Last Updated:2025/11/28

Above the mid-latitudes, the wind flows geostrophically around the pressure system, balancing Coriolis and pressure gradient forces.

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Above the mid-latitudes, the wind flows geostrophically around the pressure system, balancing Coriolis and pressure gradient forces.

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中緯度では、風は地衡の観点から気圧系の周りを流れ、コリオリ力と気圧傾度力が釣り合っています。

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