Frozen water droplets 20-80 um in diameter were dropped into supercooled clouds produced in a large cloud chamber 6.5m high. They were collected at the bottom of the chamber. They grew to various shapes from spherical frozen particles to hexagonal ice crystals. By observing their shapes, it was possible to estimate the growth process of frozen droplets. A typical case accompanied with the appearance of 20 crystal faces, was observed. They were two basal, six prism and twelve pyramidal faces. In addition to these crystal faces, small (1120) crystal faces were observed between two prism faces in a few cases. Frozen droplets nucleated at low temperatures (below about -20℃), 20 crystal faces were not appeared in most cases. Only two basal faces...
Riming experiments of supercooled droplets on the surface of an ice plate of single crystal were mad...
Abstract. We have investigated the formation of 10-50 mm long “ice spikes ” that sometimes appear on...
Atmospheric ice crystals form from a variety of different sources and at different temperatures. Bet...
[著者版]Growth of frozen water droplets, falling freely in a supercooled cloud, was investigated by usi...
Based on a careful scrutinization of a number of microphotographs of snow crystals taken at Syowa St...
Water droplets 20-80μm in diameter were produced from distilled water. They froze into polycrystalli...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...
This paper describes new laboratory observations about the size evolution of ice crystals and cloud ...
During the work involving snow crystals of low temperature types at Inuvik (68°22′N, 133°42′W), Nort...
Understanding how ice nucleates and grows into larger crystals is of crucial importance for many res...
In-situ observations of needle ice crystals growing in air at 10^5 Pa at -7℃ and at about water satu...
Experiments of formation and growth of ice crystals were carried out in situ observation to examine ...
The morphologies and growth rates of ice crystals have been observed and documented using a novel ex...
Ice crystals were produced in a supercooled cloud by seeding rock-forming minerals and clay minerals...
For the sake of studying the morphology and the growth mode of single snow crystals forming in the p...
Riming experiments of supercooled droplets on the surface of an ice plate of single crystal were mad...
Abstract. We have investigated the formation of 10-50 mm long “ice spikes ” that sometimes appear on...
Atmospheric ice crystals form from a variety of different sources and at different temperatures. Bet...
[著者版]Growth of frozen water droplets, falling freely in a supercooled cloud, was investigated by usi...
Based on a careful scrutinization of a number of microphotographs of snow crystals taken at Syowa St...
Water droplets 20-80μm in diameter were produced from distilled water. They froze into polycrystalli...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...
This paper describes new laboratory observations about the size evolution of ice crystals and cloud ...
During the work involving snow crystals of low temperature types at Inuvik (68°22′N, 133°42′W), Nort...
Understanding how ice nucleates and grows into larger crystals is of crucial importance for many res...
In-situ observations of needle ice crystals growing in air at 10^5 Pa at -7℃ and at about water satu...
Experiments of formation and growth of ice crystals were carried out in situ observation to examine ...
The morphologies and growth rates of ice crystals have been observed and documented using a novel ex...
Ice crystals were produced in a supercooled cloud by seeding rock-forming minerals and clay minerals...
For the sake of studying the morphology and the growth mode of single snow crystals forming in the p...
Riming experiments of supercooled droplets on the surface of an ice plate of single crystal were mad...
Abstract. We have investigated the formation of 10-50 mm long “ice spikes ” that sometimes appear on...
Atmospheric ice crystals form from a variety of different sources and at different temperatures. Bet...