…However, if we know the flow and temperature fields as shown in Figure 2, we can use the theory of meteorological dynamics to calculate the vertical flow. According to this, in the middle layers of the atmosphere, there is an upward movement between the trough line of the atmospheric pressure and the ridge line downwind of it, that is, where the warm air flows in. Therefore, air gathers from the surroundings in the lower layers and flows out to the surroundings in the upper layers. … *Some of the terminology that refers to "low pressure trough" is listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…しかし,図2のように流れの場と温度場を知ると,気象力学の理論を使って鉛直流が計算できる。それによると大気の中層では,気圧の谷線とその風下の尾根線の間,つまり暖気の流入するところに上昇運動がある。したがって下層で周囲から空気が集まり,上層で周囲へ流れ出す。… ※「気圧の谷線」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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