EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM
The evaporation form and the evaporation mechanism of dendritic ice crystals grown in air of 1.0×(10)^5 Pa and at water saturation and polyhedral ice crystals grown in air of 4.0×10 Pa and at relatively low supersaturation are studied. In the case of dendritic ice crystals, the evaporation preferent...
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Faculty of Science and Technology, Science University of Tokyo
1987
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ftnipr:oai:nipr.repo.nii.ac.jp:00003529 2023-05-15T13:49:00+02:00 EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM ゴンダ タケヒコ セイ タダノリ Takehiko GONDA Tadanori SEI 1987-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3529 http://id.nii.ac.jp/1291/00003529/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3529&item_no=1&attribute_id=18&file_no=1 en eng Faculty of Science and Technology, Science University of Tokyo National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3529 http://id.nii.ac.jp/1291/00003529/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 1, 113-121(1987-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3529&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1987 ftnipr 2022-12-10T19:45:40Z The evaporation form and the evaporation mechanism of dendritic ice crystals grown in air of 1.0×(10)^5 Pa and at water saturation and polyhedral ice crystals grown in air of 4.0×10 Pa and at relatively low supersaturation are studied. In the case of dendritic ice crystals, the evaporation preferentially occurs in the convex parts of the crystal surfaces and in minute secondary branches. On the other hand, in the case of polyhedral ice crystals, the evaporation preferentially occurs in the parts where screw dislocations or stacking faults emerge. On the basis of these experimental results, the formation mechanism of single bullets observed at Mizuho Station, Antarctica is inferred. Report Antarc* Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
The evaporation form and the evaporation mechanism of dendritic ice crystals grown in air of 1.0×(10)^5 Pa and at water saturation and polyhedral ice crystals grown in air of 4.0×10 Pa and at relatively low supersaturation are studied. In the case of dendritic ice crystals, the evaporation preferentially occurs in the convex parts of the crystal surfaces and in minute secondary branches. On the other hand, in the case of polyhedral ice crystals, the evaporation preferentially occurs in the parts where screw dislocations or stacking faults emerge. On the basis of these experimental results, the formation mechanism of single bullets observed at Mizuho Station, Antarctica is inferred. |
format |
Report |
author |
ゴンダ タケヒコ セイ タダノリ Takehiko GONDA Tadanori SEI |
spellingShingle |
ゴンダ タケヒコ セイ タダノリ Takehiko GONDA Tadanori SEI EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM |
author_facet |
ゴンダ タケヒコ セイ タダノリ Takehiko GONDA Tadanori SEI |
author_sort |
ゴンダ タケヒコ |
title |
EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM |
title_short |
EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM |
title_full |
EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM |
title_fullStr |
EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM |
title_full_unstemmed |
EVAPORATION FORM OF ICE CRYSTALS IN SUBSATURATED AIR AND THEIR EVAPORATION MECHANISM |
title_sort |
evaporation form of ice crystals in subsaturated air and their evaporation mechanism |
publisher |
Faculty of Science and Technology, Science University of Tokyo |
publishDate |
1987 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3529 http://id.nii.ac.jp/1291/00003529/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3529&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(44.317,44.317,-70.683,-70.683) ENVELOPE(44.317,44.317,-70.683,-70.683) |
geographic |
Mizuho Mizuho Station |
geographic_facet |
Mizuho Mizuho Station |
genre |
Antarc* Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
genre_facet |
Antarc* Antarctica 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=3529 http://id.nii.ac.jp/1291/00003529/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 1, 113-121(1987-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3529&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250405871747072 |