气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2015年
2期
103-107
,共5页
唐晓玲%任红玲%王杰%刘珂%王颖
唐曉玲%任紅玲%王傑%劉珂%王穎
당효령%임홍령%왕걸%류가%왕영
主要产粮区%NDVI%遥感监测
主要產糧區%NDVI%遙感鑑測
주요산량구%NDVI%요감감측
Main grain producing area%NDVI(Normalized Difference Vegetation Index)%Remote sensing monito-ring
为了确定作物长势遥感监测的评价指标,利用2000—2012年吉林省 EOS /MODIS 数据,采用 NDVI 旬最大值法,结合吉林省主要农作物生长发育的特点,对主要产粮区作物生长季旱田和水田的 NDVI 时空变化规律进行研究,并分析其与气温和降水的关系。结果表明:2000—2012年吉林省作物生长季农作物的 NDVI 随作物生长发育进程有明显的变化,水田和旱田两种作物的 NDVI 时间变化均呈单峰型;吉林省不同区域的 NDVI 变化趋势一致,5月上旬至6月上旬,NDVI 呈缓慢增加的趋势;6月中旬至7月上旬,NDVI 迅速增加;7月中旬至8月上旬,NDVI 增加缓慢;8月中旬开始,NDVI 开始下降。6月中旬开始,吉林省中部地区旱田 NDVI 明显高于西部地区,NDVI 增长速率中部地区大于西部地区,达到峰值的时间中部地区也早于西部地区。吉林省水田 NDVI 变化中西部地区差异较小,均在8月上旬达到峰值,植被指数时间变化与吉林省作物生长发育进程相吻合。吉林省中西部地区作物的 NDVI 与气温和降水均呈正相关,气温和降水对 NDVI 的影响有明显滞后效应,且气温的影响大于降水。
為瞭確定作物長勢遙感鑑測的評價指標,利用2000—2012年吉林省 EOS /MODIS 數據,採用 NDVI 旬最大值法,結閤吉林省主要農作物生長髮育的特點,對主要產糧區作物生長季旱田和水田的 NDVI 時空變化規律進行研究,併分析其與氣溫和降水的關繫。結果錶明:2000—2012年吉林省作物生長季農作物的 NDVI 隨作物生長髮育進程有明顯的變化,水田和旱田兩種作物的 NDVI 時間變化均呈單峰型;吉林省不同區域的 NDVI 變化趨勢一緻,5月上旬至6月上旬,NDVI 呈緩慢增加的趨勢;6月中旬至7月上旬,NDVI 迅速增加;7月中旬至8月上旬,NDVI 增加緩慢;8月中旬開始,NDVI 開始下降。6月中旬開始,吉林省中部地區旱田 NDVI 明顯高于西部地區,NDVI 增長速率中部地區大于西部地區,達到峰值的時間中部地區也早于西部地區。吉林省水田 NDVI 變化中西部地區差異較小,均在8月上旬達到峰值,植被指數時間變化與吉林省作物生長髮育進程相吻閤。吉林省中西部地區作物的 NDVI 與氣溫和降水均呈正相關,氣溫和降水對 NDVI 的影響有明顯滯後效應,且氣溫的影響大于降水。
위료학정작물장세요감감측적평개지표,이용2000—2012년길림성 EOS /MODIS 수거,채용 NDVI 순최대치법,결합길림성주요농작물생장발육적특점,대주요산량구작물생장계한전화수전적 NDVI 시공변화규률진행연구,병분석기여기온화강수적관계。결과표명:2000—2012년길림성작물생장계농작물적 NDVI 수작물생장발육진정유명현적변화,수전화한전량충작물적 NDVI 시간변화균정단봉형;길림성불동구역적 NDVI 변화추세일치,5월상순지6월상순,NDVI 정완만증가적추세;6월중순지7월상순,NDVI 신속증가;7월중순지8월상순,NDVI 증가완만;8월중순개시,NDVI 개시하강。6월중순개시,길림성중부지구한전 NDVI 명현고우서부지구,NDVI 증장속솔중부지구대우서부지구,체도봉치적시간중부지구야조우서부지구。길림성수전 NDVI 변화중서부지구차이교소,균재8월상순체도봉치,식피지수시간변화여길림성작물생장발육진정상문합。길림성중서부지구작물적 NDVI 여기온화강수균정정상관,기온화강수대 NDVI 적영향유명현체후효응,차기온적영향대우강수。
Using EOS /MODIS data from 2000 to 2012,spatial-temporal characteristics of NDVI(Normalized Difference Vegetation Index)in dry farmland and paddy field over the main grain producing areas in Jilin province were analyzed by a ten-day maximum method in order to monitoring crop growth,and its relationship with precipi-tation and temperature were discussed.The results show that NDVI has a remarkable variation with the growth of crop during growth season from 2000 to 2012,and NDVI-time curves of crop in dry farmland and paddy filed both are a single peak.Trends of NDVI in different regions are similar,i.e.,NDVI increases slowly from first ten-day of May?to first ten-day of June;it increases rapidly from the middle ten-day of June to first ten-day of July and then increases gradually from the middle ten-day of July to first ten-day of August;it decreases in the middle ten-day of August.NDVI in dry farmland is higher in the middle than in the west of Jilin province after the first ten-day of June,and its increase rate is also faster and the time of peak is earlier.However,NDVI in paddy field has no signif-icant differences between the central and the west,and both reach peak values in the first ten-day of August.There is a good relationship between variation of NDVI and crop growing.NDVI of main crops in mid-west regions of Ji-lin province has a positive correlation with temperature and precipitation,and a lag-effect of temperature and pre-cipitation on NDVI is significant.In addition,the effect of temperature is greater than that of precipitation.