Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water
Abstract Observations made of ice crystals growing on the surface of supercooled water show that they take the form of a composite structure, called surface needles, each of which consists of dendrites growing into the liquid, and of ribs growing in the liquid surface. Each needle is a single crysta...
Published in: | Journal of Glaciology |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1960
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000017998 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017998 |
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author | Hallett, J. |
author_facet | Hallett, J. |
author_sort | Hallett, J. |
collection | Cambridge University Press |
container_issue | 28 |
container_start_page | 698 |
container_title | Journal of Glaciology |
container_volume | 3 |
description | Abstract Observations made of ice crystals growing on the surface of supercooled water show that they take the form of a composite structure, called surface needles, each of which consists of dendrites growing into the liquid, and of ribs growing in the liquid surface. Each needle is a single crystal. The precise form of the needle is determined by the orientation of the initial nucleus. If its optic axis is near normal to the surface, growth occurs rapidly in two dimensions and covers a much larger proportion of the surface than is covered by the narrow surface needles, so that ice forming this way appears to have its optic axis vertical. Hollow ice spikes observed on pools are shown to have been formed by the freezing of water forced from beneath the surface at the intersection of two or three surface needles, the shape of the spike depending on their orientation. |
format | Article in Journal/Newspaper |
genre | Journal of Glaciology |
genre_facet | Journal of Glaciology |
geographic | The Needle The Spike Needles The |
geographic_facet | The Needle The Spike Needles The |
id | crcambridgeupr:10.1017/s0022143000017998 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-64.047,-64.047,63.267,63.267) ENVELOPE(-37.317,-37.317,-54.017,-54.017) ENVELOPE(-70.967,-70.967,-68.950,-68.950) |
op_collection_id | crcambridgeupr |
op_container_end_page | 704 |
op_doi | https://doi.org/10.1017/s0022143000017998 |
op_source | Journal of Glaciology volume 3, issue 28, page 698-704 ISSN 0022-1430 1727-5652 |
publishDate | 1960 |
publisher | Cambridge University Press (CUP) |
record_format | openpolar |
spelling | crcambridgeupr:10.1017/s0022143000017998 2025-01-16T22:46:47+00:00 Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water Hallett, J. 1960 http://dx.doi.org/10.1017/s0022143000017998 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017998 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 28, page 698-704 ISSN 0022-1430 1727-5652 journal-article 1960 crcambridgeupr https://doi.org/10.1017/s0022143000017998 2024-07-31T04:04:11Z Abstract Observations made of ice crystals growing on the surface of supercooled water show that they take the form of a composite structure, called surface needles, each of which consists of dendrites growing into the liquid, and of ribs growing in the liquid surface. Each needle is a single crystal. The precise form of the needle is determined by the orientation of the initial nucleus. If its optic axis is near normal to the surface, growth occurs rapidly in two dimensions and covers a much larger proportion of the surface than is covered by the narrow surface needles, so that ice forming this way appears to have its optic axis vertical. Hollow ice spikes observed on pools are shown to have been formed by the freezing of water forced from beneath the surface at the intersection of two or three surface needles, the shape of the spike depending on their orientation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press The Needle ENVELOPE(-64.047,-64.047,63.267,63.267) The Spike ENVELOPE(-37.317,-37.317,-54.017,-54.017) Needles The ENVELOPE(-70.967,-70.967,-68.950,-68.950) Journal of Glaciology 3 28 698 704 |
spellingShingle | Hallett, J. Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water |
title | Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water |
title_full | Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water |
title_fullStr | Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water |
title_full_unstemmed | Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water |
title_short | Crystal Growth and the Formation of Spikes in the Surface of Supercooled Water |
title_sort | crystal growth and the formation of spikes in the surface of supercooled water |
url | http://dx.doi.org/10.1017/s0022143000017998 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017998 |