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- W2297733690 abstract "Core Ideas Models of coupled water flow and heat transport improve our understanding of ecosystems. Soil and snow liquid water flow, water vapor flow, and ice are described using numerical models. The model is verified for a bare desert soil, a rangeland soil, and a forest soil. A one-dimensional vertical numerical model for coupled water flow and heat transport in soil and snow was modified to include all three phases of water: vapor, liquid, and ice. The top boundary condition in the model is driven by incoming precipitation and the surface energy balance. The model was applied to three different terrestrial systems: a warm desert bare lysimeter soil in Boulder City, NV; a cool mixed-grass rangeland soil near Laramie, WY; and a snow-dominated mountainous forest soil about 50 km west of Laramie, WY. Comparison of measured and calculated soil water contents with depth yielded modeling efficiency (ME) values (maximum range: −∞ < ME ≤ 1) of 0.32 ≤ ME ≤ 0.75 for the bare soil, 0.05 ≤ ME ≤ 0.30 for the rangeland soil, and 0.06 ≤ ME ≤ 0.37 for the forest soil. Results for soil temperature with depth were 0.87 ≤ ME ≤ 0.91 for the bare soil, 0.92 ≤ ME ≤ 0.94 for the rangeland soil, and 0.85 ≤ ME ≤ 0.88 for the forest soil. The model described the mass change in the bare soil lysimeter due to outgoing evaporation with moderate accuracy (ME = 0.41, based on 4 yr of data and using weekly evaporation rates). Snow height for the rangeland soil and the forest soil was captured reasonably well (ME = 0.57 for both sites based on 5 yr of data for each site). The model is physics based, with few empirical parameters, making it applicable to a wide range of terrestrial ecosystems." @default.
- W2297733690 created "2016-06-24" @default.
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- W2297733690 date "2016-03-01" @default.
- W2297733690 modified "2023-10-01" @default.
- W2297733690 title "Numerical Modeling of Coupled Water Flow and Heat Transport in Soil and Snow" @default.
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- W2297733690 doi "https://doi.org/10.2136/sssaj2015.07.0279" @default.
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