In-situ observations of needle ice crystals growing in air at 10^5 Pa at -7℃ and at about water saturation and above water saturation were performed to study the formation process of the branches of needle ice crystals. At about water saturation, six branches with boomerang-like facets are formed after the formation of a thin wall with basal facet along the edge of the basal plane by bunching of steps formed by two-dimensional nucleation at each corner on the basal plane. As time elapses, these branches change into sheath-like branches. Above water saturation, six branches with round tips grow along the c-axis because adhesive growth occurs at each corner on the basal plane. As the ice crystal grows further, these branches change into sheat...
We describe an experimental apparatus for making detailed morphological observations of the growth o...
Abstract. We propose a new type of morphological instability in the diffusion-limited growth of face...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...
Frozen water droplets 20-80 um in diameter were dropped into supercooled clouds produced in a large ...
The morphologies and growth rates of ice crystals have been observed and documented using a novel ex...
σ^* is the critical supersaturation where kinetic roughening takes place. When the supersaturation σ...
During the work involving snow crystals of low temperature types at Inuvik (68°22′N, 133°42′W), Nort...
The morphological instability and the growth mechanism of ice crystals grown in air at -30℃ and at s...
Single ice crystals have been grown in air at various constant pressures at -30℃ and various constan...
The supersaturation dependences on the slope of growth hillocks formed on the {1010} face P_P and th...
The growth mechanisms of long prisms with skeletal structures precipitating in the polar regions are...
It has been found that on very rare occasions long, thin ice needles grow into the air from the soli...
The evaporation form and the evaporation mechanism of dendritic ice crystals grown in air of 1.0×(10...
Experiments of formation and growth of ice crystals were carried out in situ observation to examine ...
[著者版]Growth of frozen water droplets, falling freely in a supercooled cloud, was investigated by usi...
We describe an experimental apparatus for making detailed morphological observations of the growth o...
Abstract. We propose a new type of morphological instability in the diffusion-limited growth of face...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...
Frozen water droplets 20-80 um in diameter were dropped into supercooled clouds produced in a large ...
The morphologies and growth rates of ice crystals have been observed and documented using a novel ex...
σ^* is the critical supersaturation where kinetic roughening takes place. When the supersaturation σ...
During the work involving snow crystals of low temperature types at Inuvik (68°22′N, 133°42′W), Nort...
The morphological instability and the growth mechanism of ice crystals grown in air at -30℃ and at s...
Single ice crystals have been grown in air at various constant pressures at -30℃ and various constan...
The supersaturation dependences on the slope of growth hillocks formed on the {1010} face P_P and th...
The growth mechanisms of long prisms with skeletal structures precipitating in the polar regions are...
It has been found that on very rare occasions long, thin ice needles grow into the air from the soli...
The evaporation form and the evaporation mechanism of dendritic ice crystals grown in air of 1.0×(10...
Experiments of formation and growth of ice crystals were carried out in situ observation to examine ...
[著者版]Growth of frozen water droplets, falling freely in a supercooled cloud, was investigated by usi...
We describe an experimental apparatus for making detailed morphological observations of the growth o...
Abstract. We propose a new type of morphological instability in the diffusion-limited growth of face...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...