Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snow

A snow drift survey around buildings in the wake of the central building of Syowa Station was carried out from February to November 2002. Wind was measured at two points above the roofs of buildings simultaneously. Measurement of mass flux of snow 0.5 m alone the ground was carried out in an undistu...

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Main Authors: Hiroki Takahashi, Toshio Hannuki, Masaru Ayukawa, Osamu Abe
Format: Article
Language:English
Published: National Institute of Polar Research 2005-07-01
Series:Antarctic Record
Online Access:http://doi.org/10.15094/00009323
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spelling doaj-904e6a23ce0a47459bf38652641e705d2020-11-24T23:08:36ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X2005-07-0149214518110.15094/00009323 Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snowHiroki Takahashi0Toshio Hannuki1Masaru Ayukawa2Osamu Abe3Student, Graduate School of Science and Technology, Nihon UniversityCollege of Science and Technology, Nihon UniversityNational Institute of Polar ResearchNational Research Institute for Earth Science and Disaster PreventionA snow drift survey around buildings in the wake of the central building of Syowa Station was carried out from February to November 2002. Wind was measured at two points above the roofs of buildings simultaneously. Measurement of mass flux of snow 0.5 m alone the ground was carried out in an undisturbed spot away from the main part of Syowa Station. Studying these observation data, it was found that the relation between the mass flux of snow and the volume of snow deposition around buildings can be expressed simply in a linear equation. And it was confirmed that the form of snow drift was sensitive to the properties of wind. The wind tunnel test was performed with a 1/100 scale model of the main part of Syowa Station. The blowing snow was modeled with artificial snow in a wind tunnel. The growth of snow deposition around the building models was measured at regular intervals. Variations of the shape of snow drift were observed in the wake especially. In comparison with the snow drift survey at Syowa Station, similarity of snow deposition on the wake of the obstacles was confirmed. The wind tunnel test with artificial snow was useful as a supplement to the field observations.http://doi.org/10.15094/00009323
collection DOAJ
language English
format Article
sources DOAJ
author Hiroki Takahashi
Toshio Hannuki
Masaru Ayukawa
Osamu Abe
spellingShingle Hiroki Takahashi
Toshio Hannuki
Masaru Ayukawa
Osamu Abe
Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snow
Antarctic Record
author_facet Hiroki Takahashi
Toshio Hannuki
Masaru Ayukawa
Osamu Abe
author_sort Hiroki Takahashi
title Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snow
title_short Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snow
title_full Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snow
title_fullStr Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snow
title_full_unstemmed Snowdrift observation around buildings in the wake of the central building of Syowa Station and a cold wind tunnel test with artificial snow
title_sort snowdrift observation around buildings in the wake of the central building of syowa station and a cold wind tunnel test with artificial snow
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 2005-07-01
description A snow drift survey around buildings in the wake of the central building of Syowa Station was carried out from February to November 2002. Wind was measured at two points above the roofs of buildings simultaneously. Measurement of mass flux of snow 0.5 m alone the ground was carried out in an undisturbed spot away from the main part of Syowa Station. Studying these observation data, it was found that the relation between the mass flux of snow and the volume of snow deposition around buildings can be expressed simply in a linear equation. And it was confirmed that the form of snow drift was sensitive to the properties of wind. The wind tunnel test was performed with a 1/100 scale model of the main part of Syowa Station. The blowing snow was modeled with artificial snow in a wind tunnel. The growth of snow deposition around the building models was measured at regular intervals. Variations of the shape of snow drift were observed in the wake especially. In comparison with the snow drift survey at Syowa Station, similarity of snow deposition on the wake of the obstacles was confirmed. The wind tunnel test with artificial snow was useful as a supplement to the field observations.
url http://doi.org/10.15094/00009323
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