Evaporation of snow crystals and snowflakes (abstract)
Experiments to evaporate natural snow crystals and snowflakes under a polarization microscope were carried out at Sapporo in 1987. Evaporation of snow crystals and snowflakes occurred preferentially at pointed ends and shapes of evaporating crystals were similar to their growth forms although their...
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Osaka Kyoiku University
1989
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ftnipr:oai:nipr.repo.nii.ac.jp:00003586 2023-05-15T18:02:10+02:00 Evaporation of snow crystals and snowflakes (abstract) Akira Yamashita Hiroyuki Konishi Wataru Shimada 1989-08 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3586 http://id.nii.ac.jp/1291/00003586/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3586&item_no=1&attribute_id=18&file_no=1 en eng Osaka Kyoiku University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3586 http://id.nii.ac.jp/1291/00003586/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 2, 174(1989-08) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3586&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1989 ftnipr 2022-12-10T19:45:40Z Experiments to evaporate natural snow crystals and snowflakes under a polarization microscope were carried out at Sapporo in 1987. Evaporation of snow crystals and snowflakes occurred preferentially at pointed ends and shapes of evaporating crystals were similar to their growth forms although their pointed ends had rather rounded surfaces. However, the following two kinds of phenomena were also observed when dendrites, rimed plates and irregular poly-crystals were evaporated at -3∿-9 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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ftnipr |
language |
English |
description |
Experiments to evaporate natural snow crystals and snowflakes under a polarization microscope were carried out at Sapporo in 1987. Evaporation of snow crystals and snowflakes occurred preferentially at pointed ends and shapes of evaporating crystals were similar to their growth forms although their pointed ends had rather rounded surfaces. However, the following two kinds of phenomena were also observed when dendrites, rimed plates and irregular poly-crystals were evaporated at -3∿-9 |
format |
Report |
author |
Akira Yamashita Hiroyuki Konishi Wataru Shimada |
spellingShingle |
Akira Yamashita Hiroyuki Konishi Wataru Shimada Evaporation of snow crystals and snowflakes (abstract) |
author_facet |
Akira Yamashita Hiroyuki Konishi Wataru Shimada |
author_sort |
Akira Yamashita |
title |
Evaporation of snow crystals and snowflakes (abstract) |
title_short |
Evaporation of snow crystals and snowflakes (abstract) |
title_full |
Evaporation of snow crystals and snowflakes (abstract) |
title_fullStr |
Evaporation of snow crystals and snowflakes (abstract) |
title_full_unstemmed |
Evaporation of snow crystals and snowflakes (abstract) |
title_sort |
evaporation of snow crystals and snowflakes (abstract) |
publisher |
Osaka Kyoiku University |
publishDate |
1989 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3586 http://id.nii.ac.jp/1291/00003586/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3586&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=3586 http://id.nii.ac.jp/1291/00003586/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 2, 174(1989-08) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3586&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766171939665084416 |