…The climate of the Alps is characterized by temperature inversions, especially in winter, when temperatures are higher on the mountain tops and significantly lower in the valleys and basins where cold air flows in. As a result, the annual temperature range at the summits is much smaller than that in the valleys, and is 14.4 °C at Sonnblick (3105 m) in the Hohe Tauern, compared to 21 °C in Vienna. The föhn is also a phenomenon that characterizes the climate of the Alps, and is particularly noticeable in the Rhine and Inn valleys. … *Some of the terminology that mentions "Sonnblick" is listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…アルプスの気候で特徴的なのは気温の逆転現象であり,特に冬の気温は,山の上で高く,冷気の流入する谷や盆地では著しく低温である。このため,山頂部の気温年較差は谷のそれに比べてはるかに小さく,ホーエ・タウエルン山脈のゾンブリックSonnblick山(3105m)では14.4℃であり,たとえばウィーンの21℃と比べても明らかである。フェーンもアルプスの気候を特徴づける現象で,とくにライン川の谷とイン谷で著しい。… ※「Sonnblick」について言及している用語解説の一部を掲載しています。 出典|株式会社平凡社世界大百科事典 第2版について | 情報 |
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