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

被引:59
作者
Chen, J. M. [1 ,2 ]
Chen, X. [3 ]
Ju, W. [2 ]
机构
[1] Nanjing Univ, Int Inst Earth Syst Sci, Nanjing 210093, Jiangsu, Peoples R China
[2] Univ Toronto, Dept Geog, Toronto, ON M5S 3G3, Canada
[3] Hohai Univ, Coll Hydrol & Water Resources, Nanjing 210098, Jiangsu, Peoples R China
关键词
LEAF-AREA INDEX; SOIL-MOISTURE; ECOSYSTEM PRODUCTIVITY; MODEL; WATER; EVAPOTRANSPIRATION; ENVIRONMENT; LANDSCAPE; SATELLITE; RUNOFF;
D O I
10.5194/bg-10-4879-2013
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
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 30m and 1 km resolutions for a 5700 km(2) watershed with an elevation range from 518m to 3767m in the Qinling Mountain, Shanxi Province, China. Assuming that the NPP simulated at 30m 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 R-2 = 0.782 to R-2 = 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 30m resolution, where the mean NPP is 668 g C m(-2) yr(-1). The range of spatial variations of NPP at 30m 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.
引用
收藏
页码:4879 / 4896
页数:18
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