Modelling Forest Soil Moisture and Temperature in Three Gorges Reservoir Area with CoupModel and Sensitivity Analysis of Parameters
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Modelling Forest Soil Moisture and Temperature in Three Gorges Reservoir Area with CoupModel and Sensitivity Analysis of Parameters
Bulletin of Soiland Water ConservationVol. 32, Issue 6, Pages: 295-301(2013)
作者机构:
1. 北京林业大学水土保持学院,北京,100083
2. 重庆市林业局,重庆,401147
3. 中国科学院教育部 水土保持与生态环境研究中心 陕西 杨凌,712100
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Published:2013
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WANG Xian, ZHANG Hong-jiang, DU Shi-cai, et al. Modelling Forest Soil Moisture and Temperature in Three Gorges Reservoir Area with CoupModel and Sensitivity Analysis of Parameters[J]. Bulletin of Soiland Water Conservation, 2013, 32(6): 295-301.
DOI:
WANG Xian, ZHANG Hong-jiang, DU Shi-cai, et al. Modelling Forest Soil Moisture and Temperature in Three Gorges Reservoir Area with CoupModel and Sensitivity Analysis of Parameters[J]. Bulletin of Soiland Water Conservation, 2013, 32(6): 295-301.DOI:
Modelling Forest Soil Moisture and Temperature in Three Gorges Reservoir Area with CoupModel and Sensitivity Analysis of Parameters
A physical process-based model(CoupModel) was applied to simulate daily soil moisture and temperature of broadleaved fore(Schima superhaLithocarpus glaher)and coniferous fores(Cunninghamia Lanceolata X Pinus massoniana)in Simian Mountain
which located in the Three Uorges Reservoir area.Then
the OAT method(one factor at a time) was adopted to analyze sensitivities of the model parameters.The validation results showed that CoupModel could fairly simulate the dynamic changes of soil moisture and temperature.Determination coefficient(R2)
mean error(ME)
root mean square error(RMSE)
and Nashsutcliffe efficiency coefficient(NSE) of soil moisture were 0.81-0.94
-0.O1%-0.26%
0.24%-1. 83%and 0.80-0.87 respectively
while they were 0.92-0.99
-0.14-0.06℃
0.18-0.34℃
and 0.90-0.98 for soil temperature.It meant that the model had a good applicability in this region.The results of the sensitivity analysis indicated that
many parameters had great influence on the simulation of soil moisture
such as lambda
air entry
residual water
saturation
matrix conductivity and PsiRs-lp.While scaling coefficient
organic layer thick
plant albedo
light extinction coefficient
cond VPD and PsiRs-lp impacted on simulation of soil temperature.
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Related Author
ZHONG Keyuan
CHEN Ying
CHEN Xingwei
LIU Meibing
Related Institution
College of Geographical Sciences, Fujian Normal University
Cultivation Base of State Key Laboratory of Humid Subtropical Mountain Ecology
Fujian Provincial Engineering Research Center for Monitoring and Assessing Terrestrial Disasters