Coupling diffusion and maximum entropy models to estimate thermal inertia

Remote Sensing of Environment

Volumn 119, Issue , 2012, Pages 222-231

  Nearing, Grey S ^a   Moran, M Susan ^b   Scott, Russell L ^b   Ponce Campos, Guillermo ^b  

^a UNIVERSITY OF ARIZONA   (United States)

^b SOUTHWEST WATERSHED RESEARCH CENTER   (United States)

Author keywords

Maximum entropy production; Soil moisture; Surface energy balance; Thermal inertia

Indexed keywords

CONVECTIVE HEAT TRANSFER; COUPLED MODELS; DIFFUSION MODEL; DIURNAL RANGES; DRY CONDITION; FLUX BOUNDARY CONDITIONS; FREE PARAMETERS; LAND SURFACE; LINEAR APPROXIMATIONS; MAXIMUM ENTROPY; MAXIMUM ENTROPY MODELS; MAXIMUM LIKELIHOOD ESTIMATE; MOISTURE CONTENTS; NET RADIATION; PARAMETERIZED; PARAMETERIZING; PROBABILISTIC UNCERTAINTY MODEL; SEMI ARID; SOIL THERMAL INERTIA; SPECIFIC HUMIDITY; SURFACE FLUX; SURFACE TEMPERATURES; THERMAL INERTIA; WET CONDITIONS;

BOUNDARY CONDITIONS; DIFFUSION; ENERGY TRANSFER; ENTROPY; ESTIMATION; HEAT FLUX; INTERFACIAL ENERGY; MAXIMUM LIKELIHOOD ESTIMATION; SOIL MOISTURE; SOIL SURVEYS; SURFACE CHEMISTRY; SURFACE MEASUREMENT;

GEOLOGIC MODELS;

DIFFUSION; ENERGY BALANCE; HEAT FLUX; HEAT TRANSFER; LAND SURFACE; MAXIMUM ENTROPY ANALYSIS; NET RADIATION; SENSITIVITY ANALYSIS; SOIL MOISTURE; SURFACE ENERGY; TIME SERIES; WATER CONTENT;

UNITED STATES;

EID: 84856077978     PISSN: 00344257     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.rse.2011.12.012     Document Type: Article

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