@article{oai:nipr.repo.nii.ac.jp:00009323,
 author = {高橋, 弘樹 and 半貫, 敏夫 and 鮎川, 勝 and 阿部, 修 and Takahashi, Hiroki and Hannuki,  Toshio and Ayukawa, Masaru and Abe, Osamu},
 issue = {2},
 journal = {南極資料, Antarctic Record},
 month = {Jul},
 note = {P(論文), 2002年2月から11月にかけて,昭和基地主要部の管理棟後流域にある倉庫棟及び汚水処理棟周辺に発生した吹きだまりの観測を行った.併せて昭和基地主要部の建物近傍2点で風向・風速を観測し,地上高度0.5 mの吹雪フラックスを計測した.これらの観測データをもとに,吹雪フラックスに対応した吹きだまりの堆積状況を明らかにし,ブリザードの主風向変動が建物周囲の吹きだまり形成に与える影響をまとめた.更に昭和基地主要部周辺を1/100模型によってモデル化した人工雪風洞実験を行って吹きだまり発生状況の再現を試み,その発生と成長の機構を考察した., 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.},
 pages = {145--181},
 title = {昭和基地管理棟後流域建物周辺の吹きだまり観測と 人工雪を用いた風洞模型実験},
 volume = {49},
 year = {2005},
 yomi = {タカハシ, ヒロキ and ハンヌキ, トシオ and アユカワ, マサル and アベ, オサム}
}