VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE

Drifting snow experiments in a cold wind tunnel were conducted to investigate impact and ejection velocities and angles of snow particles as functions of friction velocity from 0.15 to 0.39m/s. Disintegrated particles of natural compact snow were used. Trajectories of snow particles were illuminated...

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Main Authors: スギウラ コノスケ, ニシムラ コウイチ, マエノ ノリカズ, Konosuke SUGIURA, Kouichi NISHIMURA, Norikazu MAENO
Format: Report
Language:English
Published: Institute of Low Temperature Science, Hokkaido University 1997
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Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3975
http://id.nii.ac.jp/1291/00003975/
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003975 2023-05-15T18:02:11+02:00 VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE スギウラ コノスケ ニシムラ コウイチ マエノ ノリカズ Konosuke SUGIURA Kouichi NISHIMURA Norikazu MAENO 1997-11 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3975 http://id.nii.ac.jp/1291/00003975/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3975&item_no=1&attribute_id=18&file_no=1 en eng Institute of Low Temperature Science, Hokkaido University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3975 http://id.nii.ac.jp/1291/00003975/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 11, 108-116(1997-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3975&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1997 ftnipr 2022-12-31T19:49:35Z Drifting snow experiments in a cold wind tunnel were conducted to investigate impact and ejection velocities and angles of snow particles as functions of friction velocity from 0.15 to 0.39m/s. Disintegrated particles of natural compact snow were used. Trajectories of snow particles were illuminated with a laser sheet cut with a rotary shutter and were recorded with a video camera system. Both average impact and ejection velocities increased with the friction velocity. However, average impact and ejection angles decreased. Standard deviations of the ejection angles were larger than those of the impact angles. Average horizontal components of both the impact and ejection velocities increased with the friction velocity, while average vertical components did not change much. In general, faster particles had smaller impact angles and slower particles had larger angles. The ratio of the average ejection velocity to the average impact velocity, that is the restitution coefficient, increased with the friction velocity. The vertical restitution coefficient ranged from 1.5 to 2.3,showing the increase of vertical ejection velocity at each impact. The results were discussed in comparison with those of previous studies including sand particles, and it was concluded that the overall characteristics of a loose snow surface at impact are similar to those of a sand surface in spite of different materials. Report Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description Drifting snow experiments in a cold wind tunnel were conducted to investigate impact and ejection velocities and angles of snow particles as functions of friction velocity from 0.15 to 0.39m/s. Disintegrated particles of natural compact snow were used. Trajectories of snow particles were illuminated with a laser sheet cut with a rotary shutter and were recorded with a video camera system. Both average impact and ejection velocities increased with the friction velocity. However, average impact and ejection angles decreased. Standard deviations of the ejection angles were larger than those of the impact angles. Average horizontal components of both the impact and ejection velocities increased with the friction velocity, while average vertical components did not change much. In general, faster particles had smaller impact angles and slower particles had larger angles. The ratio of the average ejection velocity to the average impact velocity, that is the restitution coefficient, increased with the friction velocity. The vertical restitution coefficient ranged from 1.5 to 2.3,showing the increase of vertical ejection velocity at each impact. The results were discussed in comparison with those of previous studies including sand particles, and it was concluded that the overall characteristics of a loose snow surface at impact are similar to those of a sand surface in spite of different materials.
format Report
author スギウラ コノスケ
ニシムラ コウイチ
マエノ ノリカズ
Konosuke SUGIURA
Kouichi NISHIMURA
Norikazu MAENO
spellingShingle スギウラ コノスケ
ニシムラ コウイチ
マエノ ノリカズ
Konosuke SUGIURA
Kouichi NISHIMURA
Norikazu MAENO
VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE
author_facet スギウラ コノスケ
ニシムラ コウイチ
マエノ ノリカズ
Konosuke SUGIURA
Kouichi NISHIMURA
Norikazu MAENO
author_sort スギウラ コノスケ
title VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE
title_short VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE
title_full VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE
title_fullStr VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE
title_full_unstemmed VELOCITY AND ANGLE DISTRIBUTIONS OF DRIFTING SNOW PARTICLES NEAR THE LOSSE SNOW SURFACE
title_sort velocity and angle distributions of drifting snow particles near the losse snow surface
publisher Institute of Low Temperature Science, Hokkaido University
publishDate 1997
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3975
http://id.nii.ac.jp/1291/00003975/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3975&item_no=1&attribute_id=18&file_no=1
genre Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3975
http://id.nii.ac.jp/1291/00003975/
AA10756213
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 11, 108-116(1997-11)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3975&item_no=1&attribute_id=18&file_no=1
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