Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica

To study snowdrift formation behind elevated buildings, wind-tunnel experiments were carried out, using activated clay particles to simulate snow, on a 1/100 scale model of the observation hut at Syowa Station. The similitude of snowdrift for the model and the actual prototype was obtained precisely...

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Bibliographic Details
Main Authors: Tsukasa Tomabechi, Akihisa Endo
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1985
Subjects:
geo
Online Access:https://doi.org/10.15094/00008442
https://doaj.org/article/8a1b4d1ce0984bc3833d782cfe22b60e
id fttriple:oai:gotriple.eu:oai:doaj.org/article:8a1b4d1ce0984bc3833d782cfe22b60e
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:8a1b4d1ce0984bc3833d782cfe22b60e 2023-05-15T13:32:55+02:00 Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica Tsukasa Tomabechi Akihisa Endo 1985-03-01 https://doi.org/10.15094/00008442 https://doaj.org/article/8a1b4d1ce0984bc3833d782cfe22b60e en other eng National Institute of Polar Research doi:10.15094/00008442 0085-7289 2432-079X https://doaj.org/article/8a1b4d1ce0984bc3833d782cfe22b60e undefined Antarctic Record, Iss 84, Pp 114-119 (1985) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1985 fttriple https://doi.org/10.15094/00008442 2023-01-22T19:30:37Z To study snowdrift formation behind elevated buildings, wind-tunnel experiments were carried out, using activated clay particles to simulate snow, on a 1/100 scale model of the observation hut at Syowa Station. The similitude of snowdrift for the model and the actual prototype was obtained precisely when the tunnel wind-speed and the wind duration were 5.0m/s and 2.5 hours, respectively. This modeling technique using activated clay particles is proved to be useful for further studies on the most appropriate shape and dimensions of elevated buildings to prevent snowdrift. Article in Journal/Newspaper Antarc* Antarctica Unknown Syowa Station
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Tsukasa Tomabechi
Akihisa Endo
Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica
topic_facet geo
description To study snowdrift formation behind elevated buildings, wind-tunnel experiments were carried out, using activated clay particles to simulate snow, on a 1/100 scale model of the observation hut at Syowa Station. The similitude of snowdrift for the model and the actual prototype was obtained precisely when the tunnel wind-speed and the wind duration were 5.0m/s and 2.5 hours, respectively. This modeling technique using activated clay particles is proved to be useful for further studies on the most appropriate shape and dimensions of elevated buildings to prevent snowdrift.
format Article in Journal/Newspaper
author Tsukasa Tomabechi
Akihisa Endo
author_facet Tsukasa Tomabechi
Akihisa Endo
author_sort Tsukasa Tomabechi
title Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica
title_short Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica
title_full Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica
title_fullStr Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica
title_full_unstemmed Wind-tunnel experiments of snowdrift formation behind an elevated building at Syowa Station, Antarctica
title_sort wind-tunnel experiments of snowdrift formation behind an elevated building at syowa station, antarctica
publisher National Institute of Polar Research
publishDate 1985
url https://doi.org/10.15094/00008442
https://doaj.org/article/8a1b4d1ce0984bc3833d782cfe22b60e
geographic Syowa Station
geographic_facet Syowa Station
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Antarctic Record, Iss 84, Pp 114-119 (1985)
op_relation doi:10.15094/00008442
0085-7289
2432-079X
https://doaj.org/article/8a1b4d1ce0984bc3833d782cfe22b60e
op_rights undefined
op_doi https://doi.org/10.15094/00008442
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