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...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Hallett, J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1960
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000017998
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017998
_version_ 1821563893667856384
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