ドップラーソーダによる東京都心部の春季における風の日変化の観測
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概要
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The purpose of this study is to elucidate the wind field at the time of fine weather in Kanto Plain. We haveobserved the wind profile in the surface boundary layer using Doppler Sodar. It is located in the Tokyo bay coastsince August, 2003. When the migratory anticyclone covered Japan, and the temperature difference in the daytimeand nighttime was remarkable, two types of wind profile, sea breeze, land breeze was measured. And, these windprofiles showed daily variation. During the transition from the land breeze to the sea breeze, the wind directionchanged from northerly to southerly. And during the transition from the sea breeze to the land breeze, the winddirection changed from southerly to northerly. In this paper, the relationship between sea breeze and land breeze isdiscussed.
- 一般社団法人 日本風工学会の論文
一般社団法人 日本風工学会 | 論文
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