Published April 2018 | Version v1
Journal article

Snow particles extracted from X-ray computed microtomography imagery and their single-scattering properties

  • 1. Meteorological Research Institute, Tsukuba 305-0052 (Japan)
  • 2. National Research Institute for Earth Science and Disaster Prevention, Snow and Ice Research Center, Nagaoka 940-0821 (Japan)
  • 3. Faculty of Science, Okayama University, Okayama 700-8539 (Japan)

Description

Highlights: • Individual snow particles were extracted from X-ray micro-CT data. • Single scattering properties of realistic snow particles were calculated. • Results were compared to those of numerically originated particle shape models. Sizes and shapes of snow particles were determined from X-ray computed microtomography (micro-CT) images, and their single-scattering properties were calculated at visible and near-infrared wavelengths using a Geometrical Optics Method (GOM). We analyzed seven snow samples including fresh and aged artificial snow and natural snow obtained from field samples. Individual snow particles were numerically extracted, and the shape of each snow particle was defined by applying a rendering method. The size distribution and specific surface area distribution were estimated from the geometrical properties of the snow particles, and an effective particle radius was derived for each snow sample. The GOM calculations at wavelengths of 0.532 and 1.242 µm revealed that the realistic snow particles had similar scattering phase functions as those of previously modeled irregular shaped particles. Furthermore, distinct dendritic particles had a characteristic scattering phase function and asymmetry factor. The single-scattering properties of particles of effective radius reff were compared with the size-averaged single-scattering properties. We found that the particles of reff could be used as representative particles for calculating the average single-scattering properties of the snow. Furthermore, the single-scattering properties of the micro-CT particles were compared to those of particle shape models using our current snow retrieval algorithm. For the single-scattering phase function, the results of the micro-CT particles were consistent with those of a conceptual two-shape model. However, the particle size dependence differed for the single-scattering albedo and asymmetry factor.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.jqsrt.2018.01.021

Additional details

Identifiers

DOI
10.1016/j.jqsrt.2018.01.021;
PII
S002240731730657X;

Publishing Information

Journal Title
Journal of Quantitative Spectroscopy and Radiative Transfer
Journal Volume
209
Journal Page Range
p. 113-128
ISSN
0022-4073
CODEN
JQSRAE

INIS

Country of Publication
United Kingdom
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
54105298
Subject category
S74: ATOMIC AND MOLECULAR PHYSICS;
Descriptors DEI
ALBEDO; ASYMMETRY; COMPUTERIZED TOMOGRAPHY; PARTICLE SIZE; SCATTERING; SHAPE; SNOW; X RADIATION
Descriptors DEC
ATMOSPHERIC PRECIPITATIONS; DIAGNOSTIC TECHNIQUES; ELECTROMAGNETIC RADIATION; IONIZING RADIATIONS; RADIATIONS; SIZE; TOMOGRAPHY

Optional Information

Copyright
Copyright (c) 2018 The Authors. Published by Elsevier Ltd.