A numerical investigation on the formation of the stalling of the...
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https://data.zh-cn.virginia.gov/dataset/a-numerical-investigation-on-the-formation-of-the-stalling-of-the-cross-polar-jet-in-midnight-t
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Thermospheric winds usually flow from noon to the midnight inside the polar cap and spill further equatorward around midnight, due to the combined effects of solar radiation-...
热层风（Thermospheric winds）通常在极盖区域内从正午向午夜流动，并在午夜前后进一步向赤道方向扩散，这源于太阳辐射的联合效应……
