IN SITU OBSERVATION OF EVAPORATING ICE CRYSTALS BY LASER TWO-BEAM INTERFEROMETRY

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概要

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• 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.

• 国立極地研究所の論文

著者

• Matsuura Yuki

  Toshiba Corporation Research & Development Center Komukai

• GONDA Takehiko

  Division of General Education, Aichi-Gakuin University

• Gonda Takehiko

  Division Of General Education Aichi Gakuin University

関連論文

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• IN SITU OBSERVATION OF EVAPORATING ICE CRYSTALS BY LASER TWO-BEAM INTERFEROMETRY
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• Growth forms and growth mechanisms of single snow crystals growing at a low temperature
• FORMATION MECHANISM OF PLATE-LIKE ICE CRYSTALS GROWING IN AIR AT LOW TEMPERATURE AND LOW SUPERSATURATION
• FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE
• Formation process of branches of needle ice crystals grown from vapor

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