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...

Full description

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
Description
Summary: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.