강류역식피복개도략유강저,표현위고식피복개구면적감소,교고화중도식피복개구증가,교저화저식피복개구면적감소;②유우지질조건적영향,비암용구적평균식피복개도고우암용구,량자적변화추세여류역정체변화기본일치;③종공간분포상간,1991-2006년리강류역식피복개도적변화교현저。
In order to study the vegetation coverage changes of the Lijiang river basin in 15 years,with Landsat TM/ETM+data of 1991,2000 and 2006 as data sources,by dimidiate pixel model based on NDVI,the vege-tation coverage of the Lijiang river basin is evaluated and characteristics of temporal-spatial changes are analyzed in past 15 years.From the geological data in the study area,influences of the geological conditions to vegeta-tion coverage are analyzed.Results are described in three aspects:①Because of the climate and human activi-ties,the vegetation coverage in the Lijiang river basin got a rise in 1991 -2000.The area of high and higher vegetation coverage districts increased,while that of middle,low and lower vegetation coverage districts de-creased.Vegetation coverage got a decrease in 2000-2006.The area of high vegetation coverage districts de-creased,higher and middle vegetation coverage districts increased,while that low and lower vegetation cover-age districts decreased;②Due to the influence of the geological conditions,the average vegetation coverage in non-karst area is higher than that in karst area,but the overall trend consistent with changes in the Lijiang river basin;③Spatial distribution of vegetation coverage changes are significant in the Lijiang river basin during 1991 -2006.