Last Updated：2025/11/21
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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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。
