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Antarctica occupies a privileged position from which to observe and measure all parts of our atmosphere. Knowledge of how it works is becoming increasingly important to how we live our lives today, both in weather forecasting and in communications via satellites.

Sun Pillar and Halo, from a remote field camp on Pine Island Glacier, West Antarctica.
Sun Pillar and Halo

The British Antarctic Survey has a dedicated team of engineers and meteorologists who live all year round at Halley and Rothera research stations in the Antarctic to look after experiments designed and used by a research team of over 60 scientists and engineers at BAS in Cambridge.

Some of our Antarctic experiments remotely sense the atmosphere from the ground using spectrometers, lasers, radars, cameras, interferometers, radio receivers and magnetometers, whereas others are carried by balloons or rockets to make measurements in-situ. In this way we are able to probe every layer of the atmosphere from the ground right up into Space.

The Troposphere:

The lowest part of the atmosphere, from the ground to about 12 km altitude. This is where the weather takes place, where there is moisture and where there are living things.

The Stratosphere:

12–50 km above the earth, above the clouds and at the cruising altitude of airliners, lies the stratosphere. It contains the ozone layer that protects us all from harmful ultraviolet (UV) radiation from the Sun.

The Ozone Hole:

BAS scientists first alerted the world to a deepening ozone hole over Antarctica, with consequent increases in levels of UV radiation and hence greater risk of skin cancers.

The Mesosphere:

Between 50 and 80 km altitude lies the mesosphere, which was once dubbed the ignorosphere because of the difficulties in exploring it! Now, modern lasers, radars and sub-orbital rockets are being used to discover more of its secrets, including the highest clouds and the lowest temperatures anywhere on Earth.

Aurora over Halley 5 ACB.  Aurora are caused by the precipitation of charged particles from space towards the magnetic poles driven by plasma winds and magnetic storms.
Aurora over Halley

The Ionosphere:

80 to 1000 km above the earth lies the ionosphere, at the frontier to Space and at the orbital altitude of the space shuttle, International Space Station, and polar orbiting satellites used for mobile phone communications and remote sensing of the earth. The polar ionosphere forms nature’s TV screen for a nightly showing of the aurora — a dancing display of rays, curtains and spirals of red, green and white light. The aurora is caused by the precipitation of charged particles from space towards the magnetic poles that is driven by plasma winds and magnetic storms, known collectively as space weather.