Articles | Volume 10, issue 7
Biogeosciences, 10, 4879–4896, 2013

Special issue: Integrated Land Ecosystem-Atmosphere Processes Study (iLEAPS)...

Biogeosciences, 10, 4879–4896, 2013

Research article 18 Jul 2013

Research article | 18 Jul 2013

Effects of vegetation heterogeneity and surface topography on spatial scaling of net primary productivity

J. M. Chen1,2, X. Chen3, and W. Ju2 J. M. Chen et al.
  • 1International Institute of Earth System Science, Nanjing University, Nanjing, Jiangsu 210093, China
  • 2Department of Geography, University of Toronto, Ontario M5S 3G3, Canada
  • 3College of Hydrology and Water Resources, Hohai University, Nanjing, Jiangsu 210098, China

Abstract. Due to the heterogeneous nature of the land surface, spatial scaling is an inevitable issue in the development of land models coupled with low-resolution Earth system models (ESMs) for predicting land-atmosphere interactions and carbon-climate feedbacks. In this study, a simple spatial scaling algorithm is developed to correct errors in net primary productivity (NPP) estimates made at a coarse spatial resolution based on sub-pixel information of vegetation heterogeneity and surface topography. An eco-hydrological model BEPS-TerrainLab, which considers both vegetation and topographical effects on the vertical and lateral water flows and the carbon cycle, is used to simulate NPP at 30 m and 1 km resolutions for a 5700 km2 watershed with an elevation range from 518 m to 3767 m in the Qinling Mountain, Shanxi Province, China. Assuming that the NPP simulated at 30 m resolution represents the reality and that at 1 km resolution is subject to errors due to sub-pixel heterogeneity, a spatial scaling index (SSI) is developed to correct the coarse resolution NPP values pixel by pixel. The agreement between the NPP values at these two resolutions is improved considerably from R2 = 0.782 to R2 = 0.884 after the correction. The mean bias error (MBE) in NPP modelled at the 1 km resolution is reduced from 14.8 g C m−2 yr−1 to 4.8 g C m−2 yr−1 in comparison with NPP modelled at 30 m resolution, where the mean NPP is 668 g C m−2 yr−1. The range of spatial variations of NPP at 30 m resolution is larger than that at 1 km resolution. Land cover fraction is the most important vegetation factor to be considered in NPP spatial scaling, and slope is the most important topographical factor for NPP spatial scaling especially in mountainous areas, because of its influence on the lateral water redistribution, affecting water table, soil moisture and plant growth. Other factors including leaf area index (LAI) and elevation have small and additive effects on improving the spatial scaling between these two resolutions.

Final-revised paper