厦门理工学院学报
廈門理工學院學報
하문리공학원학보
Journal of Lujiang University
2015年
5期
59-63,88
,共6页
聂芹%满旺%李宗梅%黄于同
聶芹%滿旺%李宗梅%黃于同
섭근%만왕%리종매%황우동
植被覆盖%气象因子%博湖流域%多尺度
植被覆蓋%氣象因子%博湖流域%多呎度
식피복개%기상인자%박호류역%다척도
vegetation cover%meteorological factors%Bostent Lake basin%multi-time scale
基于SPOT-Vegetation 10 d产品数据及新疆巴音布鲁克气象站观测资料,运用小波分析与统计分析相结合的方法,从多时间尺度研究博湖流域1998—2009年间植被覆盖的非线性变化趋势,以及植被覆盖对气候变化的多尺度响应。结果表明: NDVI序列表现出具有时间尺度依赖性的非线性变化趋势,时间尺度从20 d到40 d、80 d、160 d, NDVI变化的周期性逐渐显现,最后到320 d尺度上NDVI变化趋势彰显出来;旬平均气温和旬降水在各个尺度上也呈现出与NDVI一致的变化趋势;从6个时间尺度看, NDVI与平均气温、降水之间存在着显著的线性相关关系,在小于40 d的时间尺度上,气温对NDVI的影响更大,而在80~160 d尺度上,降水的影响更强。
基于SPOT-Vegetation 10 d產品數據及新疆巴音佈魯剋氣象站觀測資料,運用小波分析與統計分析相結閤的方法,從多時間呎度研究博湖流域1998—2009年間植被覆蓋的非線性變化趨勢,以及植被覆蓋對氣候變化的多呎度響應。結果錶明: NDVI序列錶現齣具有時間呎度依賴性的非線性變化趨勢,時間呎度從20 d到40 d、80 d、160 d, NDVI變化的週期性逐漸顯現,最後到320 d呎度上NDVI變化趨勢彰顯齣來;旬平均氣溫和旬降水在各箇呎度上也呈現齣與NDVI一緻的變化趨勢;從6箇時間呎度看, NDVI與平均氣溫、降水之間存在著顯著的線性相關關繫,在小于40 d的時間呎度上,氣溫對NDVI的影響更大,而在80~160 d呎度上,降水的影響更彊。
기우SPOT-Vegetation 10 d산품수거급신강파음포로극기상참관측자료,운용소파분석여통계분석상결합적방법,종다시간척도연구박호류역1998—2009년간식피복개적비선성변화추세,이급식피복개대기후변화적다척도향응。결과표명: NDVI서렬표현출구유시간척도의뢰성적비선성변화추세,시간척도종20 d도40 d、80 d、160 d, NDVI변화적주기성축점현현,최후도320 d척도상NDVI변화추세창현출래;순평균기온화순강수재각개척도상야정현출여NDVI일치적변화추세;종6개시간척도간, NDVI여평균기온、강수지간존재착현저적선성상관관계,재소우40 d적시간척도상,기온대NDVI적영향경대,이재80~160 d척도상,강수적영향경강。
Based on SPOT-Vetetation 10 d images and meteorological data from Bayanbulak Meteorological Station this paper investigated the vegetation dynamic and its response to climate factors at different time scales during 1998-2009 in Bostent Lake Basin Xinjiang using wavelet analysis and statistical analysis. The main findings are as follows the NDVI time series presented nonlinear patterns that varied with timescales. Its periodicity manifested itself more and more with the increase of time scale from 20 d to 40 d to 80 d to 160 d until it finally stabilized at the 320 -day scale. The average temperature and precipitation in 10 days both presented the approximately coincident nonlinear patterns with that of NDVI. This further supported the significant relationship between NDVI and these two climate factors from the morphologically similar view. Temperature has greater impact on NDVI with time scale less than 40 days while precipitation has stronger influence on NDVI on time scales between 80 to 160 d.