See how low sunlight, ice, wind, and darkness shape polar weather.
Polar weather is driven by low solar angles, long winter darkness, reflective snow and ice, cold air, strong winds, and interactions with surrounding oceans. Conditions can change rapidly and remain dangerous even in summer.




Antarctica holds the lowest directly measured surface air temperatures on Earth.
Learn MoreDense cold air can race downhill from high ice sheets.
Learn MoreBlizzards combine strong wind with snow or blowing snow.
Learn MoreCold dense air often settles near the surface.
Learn MoreWinter darkness allows the surface to lose heat for long periods.
Learn MoreSummer brings continuous or nearly continuous daylight.
Learn MoreWeather stations, satellites, balloons, ships, aircraft, and automatic sensors observe polar weather.
Learn MoreCold injuries and whiteout conditions can become life threatening.
Learn MoreInterior elevations are especially cold because the air is thin, dry, and far from ocean moderation.
These katabatic winds can become extremely strong along parts of Antarctica.
Visibility can collapse even when little new snow is falling.
This can create temperature profiles opposite to the usual pattern.
At the poles, the Sun remains below the horizon for months.
Despite long days, the Sun remains low in the sky and surfaces reflect much of its energy.
Remote conditions make observations difficult and expensive.
Polar field teams use specialized clothing, shelters, navigation, communication, and strict travel planning.