@article{oai:nipr.repo.nii.ac.jp:00003974,
 author = {ゴンダ, タケヒコ and マツウラ, ユキ and GONDA, Takehiko and MATSUURA, Yuki},
 journal = {Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology},
 month = {Nov},
 note = {P(論文), 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.},
 pages = {103--107},
 title = {IN SITU OBSERVATION OF EVAPORATING ICE CRYSTALS BY LASER TWO-BEAM INTERFEROMETRY},
 volume = {11},
 year = {1997}
}