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1981~2000年中国陆地生态系统NPP时空变化特征分析
引用本文:王磊,丁晶晶,季永华,梁珍海,阮宏华,刘世荣.1981~2000年中国陆地生态系统NPP时空变化特征分析[J].江苏林业科技,2009,36(6):1-5.
作者姓名:王磊  丁晶晶  季永华  梁珍海  阮宏华  刘世荣
作者单位:1. 江苏省林业科学研究院,江苏,南京,211153;中国林业科学研究院森林生态环境与保护研究所,北京,100091
2. 江苏省林业科学研究院,江苏,南京,211153
3. 南京林业大学森林资源与环境学院,江苏,南京,210037
4. 中国林业科学研究院森林生态环境与保护研究所,北京,100091
基金项目:林业公益性行业科研专项,林业公益性行业科研专项,江苏省林业三项工程项目,江苏省国际科技合作计划 
摘    要:利用GLO-PEM模型估算了1981~2000年中国陆地生态系统植被净第一性生产力(NPP)。结果表明:1981~2000年中国总NPP呈现增加趋势,从1981年的2.82 PgC/a增加到2000年的3.13 PgC/a,年均增加0.0155PgC/a,20 a间NPP的平均值为2.98 PgC/a,约占全球NPP总量的4.7%~5.0%。NPP积累主要发生在4~10月,春季、夏季、秋季、冬季NPP量分别占全年总量的15.68%,54.54%,25.50%,4.2%。其中夏季NPP增长最快,占全年NPP增长的64.14%。全国NPP年均值从西北向东南方向呈逐步增加趋势,不同植被类型中,常绿阔叶林年均NPP最高,达745.68 gC/m2,除农业植被外各种植被类型的月均NPP最大值都出现在7月,最小值都出现在1月。经向剖线NPP变化规律不明显。纬向40°N线是南北分界线,往南随着纬度的降低,剖线平均NPP逐渐升高,往北随着纬度的增加,剖线平均NPP逐步变大。纬向剖线NPP均值最高的是20°N线,异质性最高的是30°N线。

关 键 词:GLO-PEM模型  植被净第一性生产力(NPP)  植被类型  经纬向变化

Spatiotemporal pattern of NPP in terrestrial ecosystem of China from 1981 to 2000
WANG Lei,DING Jing-jing,JI Yong-hua,LIANG Zhen-hai,RUAN Hong-hua,LIU Shi-rong.Spatiotemporal pattern of NPP in terrestrial ecosystem of China from 1981 to 2000[J].Journal of Jiangsu Forestry Science & Technology,2009,36(6):1-5.
Authors:WANG Lei  DING Jing-jing  JI Yong-hua  LIANG Zhen-hai  RUAN Hong-hua  LIU Shi-rong
Institution:WANG Lei, DING Jing-jing, JI Yong-hua, LIANG Zhen-hai, RUAN Hong-hua, LIU Shi-rong(1. Jiangsu Academy of Forestry, Nanjing 211153, China ;2. Institute of Forest Ecology,Environment and Protection, Chinese Academy of Forestry, Beijing 10(1091, China ;3. College of Forest Resources and Environment,Nanjing Forestry University, Nanjing 210037, China)
Abstract:GLO-PEM model was applied to estimate Net Primary Productivity(NPP) of terrestrial ecosystems in China from 1981 to 2000.The results indicated that the NPP increased from 2.82 PgC/a in 1981 to 3.13 PgC/a in 2000 in China.The mean NPP was 2.98 PgC/a,making up nearly 5.0% of the global NPP.NPP was accumulated during April to October within a year.The NPP in summer increased rapidly,accounting for 64.14% of the total of annual NPP.The annual NPP increased gradually from northwest to southeast in the distribution, and that in evergreen broad-leaved forest was the highest among different vegetation types, reaching 745.68 gC/(m^2·a). Monthly average NPP of all vegetation types except agricultural vegetation reached the maximum in July and the minimum in January. Meridional NPP changed irregularly. 40°N latitude was the North-South demarcating line, and mean zonal NPP in the south of the line increased gradually as the latitude lowered. The mean zonal NPP reached the peak value in the 20°N latitude while there was the highest heterogeneity in the 30°N latitude.
Keywords:GLO-PEM model  NPP  Vegetation types  Changes with longitude and latitude
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