Arid
DOI10.1016/j.agrformet.2019.02.017
A numerical analysis of aggregation error in evapotranspiration estimates due to heterogeneity of soil moisture and leaf area index
Chen, Qiting1,2; Jia, Li1; Menenti, Massimo1,3; Hutjes, Ronald2; Hu, Guangcheng1; Zheng, Chaolei1; Wang, Kun1
通讯作者Jia, Li
来源期刊AGRICULTURAL AND FOREST METEOROLOGY
ISSN0168-1923
EISSN1873-2240
出版年2019
卷号269页码:335-350
英文摘要Land Surface Models which determine evapotranspiration (ET) by neglecting the sub-grid heterogeneity of land-atmosphere parameters will cause aggregation biases in spatially-averaged ET estimates, considering the non-linear dependences of ET on the heterogeneous land-atmosphere parameters. One frequently adopted strategy clusters the heterogeneous surface within a model grid into several tiles, assumed to be homogeneous, usually based on high-resolution land cover data. While the differences in bulk-averaged parameters between different tiles are considered, the heterogeneity within each tile is neglected. This study evaluated in detail the aggregation biases in the tile mean ET estimates due to applying bulk-averages of the Saturation degree of surface Soil Moisture (SSM) and Leaf Area Index (LAI) for each tile through numerical experiments. Four types of Probability Distribution Function (PDF) were used to simulate different scenarios on the heterogeneity (within a tile) of SSM and LAI, i.e., from water scarcity to wet, and from sparse to dense vegetation covered surfaces. Aggregation bias was calculated by comparing ET estimates based on bulk-averaged SSM and LAI with the one obtained by aggregation of the flux estimates based on the PDFs, which complies with energy conservation. In addition, a wide range of meteorological conditions was applied in our numerical experiments and the impacts were evaluated by binning results according to the reference ET (ET0). We found that potentially significant bias can be found in semi-arid areas. Neglecting the actual spatial variability of both SSM and LAI within tiles can lead to both large relative error (> 20%) and absolute error (> 1 mm/day) in the estimated ET. A negative bias is expected at low ET / ET0 and a positive bias is expected at large ET / ET0, regardless of climate conditions (i.e., ET0).
英文关键词Evapotranspiration Heterogeneity Aggregation bias
类型Article
语种英语
国家Peoples R China ; Netherlands
收录类别SCI-E
WOS记录号WOS:000463120900030
WOS关键词SURFACE-ENERGY-BALANCE ; BIOSPHERE MODEL ; ECMWF MODEL ; RIVER-BASIN ; LAND ; PARAMETERIZATION ; SCALE ; WATER ; VEGETATION ; CLIMATE
WOS类目Agronomy ; Forestry ; Meteorology & Atmospheric Sciences
WOS研究方向Agriculture ; Forestry ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/213947
作者单位1.Chinese Acad Sci, Inst Remote Sensing & Digital Earth, State Key Lab Remote Sensing Sci, Beijing 100101, Peoples R China;
2.Wageningen Univ, NL-6700 AA Wageningen, Netherlands;
3.Delft Univ Technol, NL-2600 AA Delft, Netherlands
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Chen, Qiting,Jia, Li,Menenti, Massimo,et al. A numerical analysis of aggregation error in evapotranspiration estimates due to heterogeneity of soil moisture and leaf area index[J],2019,269:335-350.
APA Chen, Qiting.,Jia, Li.,Menenti, Massimo.,Hutjes, Ronald.,Hu, Guangcheng.,...&Wang, Kun.(2019).A numerical analysis of aggregation error in evapotranspiration estimates due to heterogeneity of soil moisture and leaf area index.AGRICULTURAL AND FOREST METEOROLOGY,269,335-350.
MLA Chen, Qiting,et al."A numerical analysis of aggregation error in evapotranspiration estimates due to heterogeneity of soil moisture and leaf area index".AGRICULTURAL AND FOREST METEOROLOGY 269(2019):335-350.
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