Frost flower formation on sea ice and lake ice
[1] Frost flowers are clusters of ice crystals found on freshly formed sea ice and occasionally on frozen lakes. They belong to a class of vapour-related phenomena that includes freezing fog, hoar frost and dew. It has hitherto been supposed that they form by condensation from a supersaturated atmos...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.586.182 2023-05-15T18:17:15+02:00 Frost flower formation on sea ice and lake ice Robert W. Style M. Grae Worster The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.182 http://www.itg.cam.ac.uk/people/grae/90.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.182 http://www.itg.cam.ac.uk/people/grae/90.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.itg.cam.ac.uk/people/grae/90.pdf text ftciteseerx 2016-01-08T13:16:19Z [1] Frost flowers are clusters of ice crystals found on freshly formed sea ice and occasionally on frozen lakes. They belong to a class of vapour-related phenomena that includes freezing fog, hoar frost and dew. It has hitherto been supposed that they form by condensation from a supersaturated atmosphere or from water wicked up through porous sea ice. Here we show that they can form on solid, pure ice sublimating into an unsaturated atmosphere. We derive a general regime diagram showing the atmospheric conditions under which the different vapour-related phenomena occur and confirm our predictions of frost-flower formation with a series of laboratory experiments. Our results can be used in climate models to predict occurrence of frost flowers, which significantly enhance albedo and provide the substrate for chemical production of ozone-depleting bromine monoxide, and in paleo-climate reconstructions by relating observations of sea-salt aerosols in ice cores to atmospheric conditions. Text Sea ice Unknown |
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ftciteseerx |
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English |
description |
[1] Frost flowers are clusters of ice crystals found on freshly formed sea ice and occasionally on frozen lakes. They belong to a class of vapour-related phenomena that includes freezing fog, hoar frost and dew. It has hitherto been supposed that they form by condensation from a supersaturated atmosphere or from water wicked up through porous sea ice. Here we show that they can form on solid, pure ice sublimating into an unsaturated atmosphere. We derive a general regime diagram showing the atmospheric conditions under which the different vapour-related phenomena occur and confirm our predictions of frost-flower formation with a series of laboratory experiments. Our results can be used in climate models to predict occurrence of frost flowers, which significantly enhance albedo and provide the substrate for chemical production of ozone-depleting bromine monoxide, and in paleo-climate reconstructions by relating observations of sea-salt aerosols in ice cores to atmospheric conditions. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Robert W. Style M. Grae Worster |
spellingShingle |
Robert W. Style M. Grae Worster Frost flower formation on sea ice and lake ice |
author_facet |
Robert W. Style M. Grae Worster |
author_sort |
Robert W. Style |
title |
Frost flower formation on sea ice and lake ice |
title_short |
Frost flower formation on sea ice and lake ice |
title_full |
Frost flower formation on sea ice and lake ice |
title_fullStr |
Frost flower formation on sea ice and lake ice |
title_full_unstemmed |
Frost flower formation on sea ice and lake ice |
title_sort |
frost flower formation on sea ice and lake ice |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.182 http://www.itg.cam.ac.uk/people/grae/90.pdf |
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Sea ice |
genre_facet |
Sea ice |
op_source |
http://www.itg.cam.ac.uk/people/grae/90.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.182 http://www.itg.cam.ac.uk/people/grae/90.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766191355963375616 |