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Antarctic weather right now!


Amundsen Scott station (USA)
at the South Pole


Vostok station (Russia)
at the Southern Geomagnetic Pole.
Close to the Pole of Inaccessibility.

1/ Solar pillar
The air in Antarctica is frequently very dry. The low temperatures mean that little or no water vapour is held in the air, instead it freezes and falls out, or builds up on surfaces as frost. Sometimes however depending on the particular atmospheric conditions, the frozen water vapour remains in the air as suspended ice crystals. In these conditions the crystals can reflect sunlight in a variety of ways forming atmospheric phenomena of different types.  

One of these phenomena is the "Solar Pillar" seen above. The sun is reflected very strongly so that the reflection is almost as bright as the sun itself. Like a rainbow, this sight is dependent on where the light is coming from and where the observer is standing. The pillar appears to move when the observer moves, but always remains directly below the sun.

2/ +100°C water meets -32°C air
A fun thing to do in extreme cold is to throw hot water into the air. Take a flask and fill it with boiling water to warm it up, pour this away and fill it again. Take the full flask outside, take a cup of this hot water and throw it all up into the air.  

As the +100°C water meets the cold (in this case -32°C) air, it instantly vaporizes. Most of it is turned into a cloud of steam that drifts gently away and some of the droplets that stay together are instantly turned into small pieces of ice that can be seen streaking down towards the bottom left in this photograph.

It's very weird to throw water into the air but none of it ever actually landing. Also seen in this picture is a solar halo around the sun formed by the ice crystals in the air.

 

3/ Heavy seas across Drakes Passage
The Drake Passage is the stretch of water between the most southerly tip of South America and the most northerly tip of the Antarctic peninsula.   

It is the place where not only are there high and strong winds that blow most of the time, but where the "Circumpolar Current" is squeezed through its narrowest gap. This is a Westerly flowing current that flows around Antarctica powered by Antarctic winds. It flows at the rate of around 140 million cubic metres (tonnes) of water per second, the equivalent of 5000 Amazon rivers or four times the size of the Gulf Stream.

The Drakes passage has been described as the roughest stretch of water in the world, it is what must be navigated when rounding Cape Horn and Tierra del Fuego - the southern most tip of South America. To reach the Antarctic peninsula it is necessary to traverse this stretch of water at right angles to the current flow. The result is often very lumpy seas indeed as seen in this shot where HMS Endurance is making the crossing.

 

4/ Ice mirage
Mirages are commonly seen on the horizon in the winter or as in this case at the end of winter when the sea-ice has just broken up. They are a result of temperature differences in the bottom few metres just above the ice or sea surface.  

Air of different temperatures refracts light in different ways, the same phenomena is responsible for "heat haze" as seen above a road on a very hot day.  

It is the difference in temperature that is important and in this case it is causing a reflection downwards just above the level of the horizon so that objects on the horizon appear to be floating above the sea or ice rather than resting on it.

 

 

5/  Clouds and skies

I once met someone (admittedly a meteorologist) who said that his main reason for going to the Antarctic was because of the amazing skies and clouds that he had seen in pictures. 

Who can blame him? (if not necessarily agree). The clear (almost) pollution free air and wide open vistas unencumbered by trees, buildings or other clutter give panoramas of the sky that stretch for dizzying distances.

 

6/ Solar halo
Another of the many optical atmospheric phenomena frequently seen in the Antarctic as a result of the scattering of light by ice particles suspended in the air.   

Such phenomena are usually encountered in the winter rather than summer when lower temperatures make such occurrences more likely.

 

 

 

7/ -2°C water meets -32°C air
Another take on the idea that water turns to vapour when it is considerably warmer than its surroundings.   

In this picture, water is being exposed at the "tide-cracks" that form around offshore rocks and small islands when the tide rises and falls with continuous sea-ice present. As the ice is not flexible it cracks and as it does, exposes an amount of open water to the air.  

Antarctic sea water varies between about +2°C and -2°C (approx. the freezing point of sea water) over the course of a year, so in the case of this picture, the exposed sea water is more than 30°C warmer than the surrounding air. The result - it begins to turn to a vapour being so much warmer. The sunshine on this day serves to make it more visible and different temperature layers in the air cause it to rise to a band above the clearer air close to the ice surface.

 

8/ Föhn bank
A Föhn bank is formed by a Föhn wind. This is a warm contour-hugging wind that is blowing across Coronation Island in the South Orkneys group in this case.  

As the warm (relatively to the ice and rock) wind blows across the land, it causes snow and ice to sublime. That is to turn directly from a solid to a gas without passing through a liquid phase, so causing the cloud layer that can be seen. The overall effect as seen from a distance is that the land is covered by a very large duvet. The gross contours can be seen through the cloud layer, but all of the finer detail is obscured.


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