Temperature gradient snow metamorphosis

This note shows how the rate of ice crystal growth during temperature gradient metamorphosis can be calculated using irreversible thermodynamics. The method describes the transfer of mass as a consequence of heat transfer. The main heat transfer is the latent heat change by condensing and freezing....

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Published in:Polar Research
Main Author: Ratkje, Signe Kjelstrup
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 1985
Subjects:
Polar Research
Online Access:https://polarresearch.net/index.php/polar/article/view/2520
https://doi.org/10.3402/polar.v3i2.6947
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spelling ftjpolarres:oai:journals.openacademia.net:article/2520 2023-05-15T18:02:40+02:00 Temperature gradient snow metamorphosis Ratkje, Signe Kjelstrup 1985-01-12 application/pdf https://polarresearch.net/index.php/polar/article/view/2520 https://doi.org/10.3402/polar.v3i2.6947 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2520/5771 https://polarresearch.net/index.php/polar/article/view/2520 doi:10.3402/polar.v3i2.6947 Copyright (c) 2018 Polar Research Polar Research; Vol. 3 No. 2 (1985); 141-143 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1985 ftjpolarres https://doi.org/10.3402/polar.v3i2.6947 2021-11-11T19:12:57Z This note shows how the rate of ice crystal growth during temperature gradient metamorphosis can be calculated using irreversible thermodynamics. The method describes the transfer of mass as a consequence of heat transfer. The main heat transfer is the latent heat change by condensing and freezing. Local equilibrium and no convection is assumed. The transport equation, with the temperature gradient as the force of transport, predicts mass transfer measurements. Article in Journal/Newspaper Polar Research Polar Research (E-Journal) Polar Research 3 2 141 143
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description This note shows how the rate of ice crystal growth during temperature gradient metamorphosis can be calculated using irreversible thermodynamics. The method describes the transfer of mass as a consequence of heat transfer. The main heat transfer is the latent heat change by condensing and freezing. Local equilibrium and no convection is assumed. The transport equation, with the temperature gradient as the force of transport, predicts mass transfer measurements.
format Article in Journal/Newspaper
author Ratkje, Signe Kjelstrup
spellingShingle Ratkje, Signe Kjelstrup
Temperature gradient snow metamorphosis
author_facet Ratkje, Signe Kjelstrup
author_sort Ratkje, Signe Kjelstrup
title Temperature gradient snow metamorphosis
title_short Temperature gradient snow metamorphosis
title_full Temperature gradient snow metamorphosis
title_fullStr Temperature gradient snow metamorphosis
title_full_unstemmed Temperature gradient snow metamorphosis
title_sort temperature gradient snow metamorphosis
publisher Norwegian Polar Institute
publishDate 1985
url https://polarresearch.net/index.php/polar/article/view/2520
https://doi.org/10.3402/polar.v3i2.6947
genre Polar Research
genre_facet Polar Research
op_source Polar Research; Vol. 3 No. 2 (1985); 141-143
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2520/5771
https://polarresearch.net/index.php/polar/article/view/2520
doi:10.3402/polar.v3i2.6947
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v3i2.6947
container_title Polar Research
container_volume 3
container_issue 2
container_start_page 141
op_container_end_page 143
_version_ 1766173105956323328

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