Simulation of ice accretion on a cylinder due to freezing rain

Abstract A hybrid analytical and random-walk model has been developed to predict the shape of ice accreted on a horizontal cylindrical insulator due to freezing rain. The freezing rain occurs with the temperature of the vertically falling raindrops above the freezing point and the air temperature be...

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Published in:Journal of Glaciology
Main Author: Szilder, Krzysztof
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1994
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000012478
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012478
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spelling crcambridgeupr:10.1017/s0022143000012478 2024-09-15T18:15:38+00:00 Simulation of ice accretion on a cylinder due to freezing rain Szilder, Krzysztof 1994 http://dx.doi.org/10.1017/s0022143000012478 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012478 en eng Cambridge University Press (CUP) Journal of Glaciology volume 40, issue 136, page 586-594 ISSN 0022-1430 1727-5652 journal-article 1994 crcambridgeupr https://doi.org/10.1017/s0022143000012478 2024-08-14T04:02:34Z Abstract A hybrid analytical and random-walk model has been developed to predict the shape of ice accreted on a horizontal cylindrical insulator due to freezing rain. The freezing rain occurs with the temperature of the vertically falling raindrops above the freezing point and the air temperature below freezing. The analytical model calculates the angular distribution of the water-film temperature and the location where freezing begins. The random-walk model predicts the accretion shape. The two random-walk model parameters, the freezing probability and the shedding parameter, are expressed as functions of the atmospheric conditions. The model predicts a variety of realistic accretion shapes from cylindrical to icicle-like. Model verification based on comparisons with other models and with experimental results demonstrates quantitatively and qualitatively the credibility of this new modelling approach. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 40 136 586 594
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract A hybrid analytical and random-walk model has been developed to predict the shape of ice accreted on a horizontal cylindrical insulator due to freezing rain. The freezing rain occurs with the temperature of the vertically falling raindrops above the freezing point and the air temperature below freezing. The analytical model calculates the angular distribution of the water-film temperature and the location where freezing begins. The random-walk model predicts the accretion shape. The two random-walk model parameters, the freezing probability and the shedding parameter, are expressed as functions of the atmospheric conditions. The model predicts a variety of realistic accretion shapes from cylindrical to icicle-like. Model verification based on comparisons with other models and with experimental results demonstrates quantitatively and qualitatively the credibility of this new modelling approach.
format Article in Journal/Newspaper
author Szilder, Krzysztof
spellingShingle Szilder, Krzysztof
Simulation of ice accretion on a cylinder due to freezing rain
author_facet Szilder, Krzysztof
author_sort Szilder, Krzysztof
title Simulation of ice accretion on a cylinder due to freezing rain
title_short Simulation of ice accretion on a cylinder due to freezing rain
title_full Simulation of ice accretion on a cylinder due to freezing rain
title_fullStr Simulation of ice accretion on a cylinder due to freezing rain
title_full_unstemmed Simulation of ice accretion on a cylinder due to freezing rain
title_sort simulation of ice accretion on a cylinder due to freezing rain
publisher Cambridge University Press (CUP)
publishDate 1994
url http://dx.doi.org/10.1017/s0022143000012478
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012478
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 40, issue 136, page 586-594
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000012478
container_title Journal of Glaciology
container_volume 40
container_issue 136
container_start_page 586
op_container_end_page 594
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