@article{oai:nipr.repo.nii.ac.jp:00003840,
 author = {ゴンダ, タケヒコ and ワダ, マコト and GONDA, Takehiko and WADA, Makoto},
 journal = {Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology},
 month = {Nov},
 note = {P(論文), σ^* is the critical supersaturation where kinetic roughening takes place. When the supersaturation σ<γ^*, prismatic facets are formed at the tips of primary branches of dendritic ice crystal. Then, the side branches are formed as a result of the shape instability of the prismatic facets with changing supersaturation. In the next place, when the supersaturation σ>σ^*, the tip shape of primary branches of dendritic ice crystal becomes round. In this case, the side branches are formed as a result of the change in the tip width of primary branches with changing supersaturation. Snow crystals observed in Antarctica are discussed on the basis of these experimental results.},
 title = {FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE},
 volume = {8},
 year = {1994}
}