Estimation of land surface water and energy balance parameters using conditional sampling of surface states. Issue 2 (28th February 2014)

• Record Type: Journal Article
• Authors: Farhadi, Leila; Entekhabi, Dara; Salvucci, Guido; Sun, Jian
• Is Part Of: Water resources research. Volume 50:Issue 2(2014:Feb.)
• Page Start: 1805
• Page End: 1822
• Publication Date: 2014-02-28
• Subjects: Hydrology -- Periodicals; 333.91
• DOI: 10.1002/2013WR014049
• Languages: English
• ISSNs: 0043-1397

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>Numerical models of heat and moisture diffusion in the soil‐vegetation‐atmosphere continuum are linked through the moisture flux from the surface to the atmosphere. This mass flux represents a heat exchange as latent heat flux, coupling water, and energy balance equations. In this paper, a new approach for estimating key parameters governing moisture and heat diffusion equation and the closure function which links these equations, is introduced. Parameters of the system are estimated by developing objective functions that link atmospheric forcing, surface states, and unknown parameters. This approach is based on conditional averaging of heat and moisture diffusion equations on land surface temperature and moisture states, respectively. A single objective function is expressed that measures moisture and temperature‐dependent errors solely in terms of observed forcings and surface states. This objective function is minimized with respect to the parameters to identify evaporation and drainage models and estimate water and energy balance flux components. The approach is calibration free (surface flux observations are not required), it is not hampered by missing data and does not require continuous records. Uncertainty of parameter estimates is obtained from the inverse of Hessian of the objective function, which is an approximation of the error covariance matrix. Uncertainty analysis and analysis of the covariance approximation, guides the formulation of a well‐posed estimation problem. Accuracy of this method is examined through its application over three different field sites. This approach can be applied to diverse climates and land surface conditions with different spatial scales, using remotely sensed measurements.</p> </abstract>