Antarctica Weather and Climate

Weather - what is happening in a particular place at a particular time, usually over short periods, hours or days, e.g, rain, blizzard, sunny and calm.

Climate -  the average atmospheric conditions over long time periods, weeks, months, years.

or... Climate = what you expect,    Weather = what you get.

  What is the climate like in Antarctica?

Antarctica is a continent, bigger than Europe, North America or Australia, and so doesn't just have one climate zone, but several. As it is centered on the South Pole, the climates are all cold, but there are still distinct zones:


Continental High Plateau:

  • Around the centre of the continent, high altitude with an average height of around 3,000m (10,000ft)
  • Extreme cold year-round, approx. -20°C to -60°C monthly averages, large temperature range
  • Clear skies common, constant light winds from the South
  • Snowfall is rare, precipitation in the form of fine ice crystals, no more than a few centimeters a year

e.g. Vostok, 78°27'S, 106°52'E, average temperature -55.1°C, range 36°C
Near the South Geomagnetic Pole and Southern Pole of Accessibility, deep in the Eastern Antarctic Ice sheet.

Continental Low Plateau:

  • Lower altitude West Antarctica and closer to the coast in East Antarctica, approx. 1000-1,500m (3500-5000ft)Continental low latitude
  • Very cold year-round, approx. -12°C to -35°C monthly averages, smaller temperature range than higher altitude
  • Clear skies, calm air, little precipitation common
  • Weather more variable as depressions can bring blizzards with heavy snowfall and strong winds

e.g. Byrd, 80°01'S, 120°00'W, average temperature -27.9°C, range 22.3°C
Inland on the West Antarctic Ice Sheet, approx. 660km (410 miles) from the nearest coast.

Continental High Latitude Coast:

  • Coastal areas in the deep south 70°S +
  • Cold winters and short cold summers, approx. -2°C to -30°C monthly averages
  • Frequently changing weather, cloud and year-round snow is common
  • Coasts often have fast-ice through the year which keeps temperatures low

e.g. McMurdo, 77°50'S, 166°30'E, average temperature -16.9°C, range 23.8°C
On Ross Island in the Ross Sea very close to the continent in a deep southerly indentation.

Continental Low Latitude Coast:

  • Coastal areas approx. 65°S - 70°S
  • Cold winters and short cold summers, approx. +2°C to -20°C monthly averages
  • Temperatures are higher than many non-Antarctic continental areas even in winter, summer temperatures kept low due to ice and snow cover
  • Precipitation can be heavy, winds often very strong - katabatic

e.g. Mawson, 67°36'S, 62°55E, average temperature -11.9°C, range 18.9°C
On an isolated rocky outcrop on the coast in MacRobertson Land, west of Australia.

Antarctic Peninsula:

  • Fairly typical maritime climate, cold winter and warmer summers.
  • The western side of the Peninsula is warmer than the eastern side.
  • Cold winters and short cold summers, approx. +1°C to -15°C monthly averages
  • Depressions come in from the west bringing cloud precipitation and winds, rain frequently falls in summer

e.g. Rothera, 67°34'S, 68°08'W, average temperature -5.3°C, range 13.6°C
Due South of South America, separated by the Drake's Passage.

Antarctic Islands:

  • Maritime climate similar to the Antarctic Peninsula but milder
  • Cold winters and short cold summers, approx. +1°C to -10°C monthly averages
  • Winter temperatures brought down by sea-ice Low cloud common in summer with rain and sleet, heavy snow in winter

e.g. Orcadas, 60°44'S, 44°44'W, average temperature -4.3°C, range 11°C
Islands at all points around the Antarctic Continent, more concentrated in the region of the Antarctic Peninsula.

Sub-Antarctic Islands:

  • Southern ocean islands above the northern limit of sea-ice
  • Oceanic climate with cool summers and similar but cooler winters, approx. +4°C to -1.5°C monthly averages
  • Depressions bring rain in summer, snow in winter and strong winds year-round

e.g. South Georgia, 54°18'S, 36°30'W, average temperature 1.8°C, range 6.9°C
A relatively small number of oceanic islands distributed around the Antarctic Continent.

