4.7 Article

A Comprehensive Emission Model for Layered Irregular and Inhomogeneous Medium

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IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/TGRS.2023.3249793

关键词

Coherent boundary interaction; emission model; rough boundary scattering; scattering operator; volume scattering

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Reported radiometric measurements show that microwave emission features of layered irregular and inhomogeneous medium are characterized by incoherent and coherent radiative transfer processes. In this article, a comprehensive layer emission model (CLEM) based on the scattering operator formulation is presented to consider medium and boundary scattering as well as coherent boundary interaction in general layered medium. CLEM integrates wave-based coherent multiple reflection operators and intensity-based multiple scattering processes to comprehensively describe rough boundary scattering, volume scattering, medium/boundary interaction, and coherent boundary interaction. Simulations and analyses based on CLEM are conducted to evaluate coherent boundary interaction and different impacting factors for ice- and snow-covered ground cases, and validation is performed with emission observations of snow-covered terrain and frozen soil.
Reported radiometric measurements indicate that incoherent and coherent radiative transfer processes characterize the microwave emission features of layered irregular and inhomogeneous medium. In order to develop a forward emission model to be capable of considering the medium and boundary scattering and coherent boundary interaction that may exist in general layered medium, in this article, we present a comprehensive layer emission model (CLEM) based on the scattering operator formulation. We introduce wave-based coherent multiple reflection operators to account for coherent boundary interaction and first integrate them with the intensity-based multiple scattering processes, allowing the comprehensive description of rough boundary scattering, volume scattering, medium/boundary interaction, and coherent boundary interaction in the framework of CLEM. Simulations and analyses for ice- and snow-covered ground cases are conducted based on CLEM to evaluate the coherent boundary interaction and different impacting factors. Validation on CLEM is conducted with emission observations of snow-covered terrain in campaign Nordic Snow Radar Experiment (NoSREx) 2010-2013 during dry snow period and time-series emission observations of frozen soil during freezing and thawing processes. CLEM simulation results show a good agreement with measurements. For NoSREx, root-mean-square errors (RMSEs) at L- to Ka-band are below 5.5 K for both polarizations, which are of different levels of promotion compared with the incoherent model simulations, especially for horizontal polarization at L- and X-band. Application to frozen soil case illustrates the capability of CLEM to explain coherent oscillation feature with impact from incoherent scattering effect.

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