HUSCAP logo Hokkaido Univ. logo

Hokkaido University Collection of Scholarly and Academic Papers >
理学院・理学研究院  >
雑誌発表論文等  >

Topographic effects on the thermal structure of Himalayan glacial lakes : Observations and numerical simulation of wind

フルテキスト
JAES30-2.pdf1.07 MBPDF見る/開く
この文献へのリンクには次のURLを使用してください:http://hdl.handle.net/2115/28230

タイトル: Topographic effects on the thermal structure of Himalayan glacial lakes : Observations and numerical simulation of wind
著者: Chikita, Kazuhisa A. 著作を一覧する
キーワード: Glacial lakes
Nepal Himalayas
Thermal structure
Wind-driven currents
Calving
発行日: 2007年 4月20日
出版者: Elsevier Ltd.
誌名: Journal of Asian Earth Sciences
巻: 30
号: 2
開始ページ: 344
終了ページ: 352
出版社 DOI: 10.1016/j.jseaes.2006.10.005
抄録: The thermal structure of two Himalayan glacial lakes, Tsho Rolpa and Imja in the eastern Nepal, was examined by observations in the pre-monsoon seasons of 1996 and 1997. Tsho Rolpa had an isothermal mixed layer at water depths of 0–20 m, whereas Imja did not possess such an isothermal layer. This difference in the thermal structure is explained by the condition that diurnal valley winds, producing wind-driven currents, blow strongly near the water surface of Tsho Rolpa, but very weakly near that of Imja. The wind observations above or near the end moraine indicated that a daily wind system of strong, diurnal valley winds and weak, nocturnal mountain winds is common to the lakes. It was suggested that with respect to the valley winds, the weak winds near the surface of Imja result from topographic screening effects of the upwind dead-ice zone and end moraine 20–25 m higher than the water surface. In order to ascertain the topographic effects, three-dimensional numerical simulation of airflow was carried out by making topographic models of actual size in the calculation domain, corresponding to Tsho Rolpa and Imja and their surrounding topography. The simulation revealed that, when winds blow at constant velocities of 1–5 m s−1 at 2 m above the points corresponding to the weather stations, the wind velocity at 2 m above the water surface for Imja is 33–42% smaller than for Tsho Rolpa. With increasing heights of the end moraine and dead-ice zone, the wind velocity near the lake surface efficiently decreased by decreasing the lake length from 3.1 or 2.2 km to 1.2 km.
関連URI: http://www.sciencedirect.com/science/journal/13679120
資料タイプ: article (author version)
URI: http://hdl.handle.net/2115/28230
出現コレクション:雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

提供者: 知北 和久

 

本サイトに関するご意見・お問い合わせは repo at lib.hokudai.ac.jp へお願いします。 - 北海道大学