Multi-scale regional forest carbon density estimation based on regression and sequential Gaussian co-simulation

详细信息    查看全文

• 作者：Gaoyun Shen^a ; Maozhen Zhang^a ; ^b ; ^{zhangmaozhen@163.com" class="auth_mail" title="E-mail the corresponding author}
• 关键词：Above-ground forest carbon storage ; Forest inventory ; Carbon density ; Carbon distribution ; Sequential Gaussian co-simulation ; Multi-scale
• 刊名：Acta Ecologica Sinica
• 出版年：2016
• 出版时间：April 2016
• 年：2016
• 卷：36
• 期：2
• 页码：62-71
• 全文大小：1592 K

文摘

By applying nonlinear regression of a unary cubic equation and sequential Gaussian co-simulation to Forest Inventory (plot) data in Xianju county, Zhejiang, from 2008, and Landsat TM image data collected in the same region in 2007, this research estimated the above-ground forest carbon density and its distributions at 30 m × 30 m and 270 m × 270 m resolutions, and analyzed the results comparatively. The results showed that the above-ground forest carbon density of Xianju county was continuously distributed, and was surrounded by high carbon density forestland, and the majority of the intermediate region was filled with low carbon density non-forestland. Using the random sampling method, the total carbon estimate is 5,289,437.11 Mg. At 30 m × 30 m resolution, with nonlinear regression of a unary cubic equation, the total carbon is 5,246,749.81 Mg, and the R² of the model is 0.1353. At the same scale, with sequential Gaussian co-simulation, the total carbon is 5,692,875.69 Mg, and the R² of the model is 0.6203. Compared with the results in the 270 m × 270 m resolution, the former total carbon amount is larger, the range of distribution is wider, and the model's precision is higher. Comparing the two methods, the results estimated by the sequential Gaussian co-simulation are better than those of the unary cubic nonlinear regression. The result of sequential Gaussian co-simulation, which considers the spatial distribution of carbon density, is closer to that estimated from plot data, and better represents the continuous change of the carbon distribution.