Journal ArticleDOI
A Numerical Study of Atmospheric and Soil Boundary Layers
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In this article, a numerical model of the atmosphere-soil boundary layer was developed which simulates heat and moisture exchange between the atmosphere and the soil, i.e., energy and water mass conservation and the local thermodynamic equilibrium of temperature and humidity.Abstract:
A numerical model of the atmosphere-soil boundary layer was developed which simulates heat and moisture exchange between the atmosphere and the soil. The atmospheric and soil equations are solved using the physical conditions at the atmosphere-soil interface, i.e., energy and water mass conservation and the local thermodynamic equilibrium of temperature and humidity. Quasi-stationary layers were assumed in both the atmosphere and the soil near the interface. The depth of these layers was determined by the scale analysis of various transport processes in the atmosphere and in the soil. Two calculations, which were based on different assumptions for the eddy diffusivity in the Ekman layer, were compared. The temperature calculated by use of an eddy diffusivity interpolated by Hermite polynomials is in good agreement with observations. Both examples studied predicted the wind velocity weaker than the observed, especially during the night. The numerical model thus developed was applied to the study o...read more
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Journal ArticleDOI
Efficient prediction of ground surface temperature and moisture, with inclusion of a layer of vegetation
TL;DR: In this paper, an efficient one-layer foliage parameterization was developed that extends continuously from the case of no shielding of the ground by vegetation to complete shielding, including influences of both ground and foliage albedos and emissivities, net leaf area index, stomatal resistance, retained water on the foliage, and several other considerations.
Journal ArticleDOI
Moisture and heat transport in hysteretic, inhomogeneous porous media: A matric head‐based formulation and a numerical model
TL;DR: In this paper, a general, physically based formulation of water and energy transport in partially saturated soil must account for the coupling between the fields of matric potential ψ and temperature T. This formulation facilitates a significant generalization of the theory to accommodate the omnipresent complications of hysteresis and inhomogeneity.
Journal ArticleDOI
Simulation of the effects of surface fluxes of heat and moisture in a mesoscale numerical model: 1. Soil layer
TL;DR: In this paper, a parameterization for bare soil is developed, which is to be incorporated in a mesoscale numerical prediction model, and generalized to accomodate 11 types of soil in addition to peat, using mean soil characteristics.
Journal ArticleDOI
Mutual interaction of soil moisture state and atmospheric processes
TL;DR: In this paper, the authors outline the pathways through which soil moisture and meteorological phenomena mutually influence one another at local, regional and global scales, and outline possible directions for innovative investigations on the determination of soil moisture variation influences on the moist thermodynamics, energetics and dynamics of the overlying atmosphere.
Journal ArticleDOI
Numerical Experiments on the Computation of Ground Surface Temperature in an Atmospheric General Circulation Model
TL;DR: In this paper, the Rand two-level general circulation model has been integrated to compute ground surface (bare land) temperature by solving: 1) the interface heat balance equation without soil heat flux; 2) a prognostic equation which includes the heat capacity of the soil as well as an explicit formulation for soil heat flow.
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