2023
DOI: 10.2139/ssrn.4357161
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Inconsistency and Correction of Manually Observed Ground Surface Temperatures Over Snow-Covered Regions

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“…During the soil freezing period, soil ice content ( θ i ) is set as the soil water content minus the unfrozen water content (Equation ). Soil mineral thermal conductivity ( λ m ) was set to 2.92 W m −1 K −1 for the bare ground (Cao, et al, 2019, 2023; Ling & Zhang, 2004). While λ m is variable, our sensitivity experiments indicated that λ m has a minimal influence on the simulated T s at the shallow depth of 0.03 m (not shown).…”
Section: Methodsmentioning
confidence: 99%
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“…During the soil freezing period, soil ice content ( θ i ) is set as the soil water content minus the unfrozen water content (Equation ). Soil mineral thermal conductivity ( λ m ) was set to 2.92 W m −1 K −1 for the bare ground (Cao, et al, 2019, 2023; Ling & Zhang, 2004). While λ m is variable, our sensitivity experiments indicated that λ m has a minimal influence on the simulated T s at the shallow depth of 0.03 m (not shown).…”
Section: Methodsmentioning
confidence: 99%
“…(1995): λsn=λiρsnρi1.88 ${\lambda }_{sn}={\lambda }_{i}{\left(\frac{{\rho }_{sn}}{{\rho }_{i}}\right)}^{1.88}$ where λ i is the ice thermal conductivity of 2.2 W m −1 K −1 , ρ i is the ice density of 920 kg m −3 . Static snow density is assumed here and was set to 200 kg m −3 based on the stand‐alone in situ measurements (Cao et al., 2023; Zhong, Zhang, Su, et al., 2021).…”
Section: Methodsmentioning
confidence: 99%
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