资源与生态学报(英文版)
資源與生態學報(英文版)
자원여생태학보(영문판)
JOURNAL OF RESOURCES AND ECOLOGY
2014年
1期
53-59
,共7页
王强%张勃%张志强%张喜风%戴声佩
王彊%張勃%張誌彊%張喜風%戴聲珮
왕강%장발%장지강%장희풍%대성패
NDVI%三北防护林工程区%时空变化%相关分析%动态研究%中国北部
NDVI%三北防護林工程區%時空變化%相關分析%動態研究%中國北部
NDVI%삼북방호림공정구%시공변화%상관분석%동태연구%중국북부
NDVI%Three-North Shelterbelt Program (TNSP)%spatio-temporal changes%correlation analysis%dynamic study%northern China
本文基于1982-2006年连续25年的GIMMS AVHRR NDVI植被覆盖指数,采用了最大化NDVI均值法、与气温及降水变化的相关性和一元线性回归趋势分析法,对中国三北防护林工程区连续25年的植被覆盖时空变化特征进行了动态变化研究。结果表明:(1)近25年来,研究区植被NDVI平均值总体呈缓慢上升趋势,增速为每10年0.007;(2)研究区植被和气温、降水整体呈正相关关系,植被与降水正相关面积明显大于植被与气温正相关面积,说明降水是研究区植被生长的关键因子;(3)1982-2006年,研究区植被覆盖增加的区域主要分布在大兴安岭中、南部,小兴安岭中部,长白山东北段,燕山,辽西低山丘陵区,阿尔泰山,天山,祁连山东段,西北荒漠区东部和黄土高原丘陵沟壑区南部等;植被覆盖减少的区域主要是在大兴安岭两侧,呼伦贝尔高原西部,三江平原北部,科尔沁沙地南端,西北荒漠区南部和黄土高原丘陵沟壑区北部等。
本文基于1982-2006年連續25年的GIMMS AVHRR NDVI植被覆蓋指數,採用瞭最大化NDVI均值法、與氣溫及降水變化的相關性和一元線性迴歸趨勢分析法,對中國三北防護林工程區連續25年的植被覆蓋時空變化特徵進行瞭動態變化研究。結果錶明:(1)近25年來,研究區植被NDVI平均值總體呈緩慢上升趨勢,增速為每10年0.007;(2)研究區植被和氣溫、降水整體呈正相關關繫,植被與降水正相關麵積明顯大于植被與氣溫正相關麵積,說明降水是研究區植被生長的關鍵因子;(3)1982-2006年,研究區植被覆蓋增加的區域主要分佈在大興安嶺中、南部,小興安嶺中部,長白山東北段,燕山,遼西低山丘陵區,阿爾泰山,天山,祁連山東段,西北荒漠區東部和黃土高原丘陵溝壑區南部等;植被覆蓋減少的區域主要是在大興安嶺兩側,呼倫貝爾高原西部,三江平原北部,科爾沁沙地南耑,西北荒漠區南部和黃土高原丘陵溝壑區北部等。
본문기우1982-2006년련속25년적GIMMS AVHRR NDVI식피복개지수,채용료최대화NDVI균치법、여기온급강수변화적상관성화일원선성회귀추세분석법,대중국삼북방호림공정구련속25년적식피복개시공변화특정진행료동태변화연구。결과표명:(1)근25년래,연구구식피NDVI평균치총체정완만상승추세,증속위매10년0.007;(2)연구구식피화기온、강수정체정정상관관계,식피여강수정상관면적명현대우식피여기온정상관면적,설명강수시연구구식피생장적관건인자;(3)1982-2006년,연구구식피복개증가적구역주요분포재대흥안령중、남부,소흥안령중부,장백산동북단,연산,료서저산구릉구,아이태산,천산,기련산동단,서북황막구동부화황토고원구릉구학구남부등;식피복개감소적구역주요시재대흥안령량측,호륜패이고원서부,삼강평원북부,과이심사지남단,서북황막구남부화황토고원구릉구학구북부등。
The Shelterbelt Forest System Program in northeast, north and northwest China (the Three-North Shelterbelt Program, TNSP) is the largest ecological reforestation program in the world. TNSP vegetation research has important ecological meaning and profound social and economic signiifcance. Here, spatio-temporal variation in vegetation cover under the TNSP was examined using the NDVI average method, major climatic factors such as temperature and precipitation, and linear regression trend analysis from 1982 to 2006. We found that in the past 25 years, NDVI vegetation in the study area has consistently risen at a rate of 0.007 per decade. Vegetation cover, temperature and precipitation are positively correlated. The area of vegetation associated with precipitation is larger than the area related to temperature;precipitation is the key factor affecting vegetation growth across the TNSP. From 1982 to 2006, regions with improved vegetation cover were found in the central and southern part of the Greater Khingan Mountains, central part of the Lesser Khingan Mountains, northeastern part of the Changbai Mountains, Yanshan Mountians, Western Liaoning Hilly Region, Altai Mountains, Tien Shan Mountains, eastern part of the Qilian Mountains, eastern part of the northwest desert as wel as southern part of the Gul y Region of the Loess Plateau. However, vegetation cover declined on both sides of the Greater Khingan Mountains, western part of the Hulun Buir Plateau, northern part of the Sanjiang Plain, southern part of Horqin Sandy Land, southern part of the northwest desert and northern part of the Gul y Region of the Loess Plateau.