Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station

The wind tunnel tests were conducted in order to predict profiles of the snowdrift formed around the buildings with the pilotis built at Syowa Station in Antarctica on the following assumptions. That is, assuming that the snow flakes in the wind velocity fields exceeding the certain mean wind veloci...

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Bibliographic Details
Main Authors: Toshio SATO, Toshio HANNUKI
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1978
Subjects:
geo
Online Access:https://doi.org/10.15094/00007992
https://doaj.org/article/189f64bc6b4049f5b5a02520c575e244
id fttriple:oai:gotriple.eu:oai:doaj.org/article:189f64bc6b4049f5b5a02520c575e244
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:189f64bc6b4049f5b5a02520c575e244 2023-05-15T13:36:05+02:00 Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station Toshio SATO Toshio HANNUKI 1978-09-01 https://doi.org/10.15094/00007992 https://doaj.org/article/189f64bc6b4049f5b5a02520c575e244 en other eng National Institute of Polar Research doi:10.15094/00007992 0085-7289 2432-079X https://doaj.org/article/189f64bc6b4049f5b5a02520c575e244 undefined Antarctic Record, Iss 62, Pp 1-22 (1978) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1978 fttriple https://doi.org/10.15094/00007992 2023-01-22T18:19:15Z The wind tunnel tests were conducted in order to predict profiles of the snowdrift formed around the buildings with the pilotis built at Syowa Station in Antarctica on the following assumptions. That is, assuming that the snow flakes in the wind velocity fields exceeding the certain mean wind velocity flow along with the wind and the other snow flakes in those fields not exceeding it tend to accumulate on the ground surface, the profiles of the snowdrift around the buildings can be predicted under the blizzard. The results of the wind tunnel tests (the flow-visualization by means of soap bubbles and the measurement of wind velocity distributions) using two-dimensional models are as follows 1) The profile of the snowdrift changes according to the surface friction velocity of the surface boundary layer U_* and the altitude of the pilotis h. 2) The profile of the snowdrift can be predicted in the division of the wind velocity field at the altitude Z satisfying in U/U_≒0.5. 3) The variation of the snowdrift profile can also be expressed by the index K (eq. 9) of the fluid energy of the mean wind flowing the pilotis. Since the index K is a function of U and h, it is useful for the planning information of buildings. Article in Journal/Newspaper Antarc* Antarctica Unknown Syowa Station
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Toshio SATO
Toshio HANNUKI
Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station
topic_facet geo
description The wind tunnel tests were conducted in order to predict profiles of the snowdrift formed around the buildings with the pilotis built at Syowa Station in Antarctica on the following assumptions. That is, assuming that the snow flakes in the wind velocity fields exceeding the certain mean wind velocity flow along with the wind and the other snow flakes in those fields not exceeding it tend to accumulate on the ground surface, the profiles of the snowdrift around the buildings can be predicted under the blizzard. The results of the wind tunnel tests (the flow-visualization by means of soap bubbles and the measurement of wind velocity distributions) using two-dimensional models are as follows 1) The profile of the snowdrift changes according to the surface friction velocity of the surface boundary layer U_* and the altitude of the pilotis h. 2) The profile of the snowdrift can be predicted in the division of the wind velocity field at the altitude Z satisfying in U/U_≒0.5. 3) The variation of the snowdrift profile can also be expressed by the index K (eq. 9) of the fluid energy of the mean wind flowing the pilotis. Since the index K is a function of U and h, it is useful for the planning information of buildings.
format Article in Journal/Newspaper
author Toshio SATO
Toshio HANNUKI
author_facet Toshio SATO
Toshio HANNUKI
author_sort Toshio SATO
title Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station
title_short Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station
title_full Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station
title_fullStr Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station
title_full_unstemmed Flow-Visualization by Means of Soap Bubbles on Snowdrift around the Huts at Syowa Station
title_sort flow-visualization by means of soap bubbles on snowdrift around the huts at syowa station
publisher National Institute of Polar Research
publishDate 1978
url https://doi.org/10.15094/00007992
https://doaj.org/article/189f64bc6b4049f5b5a02520c575e244
geographic Syowa Station
geographic_facet Syowa Station
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Antarctic Record, Iss 62, Pp 1-22 (1978)
op_relation doi:10.15094/00007992
0085-7289
2432-079X
https://doaj.org/article/189f64bc6b4049f5b5a02520c575e244
op_rights undefined
op_doi https://doi.org/10.15094/00007992
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