地球信息科学学报
地毬信息科學學報
지구신식과학학보
GEO-INFORMATION SCIENCE
2013年
2期
270-279
,共10页
于海达%杨秀春%徐斌%金云翔%高添%李金亚
于海達%楊秀春%徐斌%金雲翔%高添%李金亞
우해체%양수춘%서빈%금운상%고첨%리금아
锡林郭勒盟%长势%气象因子%滞后效应
錫林郭勒盟%長勢%氣象因子%滯後效應
석림곽륵맹%장세%기상인자%체후효응
Xilin Gol League%vegetation growth%meteorological factors%hysteresis effect
对草原植被长势变化的监测,及其与气候因子关系的分析,对生态环境治理及保护具有重要意义。本文利用250m的MODIS-NDVI数据,构建草原植被长势指数(MGI),分析了16天间隔的植被长势变化及其与降水、气温的相关性和对降水响应的滞后性。得到锡盟3种草原类型区2001-2010年草原长势变化情况,及降水、气温在草原生长不同阶段对草原长势的影响。研究结果表明:(1)在空间上长势东部变化好于中部与西部,北部好于南部;时间上2003年长势最好、2001年长势最差。(2)锡盟内3种草原类型区MGI均与降水关系明显,与气温相关性不显著,降水对温性草原区长势变化的影响最大。(3)在草原生长的不同阶段,影响因子不同,前期与后期主要受气温影响,中期主要受降水影响,草原生长对降水存在明显的滞后,一般在32-48天,同时指出草原植被在不同时间段对降水响应的滞后时间。
對草原植被長勢變化的鑑測,及其與氣候因子關繫的分析,對生態環境治理及保護具有重要意義。本文利用250m的MODIS-NDVI數據,構建草原植被長勢指數(MGI),分析瞭16天間隔的植被長勢變化及其與降水、氣溫的相關性和對降水響應的滯後性。得到錫盟3種草原類型區2001-2010年草原長勢變化情況,及降水、氣溫在草原生長不同階段對草原長勢的影響。研究結果錶明:(1)在空間上長勢東部變化好于中部與西部,北部好于南部;時間上2003年長勢最好、2001年長勢最差。(2)錫盟內3種草原類型區MGI均與降水關繫明顯,與氣溫相關性不顯著,降水對溫性草原區長勢變化的影響最大。(3)在草原生長的不同階段,影響因子不同,前期與後期主要受氣溫影響,中期主要受降水影響,草原生長對降水存在明顯的滯後,一般在32-48天,同時指齣草原植被在不同時間段對降水響應的滯後時間。
대초원식피장세변화적감측,급기여기후인자관계적분석,대생태배경치리급보호구유중요의의。본문이용250m적MODIS-NDVI수거,구건초원식피장세지수(MGI),분석료16천간격적식피장세변화급기여강수、기온적상관성화대강수향응적체후성。득도석맹3충초원류형구2001-2010년초원장세변화정황,급강수、기온재초원생장불동계단대초원장세적영향。연구결과표명:(1)재공간상장세동부변화호우중부여서부,북부호우남부;시간상2003년장세최호、2001년장세최차。(2)석맹내3충초원류형구MGI균여강수관계명현,여기온상관성불현저,강수대온성초원구장세변화적영향최대。(3)재초원생장적불동계단,영향인자불동,전기여후기주요수기온영향,중기주요수강수영향,초원생장대강수존재명현적체후,일반재32-48천,동시지출초원식피재불동시간단대강수향응적체후시간。
Monitoring of grassland vegetation growth is an important part in grassland studies. It is helpful to ac-quire the grassland situation and has significance to environmental management and protection through analysis on the relationship between vegetation growth and meteorological factors. In this research, we obtained the spa-tial distribution of temperature and precipitation by using the ANUSPLIN spatial interpolation method and uses 16days, 250m MODIS-NDVI data to build grassland vegetation growth index MGI (modified growth index), get the changes of Xilin Gol League grassland vegetation growth from 2001 to 2010, analyze the relationships be-tween vegetation growth and temperature/precipitation, and reveal the hysteresis effect of precipitation. The re-sults of this research showed: (1) spatially, the vegetation growth in east part is better than in central part and west part, in north part is better than in south part. Growth in 2003 is better than the other years, and 2001 is the worst year. (2) The correlation between MGI and precipitation of the three grasslands in Xilin Gol is significant, but the relation between MGI and temperature is week. Precipitation can explain 57.5% of desert grassland grow,75.2% of typical steppe grow and 63.7% of meadow prairie grow. So,we can say that vegetation growth per-forms better with the increase of precipitation. (3) Impact factor is different to grassland vegetation growth in dif-ferent phrases, temperature limits the growth during early and late stage, precipitation is the main impact factor to growth during middle stage. Grassland vegetation grow has an obvious lag response, about 32-48 days. And we pointed out that lag response time is different in different grow stage, during early stage is 32days, during middle stage is 48days, and during late stage is 32days.