IN SITU OBSERVATION OF EVAPORATING ICE CRYSTALS BY LASER TWO-BEAM INTERFEROMETRY
The evaporation rate of a polyhedral ice crystal is several times larger than the growth rate. The reason is because the slope of an evaporation pit P_e of the ice crystal is larger than the slope of a growth hillock P_g in addition to the increase of active sites of evaporation. The former means th...
Main Authors: | , , , |
---|---|
Format: | Report |
Language: | English |
Published: |
Division of General Education, Aichi Gakuin University
1997
|
Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3974 http://id.nii.ac.jp/1291/00003974/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3974&item_no=1&attribute_id=18&file_no=1 |
Summary: | The evaporation rate of a polyhedral ice crystal is several times larger than the growth rate. The reason is because the slope of an evaporation pit P_e of the ice crystal is larger than the slope of a growth hillock P_g in addition to the increase of active sites of evaporation. The former means that the step separation of the evaporation pit λ_e is smaller than that of the growth hillock λ_g. |
---|