The Poles: Extreme Weather
The snow and ice covering Antarctica reflects most of the sunís light and makes it the coldest place on Earth.
Horizontally blowing snow streaks across the front door of a quanset hut used by NOAA in 1950. Photo courtesy of the NOAA Corps Library.
Why is Antarctica colder than the Arctic?
The main reason why Antarctica is colder than the Arctic is that Antarctica is a continent surrounded by an ocean while the Arctic is an ocean almost completely surrounded by continents and Greenland. The Arctic's ice is relatively thin compared with Antarctica and it has water, not land, under it. While the water is not warm, it usually stays around 30° F, which is often significantly warmer than the air above the ice. Some of this heat makes its way through the ice to the air moderating temperatures somewhat. By contrast, Antarctic has a higher average elevation that any other continent on Earth, and it is covered by a few thousand feet of ice. All the snow and ice covering the continent reflects most of the sun’s light and makes Antarctica the coldest place on Earth.
The coldest time of the year is usually September, and mean winter temperatures are -40 to -70°C (-40 to -94°F). During winter, the size of Antarctica doubles as the surrounding seawater freezes. In the summer, mean temperatures range between -5 to -31°C (-15 to -35°C). There is very little precipitation—less than 10 cm (4 in) in a year – and the continent is as dry as a desert. Strong winds lead to low effective temperatures (see classroom activity below).
The Greenland ice sheet and the Arctic Ocean maintain cold temperatures throughout the year, but the tundra-covered coastal areas warm up each summer for a brief period. The coldest time of the year is usually March but, because salt water freezes at -1.8°C (29°F), the ocean temperature never gets below that. However, the continental parts of the Arctic can get very cold—the coldest average temperature is -68°C (-90°F). The Arctic also has low precipitation, with an average of less than 51 cm (20 in) each year.
Classroom Activity from "Classroom Antarctica." Click here for a pdf version to work with yourself!
To estimate effective temperature, draw a line from the appropriate point on the top scale (air temperature) to the appropriate point on the wind-speed scale at the bottom. The effective temperature is the point at which the line crosses the middle scale. In the example, a wind speed of 30 km/h (bottom scale) lowers a temperature of minus 20°C (top scale) to an effective temperature of 31°C (middle scale).
More Reading: Weather Links
Site showing annual changes in the ice cover over Antarctic seas
A 2000 NASA (National Aeronautics and Space Administration) educational site on Antarctic seasons
Weather in Antarctica during the year
Real-time weather data collection
Weather and season descriptions from the Antarctic Connection site