Development of a Land Surface Model Including Evaporation and Adsorption Processes in the Soil for the Land–Air Exchange in Arid Regions

• Published in: Journal of hydrometeorology 2007-12, Vol.8 (6), p.1307-1324
• Main Authors: Katata, Genki, Nagai, Haruyasu, Ueda, Hiromasa, Agam, Nurit, Berliner, Pedro R.
• Format: Article
• Language: English
• Subjects: Adsorption; Arid soils; Desert soils; Evaporation; Latent heat; Sandy loam soils; Soil pore water; Soil water; Soil water content; Water vapor
• ISSN: 1525-755X; 1525-7541
• DOI: 10.1175/2007jhm829.1

A one-dimensional soil model has been developed to better predict heat and water exchanges in arid and semiarid regions. New schemes to calculate evaporation and adsorption in the soil were incorporated in the model. High performance of the model was confirmed by comparison of predicted surface fluxes, soil temperature, and volumetric soil water content with those measured in the Negev Desert, Israel. Evaporation and adsorption processes in the soil have a large impact on the heat and water exchange between the atmosphere and land surface and are necessary to accurately predict them. Numerical experiments concerning the drying process of soil are performed using the presented model and a commonly used land surface model. The results indicated that, when the dry soil layer (DSL) develops, water vapor flux to the atmosphere is caused by evaporation in the soil rather than evaporation at the ground surface. Moreover, the adsorption process has some impact on the water and heat balance at the ground surface. The upward water vapor flux during the daytime is due to evaporation of soil water in the DSL, which is stored during the night due to adsorption. When the DSL progresses sufficiently, almost the same amounts of water are exchanged between the air and the soil surface by daytime evaporation and nighttime adsorption. In such conditions, latent heat due to evaporation and adsorption in the soil also work to reduce the diurnal variation of surface temperature.