Popupikkutoiminnot
Popupikkutoiminnot, which translates to "polar sunshine phenomena" in English, refer to the temporarily visible upper parts of the sun during polar nights. This occurs when the sun is below the horizon and its upper edge can be seen above the horizon due to the Earth's curvature.
During the polar night, the sun remains below the horizon for a certain period, but its upper
The upper parts of the sun visible during polar nights is often referred to as the Omega
Different cultures have interpreted this phenomenon in various ways. In some Northern societies, the appearance of
The appearance of the upper parts of the sun during polar nights can be an exciting and