During the June solstice, the Arctic Circle experiences nearly 24 hours of daylight. Because the Earth's axial tilt points the Northern Hemisphere toward the sun, the sun remains above the horizon throughout the day. The duration of continuous daylight increases with latitude: locations on the Arctic Circle itself see one day of 24-hour sun, while areas farther north (e.g., Tromsø, Svalbard) enjoy weeks or even months of midnight sun.
Conversely, the Antarctic Circle endures nearly 24 hours of darkness during the June solstice. The Southern Hemisphere is tilted away from the sun, leaving the sun below the horizon. As in the Arctic, the length of continuous night grows with latitude. Research stations on the Antarctic coast may see a few hours of twilight, while the South Pole experiences six months of darkness centered on the June solstice.
The opposing conditions are a direct result of the Earth's 23.5° axial tilt. During the June solstice, the North Pole leans toward the sun, bathing the Arctic in constant light, while the South Pole leans away, plunging the Antarctic into constant night. The situation reverses at the December solstice.