The development of bi-continuous scattering model greatly enhanced the ability to model the snow scattering characteristics based on microstructure with most similarity to real snowpack. In this study, snow section images of snow microstructure were used to study the scattering characteristics of snow by using the reconstructed snow 3D microstructure. The equivalent grain size of the continuous random structure is derived by using stereological method. By combining with dense media radiative transfer equations, the snow backscattering is simulated. The polarimetric and frequency characteristics were studied.

MICROWAVE SNOW BACKSCATTERING MODELING BASED ON TWO-DIMENSIONAL SNOW SECTION IMAGE AND EQUIVALENT GRAIN SIZE

Brogioni Marco;
2012

Abstract

The development of bi-continuous scattering model greatly enhanced the ability to model the snow scattering characteristics based on microstructure with most similarity to real snowpack. In this study, snow section images of snow microstructure were used to study the scattering characteristics of snow by using the reconstructed snow 3D microstructure. The equivalent grain size of the continuous random structure is derived by using stereological method. By combining with dense media radiative transfer equations, the snow backscattering is simulated. The polarimetric and frequency characteristics were studied.
2012
Istituto di Fisica Applicata - IFAC
Inglese
2012 IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM (IGARSS)
150
153
4
978-1-4673-1158-8
IEEE-INSTITUTE OF ELECTRICAL AND ELECTRONICS ENGINEERS INC.
345 E 47TH ST, NEW YORK, NY 10017-2394
STATI UNITI D'AMERICA
bi-continuous
snow
stereology
equivalent grain size
polarimetric
frequency
4
none
Xiong, Chuan; Shi, Jiancheng; Brogioni, Marco; Tsang, Leung
273
info:eu-repo/semantics/conferenceObject
04 Contributo in convegno::04.01 Contributo in Atti di convegno
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/264037
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