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基于CASA模型和SEVI指数的福建省植被NPP遥感估算与分析

Estimation and Analysis of Vegetation Net Primary Productivity of Fujian Province Using CASA Model and SEVI Information

  • 摘要: 植被净初级生产力(NPP)是评估陆地生态系统碳汇和调节过程的重要指标,但遥感影像上崎岖地形造成的光学辐射传输畸变会降低植被NPP估算精度.为了消除地形对山区植被NPP模型估算的影响,以福建省为研究区,利用阴影消除植被指数(SEVI)改进CASA 模型中的植被光合有效辐射吸收比率因子(FPAR)计算模型,进行福建省2005年和2015年的植被NPP估算和时空分布特征分析.研究结果显示SEVI反演的FPAR在阴影处的相对误差降低至0.53%,能有效消除地形阴影对FPAR的影响.采用消除了地形阴影影响的FPAR进行CASA模型反演福建省2005年和2015年的植被NPP平均值分别达到861.9 gm-2·a-1和855.7 gm-2·a-1.其中常绿阔叶林NPP最高,农用地NPP最低.不同地区植被NPP分布差异明显,西部内陆较高,东部沿海较低.月均植被NPP总体变化趋势与温度因子走势相同,相关系数分别为0.96和0.95,夏季月均植被NPP最高,达110 gm-2以上;冬季月均植被NPP最低,在20 gm-2以下.

     

    Abstract: Vegetation Net Primary Productivity (NPP) is an important index to evaluate the terrestrial ecosystem carbon sink and regulation process, however, the estimating accuracy of vegetation NPP decreases in rugged terrain, due to the optical radiative transfer distortion caused by the topographic effect. In the report, in order to eliminate the effects of topographic shadow on vegetation NPP estimation, the shadow-eliminated vegetation index (SEVI) was used to improve the photosynthetically active radiation (FPAR) model of the Carnegie-Ames-Stanford approach (CASA) model and analyze the spatial-temporal distribution characteristics of vegetation NPP in Fujian Province of 2005 and 2015. The results showed that when the relative error of FPAR in shadow calculated by the SEVI information was reduced to 0.53%, the effects of topographic shadow were eliminated. With the improved method, the average vegetation NPP of Fujian province was 861.9 g·m-2·a-1 in 2005 and 855.7 g·m-2·a-1 in 2015, respectively. The NPP of evergreen broad-leaved forest was the highest, and that of farmland was the lowest. The distribution of vegetation NPP was high in the western inland area and low in the eastern coastal area. The overall trend of monthly average vegetation NPP was approximately to that of temperature, with the highest NPP in summer of above 110 g·m-2, while the lowest NPP in winter of less than 20 g·m-2.

     

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