Abstract

Traditionally, Radiative Transfer (RT) formulation has been used to simulate scattering from snow layer with the incorporation of phase matrix of scatterers in the formulation. Typically, spherical scatterers were assumed to represent the ice particles embedded inside the air medium and Mie phase matrix was applied. However, the real scatterers in the actual snow are generally more irregular than the assumed spherical shape. In this paper, a numerical solution based on the Hierarchical Equivalent Source Algorithm (HESA) has been developed to calculate the phase matrix of scatterers of other shapes to be incorporated in the existing RT formulation. Results from the new model shows good agreement with the ground truth measurement data collected from NASA Cold Land Processes Field Experiment (CLPX). The comparison shows that the scatterer shape could have significant contribution on total backscattering when the frequency is high.

Department(s)

Electrical and Computer Engineering

Keywords and Phrases

CLPX; equivalent source algorithm; Mie-scattering; radiative transfer

International Standard Book Number (ISBN)

978-150904951-6

Document Type

Article - Conference proceedings

Document Version

Citation

File Type

text

Language(s)

English

Rights

© 2024 Institute of Electrical and Electronics Engineers, All rights reserved.

Publication Date

01 Dec 2017

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