Observing the Effect of Morphology on Elastic Properties of New Snow using a Non-contacting Laser Ultrasound System

Quantifying micromechanical and microstructural properties of snow is crucial, they control bulk thermal, electrical, and mechanical properties.Snow density can provide an estimate of mechanical properties, while direct observation of snow microstructure is necessary to determine mechanical properties.We utilized a novel non-contacting laser ultrasound system (LUS), providing high frequency acoustic waveform measurements, to observe mechanical properties at the microscale.We investigated the temporal relationship between p-wave velocity, snow crystal type, p-wave modulus, stiffness, and SSA.We created homogeneous snow samples, each composed of a single type of precipitation particle, compacted to a density of 250 kg{m 3 .We measured wave propagation through these snow samples and observed changes in p-wave speed during equilibrium metamorphism.We also measured SSA with the InfraSnow Sensor, as well as micromechanical properties with the SnowMicroPenetrometer.With these data we observed changes in mechanical properties, with up to a factor of 2 increase in elastic modulus depending on crystal type during a period of 72 hours.Estimated elastic modulii increased over time, as expected and in agreement with previous work.Needles and columns had faster p-wave velocities, implying larger elastic modulus, com-

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Publication Details

Journal
Journal of Glaciology
Published
2026-01-01
DOI
https://doi.org/10.1017/jog.2026.10138
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
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article

Observing the Effect of Morphology on Elastic Properties of New Snow using a Non-contacting Laser Ultrasound System

Journal of Glaciology
Cryospheric studies and observations
article

Observing the Effect of Morphology on Elastic Properties of New Snow using a Non-contacting Laser Ultrasound System

article en

Abstract

Quantifying micromechanical and microstructural properties of snow is crucial, they control bulk thermal, electrical, and mechanical properties.Snow density can provide an estimate of mechanical properties, while direct observation of snow microstructure is necessary to determine mechanical properties.We utilized a novel non-contacting laser ultrasound system (LUS), providing high frequency acoustic waveform measurements, to observe mechanical properties at the microscale.We investigated the temporal relationship between p-wave velocity, snow crystal type, p-wave modulus, stiffness, and SSA.We created homogeneous snow samples, each composed of a single type of precipitation particle, compacted to a density of 250 kg{m 3 .We measured wave propagation through these snow samples and observed changes in p-wave speed during equilibrium metamorphism.We also measured SSA with the InfraSnow Sensor, as well as micromechanical properties with the SnowMicroPenetrometer.With these data we observed changes in mechanical properties, with up to a factor of 2 increase in elastic modulus depending on crystal type during a period of 72 hours.Estimated elastic modulii increased over time, as expected and in agreement with previous work.Needles and columns had faster p-wave velocities, implying larger elastic modulus, com-

Journal of Glaciology
Boise State University (US), Norwegian Geotechnical Institute (NO), Cold Regions Research and Engineering Laboratory (US)
Climate action
Openalex Percentile: Top 7%
Cryospheric studies and observations
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Observing the Effect of Morphology on Elastic Properties of New Snow using a Non-contacting Laser Ultrasound System · Journal of Glaciology (2026) | TGRS Research Map | TGRS