气候与环境研究
氣候與環境研究
기후여배경연구
CLIMATIC AND ENVIRONMENTAL RESEARCH
2013年
2期
156-164
,共9页
王筝%赵天保%侯美亭%延晓冬
王箏%趙天保%侯美亭%延曉鼕
왕쟁%조천보%후미정%연효동
植被覆盖变化%增强型植被指数(EVI)%遥感数据
植被覆蓋變化%增彊型植被指數(EVI)%遙感數據
식피복개변화%증강형식피지수(EVI)%요감수거
Vegetation change%Enhanced Vegetation Index (EVI)%Satellite data
利用增强型植被指数(EVI)作为植被活动的指标,用MODIS-EVI时间序列数据定量分析了2000~2009年间中国北方地区EVI的变化规律.结果表明:1)21世纪初中国北方地区植被覆盖总体改善,局部退化,10年来区域年平均EVI增加5.97%;2)逐季节平均EVI均呈现上升趋势,春季、秋季上升幅度小,夏季、冬季上升幅度大;3)中国北方地区植被稀少的区域呈减少趋势,同时单位面积EVI增加,植被生长更加茂盛;4)中国北方地区EVI变化空间异质性大.东北平原、华北平原、黄土高原和新疆农业区显著增加,东北和西部部分地区植被退化.
利用增彊型植被指數(EVI)作為植被活動的指標,用MODIS-EVI時間序列數據定量分析瞭2000~2009年間中國北方地區EVI的變化規律.結果錶明:1)21世紀初中國北方地區植被覆蓋總體改善,跼部退化,10年來區域年平均EVI增加5.97%;2)逐季節平均EVI均呈現上升趨勢,春季、鞦季上升幅度小,夏季、鼕季上升幅度大;3)中國北方地區植被稀少的區域呈減少趨勢,同時單位麵積EVI增加,植被生長更加茂盛;4)中國北方地區EVI變化空間異質性大.東北平原、華北平原、黃土高原和新疆農業區顯著增加,東北和西部部分地區植被退化.
이용증강형식피지수(EVI)작위식피활동적지표,용MODIS-EVI시간서렬수거정량분석료2000~2009년간중국북방지구EVI적변화규률.결과표명:1)21세기초중국북방지구식피복개총체개선,국부퇴화,10년래구역년평균EVI증가5.97%;2)축계절평균EVI균정현상승추세,춘계、추계상승폭도소,하계、동계상승폭도대;3)중국북방지구식피희소적구역정감소추세,동시단위면적EVI증가,식피생장경가무성;4)중국북방지구EVI변화공간이질성대.동북평원、화북평원、황토고원화신강농업구현저증가,동북화서부부분지구식피퇴화.
@@@@Moderate-resolution Imaging Spectroradiometer (MODIS)–Enhanced Vegetation Index (EVI) data reported during 2000–2009 have been analyzed to study recent trends in vegetation greenness over the northern part of China at the beginning of the 21st century. The results showed that the afforestation area was larger than the degraded area in the northern part of China during the last 10 years, and the regional total mean annual EVI increased by 5.97%. Seasonal EVI increased significantly, and trends in summer and winter were larger than those in spring and autumn. The sparsely vegetated area declined, unit area EVI increased, and vegetation activity rose during the study period. In addition, EVI changes in the northern part of China exhibited relatively large spatial heterogeneity. The Northeast China Plain, North China Plain, Loess Plateau, and Xinjiang agriculture regions experienced marked increases, and part of Northeast China and West China experienced declining trends. Such patterns are attributed primarily to regional climate changes and human activities such as ecological construction and urbanization.