HUSCAP logo Hokkaido Univ. logo

Hokkaido University Collection of Scholarly and Academic Papers >
環境科学院・地球環境科学研究院  >
雑誌発表論文等  >

Diurnal Variations in Lower-Tropospheric Wind over Japan Part I: Observational Results using the Wind Profiler Network and Data Acquisition System (WINDAS)

フルテキスト
JMSJ88-3_325-347.pdf2.07 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/2115/44056

タイトル: Diurnal Variations in Lower-Tropospheric Wind over Japan Part I: Observational Results using the Wind Profiler Network and Data Acquisition System (WINDAS)
著者: Sakazaki, Takatoshi 著作を一覧する
Fujiwara, Masatomo 著作を一覧する
発行日: 2010年 7月21日
出版者: Meteorological Society of Japan
誌名: Journal of the Meteorological Society of Japan
巻: 88
号: 3
開始ページ: 325
終了ページ: 347
出版社 DOI: 10.2151/jmsj.2010-305
抄録: This study investigates diurnal variations in lower-tropospheric wind over Japan during 2002-2008 using data from 31 stations of the Wind profiler Network and Data Acquisition System (WINDAS) and the Automated Meteorological Data Acquisition System (AMeDAS). The diurnal and semidiurnal components are extracted and analyzed to identify the dominant processes for each height range and for each season. Near the surface, the diurnal component is controlled by local wind systems (e.g., land-sea breezes) throughout the year. At 1-3 km, the diurnal component is primarily controlled by the return currents of local wind systems, with additional influence by other disturbances; the superposition of these two wind systems generates amplitude maxima in spring (∼0.5 m s^[-1]) and autumn (∼0.6 m s^[-1]). At 3-5 km, the diurnal wind in DJF-MAM is controlled by medium-scale eastward traveling waves, which generate the amplitude maximum (∼0.8 m s^[-1]) in winter-spring. In JJA-SON, the diurnal component is controlled by a large-scale wind system with an amplitude of ∼0.3 m s^[-1], probably related to the diurnal tide. At stations located on small islands located south of the Japanese mainland, the diurnal wind within the lower troposphere has different characteristics from those described above throughout the year. Throughout Japan, the semidiurnal wind component is controlled by the semidiurnal migrating tide above ∼1 km, and is influenced by local wind systems below ∼1 km. The amplitude of the semidiurnal tide below 5 km is largest in DJF (∼0.4 m s^[-1]) and smallest in JJA (∼0.2 m s^[-1]).
資料タイプ: article
URI: http://hdl.handle.net/2115/44056
出現コレクション:雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

提供者: 坂崎 貴俊

 

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