
Период когда солнце не опускается за горизонт называются


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The period when the sun does not set below the horizon is called "the midnight sun".
The phenomenon of the midnight sun occurs in regions near the Earth's poles during the summer months. It is characterized by the sun remaining visible for 24 hours a day, resulting in continuous daylight. This phenomenon is caused by the tilt of the Earth's axis, which causes the sun to stay above the horizon for an extended period of time in polar regions during the summer solstice.
The specific duration of the midnight sun varies depending on the latitude and the time of year. In the Arctic Circle, for example, the midnight sun can be observed for several weeks around the summer solstice, which usually falls on June 21st. In the Antarctic Circle, the same phenomenon occurs during the winter solstice, which usually falls on December 21st.
The midnight sun has significant cultural and ecological implications for regions experiencing this phenomenon. It affects the behavior of wildlife, the daily routines of people, and various cultural traditions.


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