Particle trajectories, velocities, accelerations and rotation rates in snow avalanches

Abstract Understanding the dynamics of snow avalanches is crucial for predicting their destructive potential and mobility. To gain insight into avalanche dynamics at a particle level, the AvaNode in-flow sensor system was developed. These synthetic particles, equipped with advanced and affordable se...

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Published in:Annals of Glaciology
Main Authors: Neuhauser, Michael, Köhler, Anselm, Neurauter, Rene, Adams, Marc S., Fischer, Jan-Thomas
Other Authors: Deutsche Forschungsgemeinschaft, Austrian Science Fund
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2023.69
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000691
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spelling crcambridgeupr:10.1017/aog.2023.69 2024-06-09T07:38:27+00:00 Particle trajectories, velocities, accelerations and rotation rates in snow avalanches Neuhauser, Michael Köhler, Anselm Neurauter, Rene Adams, Marc S. Fischer, Jan-Thomas Deutsche Forschungsgemeinschaft Austrian Science Fund 2023 http://dx.doi.org/10.1017/aog.2023.69 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000691 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Annals of Glaciology page 1-18 ISSN 0260-3055 1727-5644 journal-article 2023 crcambridgeupr https://doi.org/10.1017/aog.2023.69 2024-05-15T12:55:50Z Abstract Understanding the dynamics of snow avalanches is crucial for predicting their destructive potential and mobility. To gain insight into avalanche dynamics at a particle level, the AvaNode in-flow sensor system was developed. These synthetic particles, equipped with advanced and affordable sensors such as an inertial measurement unit (IMU) and global navigation satellite system (GNSS), travel with the avalanche flow. This study focuses on assessing the feasibility of the in-flow measurement systems. The experiments were conducted during the winter seasons of 2021–2023, both in static snow cover and dynamic avalanche conditions of medium-sized events. Radar measurements were used in conjunction with the particle trajectories and velocities to understand the behaviour of the entire avalanche flow. The dynamic avalanche experiments allowed to identify three distinct particle flow states: (I) initial rapid acceleration, (II) a steady state flow with the highest velocities (9–17 ms −1 ), and (III) a longer deceleration state accompanied by the largest measured rotation rates. The particles tend to travel towards the tail of the avalanche and reach lower velocities compared to the frontal approach velocities deduced from radar measurements (ranging between 23–28 ms −1 ). The presented data give a first insight in avalanche particle measurements. Article in Journal/Newspaper Annals of Glaciology Cambridge University Press Annals of Glaciology 1 18
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Understanding the dynamics of snow avalanches is crucial for predicting their destructive potential and mobility. To gain insight into avalanche dynamics at a particle level, the AvaNode in-flow sensor system was developed. These synthetic particles, equipped with advanced and affordable sensors such as an inertial measurement unit (IMU) and global navigation satellite system (GNSS), travel with the avalanche flow. This study focuses on assessing the feasibility of the in-flow measurement systems. The experiments were conducted during the winter seasons of 2021–2023, both in static snow cover and dynamic avalanche conditions of medium-sized events. Radar measurements were used in conjunction with the particle trajectories and velocities to understand the behaviour of the entire avalanche flow. The dynamic avalanche experiments allowed to identify three distinct particle flow states: (I) initial rapid acceleration, (II) a steady state flow with the highest velocities (9–17 ms −1 ), and (III) a longer deceleration state accompanied by the largest measured rotation rates. The particles tend to travel towards the tail of the avalanche and reach lower velocities compared to the frontal approach velocities deduced from radar measurements (ranging between 23–28 ms −1 ). The presented data give a first insight in avalanche particle measurements.
author2 Deutsche Forschungsgemeinschaft
Austrian Science Fund
format Article in Journal/Newspaper
author Neuhauser, Michael
Köhler, Anselm
Neurauter, Rene
Adams, Marc S.
Fischer, Jan-Thomas
spellingShingle Neuhauser, Michael
Köhler, Anselm
Neurauter, Rene
Adams, Marc S.
Fischer, Jan-Thomas
Particle trajectories, velocities, accelerations and rotation rates in snow avalanches
author_facet Neuhauser, Michael
Köhler, Anselm
Neurauter, Rene
Adams, Marc S.
Fischer, Jan-Thomas
author_sort Neuhauser, Michael
title Particle trajectories, velocities, accelerations and rotation rates in snow avalanches
title_short Particle trajectories, velocities, accelerations and rotation rates in snow avalanches
title_full Particle trajectories, velocities, accelerations and rotation rates in snow avalanches
title_fullStr Particle trajectories, velocities, accelerations and rotation rates in snow avalanches
title_full_unstemmed Particle trajectories, velocities, accelerations and rotation rates in snow avalanches
title_sort particle trajectories, velocities, accelerations and rotation rates in snow avalanches
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/aog.2023.69
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000691
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source Annals of Glaciology
page 1-18
ISSN 0260-3055 1727-5644
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/aog.2023.69
container_title Annals of Glaciology
container_start_page 1
op_container_end_page 18
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