福州大学学报(自然科学版)
福州大學學報(自然科學版)
복주대학학보(자연과학판)
JOURNAL OF FUZHOU UNIVERSITY(NATURAL SCIENCE EDITION)
2015年
4期
482-487
,共6页
小波相干%归一化植被指数%环境因子%关联性分析%武夷山
小波相榦%歸一化植被指數%環境因子%關聯性分析%武夷山
소파상간%귀일화식피지수%배경인자%관련성분석%무이산
wavelet coherency%normalized difference vegetation index%environmental factors%corre-lation analysis%Wuyi Mountain
为了揭示武夷山世界遗产地植被覆盖与其影响因素的空间尺度变化规律,利用武夷山世界遗产地2009年的TM遥感影像及DEM、居民地、道路、河流等数据,运用小波相干分析方法研究该地区两条样带上归一化植被指数( NDVI)与高程、坡度、坡向、距最近居民点距离、距最近道路距离以及距最近河流距离等环境因子的相关性。研究表明, NDVI与环境因子的关系随尺度变化,在大中尺度上NDVI与海拔、坡度、坡向显著相关,其中海拔是主导控制因子;海拔600 m以下, NDVI与海拔为正相关,而600 m以上, NDVI与海拔的关系在东南季风的迎风坡为正相关,背风坡为负相关,海拔大于1200 m的区域为负相关。
為瞭揭示武夷山世界遺產地植被覆蓋與其影響因素的空間呎度變化規律,利用武夷山世界遺產地2009年的TM遙感影像及DEM、居民地、道路、河流等數據,運用小波相榦分析方法研究該地區兩條樣帶上歸一化植被指數( NDVI)與高程、坡度、坡嚮、距最近居民點距離、距最近道路距離以及距最近河流距離等環境因子的相關性。研究錶明, NDVI與環境因子的關繫隨呎度變化,在大中呎度上NDVI與海拔、坡度、坡嚮顯著相關,其中海拔是主導控製因子;海拔600 m以下, NDVI與海拔為正相關,而600 m以上, NDVI與海拔的關繫在東南季風的迎風坡為正相關,揹風坡為負相關,海拔大于1200 m的區域為負相關。
위료게시무이산세계유산지식피복개여기영향인소적공간척도변화규률,이용무이산세계유산지2009년적TM요감영상급DEM、거민지、도로、하류등수거,운용소파상간분석방법연구해지구량조양대상귀일화식피지수( NDVI)여고정、파도、파향、거최근거민점거리、거최근도로거리이급거최근하류거리등배경인자적상관성。연구표명, NDVI여배경인자적관계수척도변화,재대중척도상NDVI여해발、파도、파향현저상관,기중해발시주도공제인자;해발600 m이하, NDVI여해발위정상관,이600 m이상, NDVI여해발적관계재동남계풍적영풍파위정상관,배풍파위부상관,해발대우1200 m적구역위부상관。
Using wavelet coherency analysis, this paper studies the relationships between normalized difference vegetation index ( NDVI ) and environmental factors at world heritage of Wuyi Mountain. This factors are elevation, slope, aspect, distance to the nearest resident, distance to the nearest road and distance to the nearest river in two transects based on data of TM remote sensing image, DEM, settlements, roads and rivers in 2009.The results show that the relationships between NDVI and envi-ronmental factors change as scale changes.At medium and large scale, NDVI is significantly correla-ted with elevation, aspect, slope.Thus elevation is the dominant controlling factors on the vegetation cover.There is positive correlation between NDVI and elevation below the altitude of 600 m, and a-bove 600 m, the relationships between NDVI and elevation are positive in the windward side of the southeast monsoon and negative in the leeward side, but inversely above 1 200 m.