Last Updated：2025/11/21
Sentence
気象学者はしばしば大規模な地衡風をモデル化して上空の大気循環を推定します。地衡風は水平方向の気圧勾配力とコリオリ力との釣り合いによって向きと速度が決まる風です。
Quizzes for review
Meteorologists often model the large-scale geostrophic wind to estimate upper-atmosphere circulation because its direction and speed result from a balance between the horizontal pressure-gradient force and the Coriolis force.
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Meteorologists often model the large-scale geostrophic wind to estimate upper-atmosphere circulation because its direction and speed result from a balance between the horizontal pressure-gradient force and the Coriolis force.
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Related words
geostrophic wind
Noun
Japanese Meaning
地衡風：水平な気圧勾配力と地球の自転による力（北半球では左、南半球では右）との釣り合いにより、その方向と速度が決定される風のこと。
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