The temperature through the year at increasingly
southerly regions in Antarctica

Antarctic temperatures


e.g. Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Average Range
Continental High
Vostok -32.1 -44.3 -57.9 -64.7 -65.6 -65.2 -66.9 -67.6 -66.0 -57.1 -43.3 -32.1 -55.1 36.0
Continental Low
Byrd -14.7 -19.8 -27.7 -29.7 -33.0 -34.1 -35.6 -36.7 -36.6 -30.2 -21.4 .14.4 -27.9 22.3
Continental High
Latitude Coast
McMurdo -2.9 -9.5 -18.2 -20.7 -21.7 -23.0 -25.7 -26.1 -24.6 -18.9 -9.7 -3.4 -16.9 23.8
Continental Low
Latitude Coast`
Mawson -0.7 -5.4 -11.2 -15.0 -16.8 -16.7 -18.0 -18.8 -18.2 -13.9 -6.2 -0.9 -11.9 18.9
Antarctic Peninsula Rothera 1.0 0.1 -1.6 -3.7 -6.8 -8.8 -12.6 -11.8 -9.4 -7.2 -3.3 0.2 -5.3 13.6
Antarctic Islands Orcadas 0.3 0.5 -0.6 -3.0 -6.7 -9.8 -10.5 -9.8 -6.4 -3.4 -2.1 -0.5 -4.3 11.0
Sub-Antarctic Islands South
4.7 5.4 4.6 2.5 0.2 -1.5 -1.5 -1.5 0.1 1.7 3.0 3.8 1.8 6.9

  What sorts of weather does Antarctica experience?


  • Antarctica is the windiest continent on earth, the relative intensity as you get further south is told by the old sailors descriptions of what it's like at different degrees of latitude:

    • Roaring Forties, Furious Fifties and Screaming Sixties

  • Storms are common in Antarctica and are frequently very energetic and dramatic.

  • Between 50°S and 60°S the Westerly winds are driven by the pole/equator temperature gradient.

  • Below 60°S winds are largely katabatic, this is a result of cold air forming over the high polar plateau at around 3,000m (10,000ft) and falling (as cold air is heavier) down the slope to the coast . The cold air falls gets faster as it goes and by the time it reaches the coast, the earth's rotation (Coriolis force) makes the wind westerly.


  • Estimations of cloud cover has been problematic in Antarctica as the whole landscape is difficult to estimate and features that may seem a few km distant can actually be 50km or more, this makes cloud height estimations particularly difficult.

  • Cloud cover averages may be 6/8 or 4/8, but the reality is that often cloud is either 0/8 or 8/8 i.e. no cloud or total cloud.

  • Coastal areas are cloudier than continental areas and continental clouds are often made up entirely of ice crystals rather than the mix of ice and water vapour at the coast.


  • Most precipitation falls as snow in Antarctica. Constant strong winds make measurement of snow fall very difficult as once it's fallen it then blows around an awful lot without any extra being added to any one position. It rarely comes down vertically making it hard to catch and measure it.

  • Precipitation is often measured as "water equivalent" the amount of water that would be obtained if the snow was melted.

  • The high plateau of East Antarctica is a desert with less than 50mm of water equivalent falling per year, this does not fall as snow but as tiny ice crystals in the air known as "diamond dust" from a perfectly clear sky and causes many optical phenomena such as solar pillars and haloes.

  • The heaviest snow falls are on the western coast of the Antarctic Peninsula.

  • Rain commonly falls in coastal regions in the summer.


  • A combination of high winds and blowing snow, the snow may or may not be falling from the sky.

  • When snow falls in low temperatures, or when ice crystals in the air settle, they are only very loosely bound together and so may be blown around for a long time, the result is that there is often blowing snow in Antarctica without there being very much precipitation.

