Because Antarctica centers on the South Pole, it experiences the most dramatic seasonal daylight variations on Earth. The solstices in June and December mark the extremes of this cycle.
On the June solstice, the Sun barely grazes the horizon at the South Pole, marking the start of the polar day (midnight sun). Due to atmospheric refraction, the Sun appears above the horizon for several days before and after the solstice, resulting in continuous daylight for up to a week or more depending on latitude. The further north you travel from the pole, the shorter this period becomes.
Conversely, the December solstice brings the polar night. The Sun remains below the horizon for a full 24 hours at the pole, and atmospheric refraction extends this darkness for several additional days. Again, the effect diminishes with lower latitudes.
Coastal research stations experience less extreme versions: they may see a few hours of twilight on the June solstice and a few hours of daylight on the December solstice. The exact duration of continuous light or darkness varies significantly across the continent.