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A detailed analysis of the cross-mountain air currents\nis important to understanding the climate in the northwestern inland region\nof the Kanto Plain on the leeward side. In addition, little research has been\nconducted on the role of the gap flow in regard to the winter cross-mountain\nair currents. To address this shortage, advanced meteorological observation\nwas carried out along the channel traversing the Joshin’etsu mountainous\nregion, and that data was used to research the characteristics of the surface\natmosphere along the mountain slopes when winter cross-mountain\nair currents blow. As a result, in the case in which cross-mountain air currents\nwere not blowing, the potential temperature along the mountain slope\ntended to rise with altitude, in both the Sea of Japan side and Pacific Ocean\nside. However, in the case in which cross-mountain air currents were blowing,\nthe potential temperature distribution was nearly uniform on the slope\nof the leeward, Pacific Ocean side, regardless of elevation. The case in\nwhich cross-mountain air currents were blowing had characteristics similar\nto foehn. 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Characteristics of the Potential Temperature Distribution Along Mountain Slopes Experiencing Cross-Mountain Air Currents in the Winter Season
http://hdl.handle.net/11266/6645
http://hdl.handle.net/11266/66453570135a-325a-416f-a4a1-5cccc6df41a6
名前 / ファイル | ライセンス | アクション |
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12_Watarai_P293-312.pdf (3.6 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||||||||||||||
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公開日 | 2019-05-29 | |||||||||||||||||
タイトル | ||||||||||||||||||
言語 | en | |||||||||||||||||
タイトル | Characteristics of the Potential Temperature Distribution Along Mountain Slopes Experiencing Cross-Mountain Air Currents in the Winter Season | |||||||||||||||||
言語 | ||||||||||||||||||
言語 | eng | |||||||||||||||||
資源タイプ | ||||||||||||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_3248 | |||||||||||||||||
資源タイプ | book part | |||||||||||||||||
アクセス権 | ||||||||||||||||||
アクセス権 | open access | |||||||||||||||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||||||||||
著者 |
渡来, 靖
× 渡来, 靖
× 重田, 祥範
× 中川, 清隆
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抄録 | ||||||||||||||||||
内容記述タイプ | Abstract | |||||||||||||||||
内容記述 | In winter, northwesterly winds in the vicinity of Japan are predominant in the winter pressure distribution pattern that characterizes the climate of the environs of Japan, and on the Kanto Plain cross-mountain air currents frequently occur in winter because the winds pass over the Joshin’etsu mountainous region. A detailed analysis of the cross-mountain air currents is important to understanding the climate in the northwestern inland region of the Kanto Plain on the leeward side. In addition, little research has been conducted on the role of the gap flow in regard to the winter cross-mountain air currents. To address this shortage, advanced meteorological observation was carried out along the channel traversing the Joshin’etsu mountainous region, and that data was used to research the characteristics of the surface atmosphere along the mountain slopes when winter cross-mountain air currents blow. As a result, in the case in which cross-mountain air currents were not blowing, the potential temperature along the mountain slope tended to rise with altitude, in both the Sea of Japan side and Pacific Ocean side. However, in the case in which cross-mountain air currents were blowing, the potential temperature distribution was nearly uniform on the slope of the leeward, Pacific Ocean side, regardless of elevation. The case in which cross-mountain air currents were blowing had characteristics similar to foehn. This also suggests an impact by gap winds that pass through the Uonogawa-Tonegawa channel. |
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言語 | en | |||||||||||||||||
書誌情報 |
en : The Rissho International Journal of Academic Research in Culture and Society 巻 2, p. 293-312, 発行日 2019-03-20 |
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出版タイプ | VoR | |||||||||||||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||||||||
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言語 | en | |||||||||||||||||
出版者 | Rissho University |