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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Institute of Low Temperature Science, Hokkaido University
1997
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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 |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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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 |
_version_ |
1766171964539404288 |