行星的光面(白昼侧)与太阳风有着最直接的接触。
The dayside has the most direct contact with the solar wind.
在磁场方向为北的情况下，电离层白昼侧的极地地区也有很强的能量传递。
There are times when the field is northward and there are strong flows in the dayside polar ionosphere.
这意味著在第二天的阳光下，地球上白昼的那一侧只有加热，没有冷却；同样，夜晚的那一侧只有冷却，没有加热。
This means that the day side of the Earth warms up without cooling, and likewise the night side cools down without warning up under sunlight the next day.
在白昼一侧的增加更大，表明环电流具有不对称性的特征。
This enhancement is larger at the daytime than at the nighttime. Showing that the intensifying ring current is asymmetrical.
在白昼一侧的增加更大，表明环电流具有不对称性的特征。
This enhancement is larger at the daytime than at the nighttime. Showing that the intensifying ring current is asymmetrical.
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