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Halley Research Station Team

Halley was founded in 1956, for the International Geophysical Year of 1957-58, by an expedition from the Royal Society. The bay where the expedition decided to set up their base was named Halley Bay, after the astronomer Edmond Halley. The name was changed to Halley in 1977 as the original bay had disappeared due to changes in the ice shelf.
During winter there are usually around 16 over wintering staff (winterers). In the summer period, from late December to early March, these staffs increase to around 70.

It is often not clear from articles about Antarctic bases that very few of the winterers are scientists. Most are the technical specialists required to keep the station and the scientific experiments running. The wintering team at Halley includes a chef, a doctor, mechanics, an electrician, several electronics engineers and a heating and ventilation engineer.

One of the winterers each year is designated as the Winter Base Commander and sworn in as a magistrate; this job is carried out in addition to their normal duties.

1996 saw the first female winterers at Halley, reflecting the changes within the British Antarctic Survey. There have been at least two women wintering every year since then.

The station operates throughout the year with a maximum population of 70 in the summer and an average of 16 over winter. The Emperor penguin colony near Halley, which is present from May to February, is a special attraction, while other recreational trips take members further inland towards the "hinge zone" where the floating ice shelf is joined to the continent.

Approximately 1.2 metres of snow accumulate each year on the Brunt Ice Shelf and buildings on the surface become covered and eventually crushed by snow, necessitating periodic rebuilding of the station. This part of the ice shelf is also moving westward by approx. 700m per year.

There have been five Halley bases built so far. The first four were all buried by snow accumulation and crushed until they were uninhabitable. Various construction methods were tried, from unprotected wooden huts to steel tunnels. Halley V has the main buildings built on steel platforms that are raised annually to keep them above the snow surface.

For more information on the Halley Research Station in Antarctica, please visit http://www.antarctica.ac.uk/living_and_working/research_stations/halley/index.php .

Deep Down into the Antarctic Ice

It’s early Sunday morning at Halley Research Station, Antarctica. The sun is rising quickly on the horizon, the wind is low and the temperature outside is a modest -18 degrees C. Conditions look perfect. As I look across the dining room at my friends and colleagues Niv and Colin I see two smiling faces nodding back at me. Today we are going to head out to the coast and attempt to explore a large crevasse at a point on the Ice shelf known as Creek Five.

Halley Research Station sits on the Brunt Ice Shelf 15km in from the edge of the shelf. It is the British Antarctic Surveys most southerly and remote research station. I am lucky enough to be a member of the eleven strong wintering team working as the chef on Station. With the impending arrival of 24 hour darkness we are all keen to make the most of the remaining daylight, taking every opportunity to make the most of our time in this amazing place.

Dancing Skies over Antarctica

During the winter months on the Antarctic continent not only do we experience 24 hour darkness but we are privileged to see the aurora australis.  Here at Halley Station we were looking forward to experiencing many a night gazing at the dancing lights as they flitter across the sky.   Reading the small print however, revealed that there is a cycle of activity that revolves around an 11 year period.  It seems that 2009 is a low solar activity year and hence our expectations might have been a bit high.

Large flares or solar explosions from the sun will expel numerous amounts of solar particles which make their way towards Earth.  These particles come into contact with the Earth’s magnetosphere and are directed towards the polar regions.  High energy particles then cascade into the highest parts of the Earth’s atmosphere, ionising gases.  It’s this process that emits the glows that we see on Earth.  The variation of colour is a result of particles with different energies ionising different gases.

Extreme Cold, Extreme South, Extreme Science

VP-FBB on the Antarctic Plateau

As I take off from the ice runway at the British Antarctic Survey’s Halley base, situated on the Brunt Ice Shelf (75o34’S 26o34’W), I finally realise I am living and working at the extreme of human endurance.  I am in one of the Survey’s De Havilland Twin Otters, known as Victor Papa Foxtrot Bravo Bravo (or VP-FBB), heading to the remote automatic weather station known affectionately as Baldrick, located at 83oSouth.
The weather station is hundreds of miles from the nearest living thing (human or otherwise) in the middle of the most inhospitable environment on the planet.  My life is entirely in the hands of the pilot Mark; fortunately they are very skilled hands.

Living in Antarctica: A Chance of a Lifetime

Editor’s Note: This article was written by Agnieszka Fryckowska, Meteorologist and Halley Winter Base Commander at Halley Station in Antarctica. This is the first of an ongoing series of posts written by the Halley Station team, which will give readers a window into life in Antarctica.

Introducing Halley Station (75°34’S 26°34’W), located on the 150m thick, continually moving, Brunt Ice Shelf in Antarctica.  Named after the Astronomer Edmond Halley, the current station (Halley V) is the fifth to be built.  It is the British Antarctic Survey’s most remote research station and has been operational since 1956 (established by the Royal Society for the International Geophysical Year, 1957-58).   Halley Station (also known as Base Z) has presented itself in many forms since those first buildings in 1956.

The extreme environment challenges even the most thought out buildings.  Blizzards and snow drifts eventually bury any structures left on the ground and the constant movement of the ice shelf compresses any structures under the surface, making these buildings eventually unsuitable for use.

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