南京大学学报(自然科学版)
南京大學學報(自然科學版)
남경대학학보(자연과학판)
JOURNAL OF NANJING UNIVERSITY(NATURAL SCIENCES)
2015年
3期
626-640
,共15页
李前%汤剑平%张建友%潘华
李前%湯劍平%張建友%潘華
리전%탕검평%장건우%반화
植被%气候%年际变化%时滞相关
植被%氣候%年際變化%時滯相關
식피%기후%년제변화%시체상관
vegetation%climate%interannual variation%lagged correlations
利用 NOAA AVHRR 遥感资料反演得到的中国地区19年(1982—2000)逐月光合有效辐射分量(FPAR)与英国气候变化研究中心(CRU)高分辨率格点资料中逐月平均的近地面气温和降水进行时滞相关分析。结果表明,我国大部分地区 FPAR 与同期气温的相关为显著正相关,说明温度对植被的即时强迫很强;而 FPAR 与超前一月的降水相关系数最大,均为正的显著相关,特别是在春季华北地区,表明前一月的降水对植被生长影响很大。 FPAR 与温度的相关性在春、秋季最明显,FPAR 与降水的相关性在春、夏季最强。
利用 NOAA AVHRR 遙感資料反縯得到的中國地區19年(1982—2000)逐月光閤有效輻射分量(FPAR)與英國氣候變化研究中心(CRU)高分辨率格點資料中逐月平均的近地麵氣溫和降水進行時滯相關分析。結果錶明,我國大部分地區 FPAR 與同期氣溫的相關為顯著正相關,說明溫度對植被的即時彊迫很彊;而 FPAR 與超前一月的降水相關繫數最大,均為正的顯著相關,特彆是在春季華北地區,錶明前一月的降水對植被生長影響很大。 FPAR 與溫度的相關性在春、鞦季最明顯,FPAR 與降水的相關性在春、夏季最彊。
이용 NOAA AVHRR 요감자료반연득도적중국지구19년(1982—2000)축월광합유효복사분량(FPAR)여영국기후변화연구중심(CRU)고분변솔격점자료중축월평균적근지면기온화강수진행시체상관분석。결과표명,아국대부분지구 FPAR 여동기기온적상관위현저정상관,설명온도대식피적즉시강박흔강;이 FPAR 여초전일월적강수상관계수최대,균위정적현저상관,특별시재춘계화북지구,표명전일월적강수대식피생장영향흔대。 FPAR 여온도적상관성재춘、추계최명현,FPAR 여강수적상관성재춘、하계최강。
Time-lag correlation coefficients between monthly fraction photosynthetically active radiation (FPAR), derived from satellite remote sensing by NOAA Advanced Very High Resolution Radiometer(AVHRR),surface air temperature and precipitation from Climatic Research Unit(CRU)of high-resolution climatic girds data during the 1 9-year period(1 982-2000)are analyzed for the whole year and four seasons.The simultaneous correlation of FPAR with temperature has a significant positive correlation in most parts of china,particularly in the Northeast,this result shows that temperature imposes a significant instantaneous forcing on FPAR.While precipitation’s impact on FPAR is greatest at one-month lead,the correlation coefficient is a significant positive correlation in china,especially in North China region on spring time,the result shows that the precipitation at one-month lead impacts on vegetation growth in a large part.The correlation of FPAR with temperature is significant on spring and autumn time,and the correlation of FPAR with precipitation is significant on spring and summer time.