Accounting for Calcareous Concretions in Calcic Vertisols Improves the Accuracy of Soil Hydraulic Property Estimations

2017 ◽  
Vol 81 (6) ◽  
pp. 1296-1302 ◽  
Author(s):  
Feng Gu ◽  
Tusheng Ren ◽  
Baoguo Li ◽  
Lujiu Li
Keyword(s):  
Hydraulic Property ◽  
Soil Hydraulic Property ◽  
Soil Hydraulic

scholarly journals Pedotransfer Function for the Brunswick Soil Hydraulic Property Model and Comparison to the van Genuchten‐Mualem Model

2020 ◽  
Vol 56 (9) ◽  
Author(s):  
Tobias K. D. Weber ◽  
Michael Finkel ◽  
Maria Gonçalves ◽  
Harry Vereecken ◽  
Efstathios Diamantopoulos
Keyword(s):  
Pedotransfer Function ◽  
Hydraulic Property ◽  
Soil Hydraulic Property ◽  
Property Model ◽  
Soil Hydraulic

scholarly journals A Simulation and Validation of CLM during Freeze-Thaw on the Tibetan Plateau

2016 ◽  
Vol 2016 ◽  
pp. 1-15 ◽  
Author(s):  
Xuewei Fang ◽  
Siqiong Luo ◽  
Shihua Lyu ◽  
Boli Chen ◽  
Yu Zhang ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Frozen Soil ◽  
Surface Radiation ◽  
The Tibetan Plateau ◽  
Hydraulic Property ◽  
Freeze Thaw ◽  
Community Land Model ◽  
Thaw Cycle ◽  
Soil Hydraulic Property ◽  
Soil Hydraulic

The applicability of a new soil hydraulic property of frozen soil scheme applied in Community Land Model 4.5 (CLM4.5), in conjunction with an impedance factor for the presence of soil ice, was validated through two offline numerical simulations conducted at Madoi (GS) and Zoige (ZS) on the Tibetan Plateau (TP). Sensitivity analysis was conducted via replacing the new soil hydraulic property scheme in CLM4.5 by the old one, using default CLM4.5 runs as reference. Results indicated that the new parameterization scheme ameliorated the surface dry biases at ZS but enlarged the wet biases which existed at GS site due to ignoring the gravel effect. The wetter surface condition in CLM4.5 also leads to a warmer surface soil temperature because of the greater heat capacity of liquid water. In addition, the combined impact of new soil hydraulic property schemes and the ice impedance function on the simulated soil moisture lead to the more reasonable simulation of the starting dates of freeze-thaw cycle, especially at the thawing stage. The improvements also lead to the more reasonable turbulent fluxes simulations. Meanwhile, the decreased snow cover fraction in CLM4.5 resulted in a lower albedo, which tended to increase net surface radiation compared to previous versions. Further optimizing is needed to take the gravel into account in the numerical description of thermal-hydrological interactions.

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