  • A blizzard may easily lead to white-out conditions when it is impossible to see surface features, the whole world is just a big white blur, this can be very dangerous as it is possible to walk over a cliff edge without even being aware it is there.

  Does Antarctica influence the climate and weather elsewhere?

The contribution to the weather outside of Antarctica is actually very small, Antarctic weather keeps itself to itself most of the time, there is a much greater influence from ocean currents than from atmospheric effects. This contributes to Antarctica being so cold, as the weather goes round and round the continent rather than spilling over to lower latitudes as the arctic weather systems do at the other end of the planet.

A greater influence is from the Thermohaline circulation. Thermo - heat, haline - salt/salinity. Very salty water is denser than less salty water and will sink beneath it, colder water likewise is denser than warmer water and sinks beneath it. Around Antarctica very low air temperatures cause surface waters to cool, become denser and sink beneath the rest of the ocean, this falls to the bottom of the sea and then starts to flow northwards (a similar thing happens in the Arctic flowing south). It is important as means that there are deep currents moving sea water around the oceans that are independent of winds. This moves huge amounts of heat around the planet largely independent of surface weather (although surface weather initiates it) these currents can take 100's of years to reach their destination.

  What is the circumpolar vortex?

The "circumpolar vortex" is a strong Westerly circulation of winds that builds up during the winter months in the upper layers of the atmosphere (stratosphere) over Antarctica.

Cold temperature nacreous clouds are lit up by the sunrise at McMurdo, Antarctica Nacreous clouds lit up by the sunrise at McMurdo, Antarctica

They cut off the central Antarctic weather from the rest of the world causing temperatures to fall and stay low. It also adds to the breakdown of the ozone layer by trapping clouds called "Polar Stratospheric Clouds" that cause ozone depletion by (also trapped) Chlorine containing compounds (such as chlorofluorocarbons - CFC's). These clouds may be called "Nacreous" as they look like the nacre of shells or mother-of-pearl. The circumpolar vortex breaks up in the spring and summer months, it maintains very low and stable temperatures in the winter.

  Infrared cooling

A way of saying that hot things cool down! At night the warm earth gives out infrared rays that cool it down, it also happens during the day, but we don't notice it amongst the warmth from the sun, it only really causes a temperature drop at night. It's this that balances the heat coming in from the sun, so the planet doesn't just keep getting hotter and hotter.

Thermal image of emperor penguin group
Thermal images of emperor penguins, separate and in a huddle.

Clouds and water vapor in the air reduce infrared cooling by trapping the rays in the atmosphere. Dry air and a lack of clouds allow the rays to escape, which is why deserts can get very cold at night while they are very hot during the day.

  Specific heat

Water and ice around coasts influence local temperatures

Specific heat is a measure of the energy needed to raise a standard amount of a substance by 1°C, usually given in Joules, could be calories.

e.g. the specific heat of water is 4.2 J/g °C - it takes 4.2J to raise 1g of water by 1°C.

The specific heat of ice is 2.1J, air 1J, iron 0.45J. The higher the number the greater the amount of energy the substance can store and the slower it will cool down.

Water has a high specific heat capacity, this means that it has a large influence on local weather, cooling or warming the surrounding land and keeping temperatures more even and constant. If you look at the climate zones map at the top of this page, you will see that coastal areas generally have smaller temperature ranges over the year than inland areas. This is partly due to the high specific heat capacity of the surrounding or nearby water.

  How does pack-ice affect the climate?

Pack ice is floating ice that is frozen sea-water, it may have formed in situ, or may have floated from many hundreds or thousands of miles away.It can be open-pack or closed-pack, depending on how pushed together the pieces are. It can last a year or less, or may be old ice that has survived 2 or 3 years before being broken up and drifting off. It forms each year from the sea and melts back into the sea so it does not contribute to sea-level changes, but has a major impact in reflecting light and heat from the sun.

More pack ice makes local conditions colder, less makes it warmer.

Picture credits, copyright pictures used by permission: Climates zones map - Modified from original provided by Tentotwo under Creative Commons 3.o Share and Share Alike Unported license