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Wednesday, 09 January 2008 00:58
Japanese-Swedish Antarctic Expedition: Report no 16
Written by Sweden/Japan Traverse
Expedition Diary January 7, 2008
3500 meters above sea level
Maximum & Minimum temperatures: - 24 to - 35 °C
Never a uniform white blanket on the ice sheet, the character of the surface snow takes on many different forms. On the microscale, different crystal forms tell stories of their arrival to the surface as gently falling snow, wind-battered hard pack, or deposition as surface hoar through condensation events.
To a traverse train of vehicles, generous amounts of gently-fallen snow represent “snow swamps” in which the treads sink and dig their way in, sometimes preventing a vehic...
Expedition Diary January 7, 2008
3500 meters above sea level
Maximum & Minimum temperatures: - 24 to - 35 °C
Never a uniform white blanket on the ice sheet, the character of the surface snow takes on many different forms. On the microscale, different crystal forms tell stories of their arrival to the surface as gently falling snow, wind-battered hard pack, or deposition as surface hoar through condensation events.
To a traverse train of vehicles, generous amounts of gently-fallen snow represent “snow swamps” in which the treads sink and dig their way in, sometimes preventing a vehic...
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January 7th 2008
I am halfway through my sojourn at sea and loving the perpetual motion of the ship. We are moving through an endless ocean in apparently endless circles. Not having a 'destination' is quite a nice thing. There is nothing on the horizon for 360 degrees. There's no ice to be seen, not even a growler. We are nearly 200nm north of Cape Denison on the Antarctic continent, adrift on a lonely sea.
In fact we do have a purpose. This is the CASO (Climate of the Antarctic and Southern Ocean) sampling area. We must cover 31 stations in six days making CTD drops of around 3,600 metres to sample the cold, dense, Antarctic bottom water that drains from the Mertz Glacier. We are working over the skid marks on Rob's Gondwana map that show the seabed cany...
Sunday January 6th 2008
A clatter of footsteps in the stairwell is a sure signal to grab the camera and follow the mob. I raced up to C deck and saw a distant spouting. The CTD door was open to the sea so I ran back down to E deck. The CASO crew was riveted, watching a pair of humpbacks curving and spouting. They moved aft and we all jumped like fleas across the trawl deck to watch them coast and roll and play in a large drift close to the ship. I scurried up to the mezzanine, craning over the ship’s rail on the way, keeping them in sight, then made a dash up the stairwell and back onto C deck.
Rail spac...
Tuesday, 8 January
My alarm clock rings at seven, like almost every morning, and before I get up I try to guess whether we are standing or travelling, as I do almost every morning. Did the krill people finish the calibration of the echosounder? Yesterday afternoon it still seemed like a very big task... But no, a glimpse out of the window tells me that we are quietly sailing through the polynya which surrounds the ship as calm as a little mill pond. The shelf ice edge is shimmering magically in the distance even under the overcast sky.
During the morning preparations start to accommodate the 33...
Written 6 January, 2008
3608 meters a.s.l.
Maximum & Minimum temperatures: -29 to -35 °C
Nearly all the way from Troll Station to the Pole of Inaccessibility we have driven along the crest of the continent. On this last leg towards the South Pole we have left the ridge and will gradually be descending to lower ground. This implies different patterns of winds and snow accumulation. We are starting to see the effects of this in the shape of rougher snow drifts and more sastrugi, so the ride is getting bumpier. However, there are positive side effects to this. One is that it is much easier for the drivers to...
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Monday, 7 January
Finally the conditions are perfect for a game of Boccia! There is only a soft breeze, and we are in open water surrounded by a broad band of sea ice which keeps the swell from the open ocean from hitting us. The Polarstern is fairly stable in the water, so we started our boccia game at 6 a.m.
We play with four copper balls, the smallest of which is about as big as a hazelnut, and the largest the size of a tomato. Now in our game the goal is not to bring the balls together as closely as possible, but rather to get them into a target area under the ship. This area, 15 m under th...
Which way did the camera go first: north or south? The Antarctic edged out her northern counterpart by only a handful of years. James Clark Ross' narrative of his 1839-43 expedition does not reveal any photographic outfit in its inventory, but one of his medical men later noted just such an apparatus for posterity. Dr. Joseph D. Hooker was lecturing about the historic expedition at the Royal Institution of South Wales in 1846 when he offered these words:
I believe no instruments, however newly invented, was omitted, even down to an apparatus for daguerreotyping and talbotyping, and we left England provided with a register for every known phenomenon of nature, though certainly not qualified to cope with them all.
The responsibility for any photographic ...
Saturday January 5th 2008
Collecting the pole compass early today marked the completion of what we are calling the 'eastern' CEAMARC sampling stations. The central and northern reach of our grid marks out the 'Climate of Antarctica and Southern Ocean' (CASO) stations which we will work through over the coming week before another CEAMARC burst to the west off Dumont d'Urville on the continent.
As well as CTD sampling, the CASO team is gathering information on the speed and direction of water currents from polynya moorings. These Acoustic Doppler Current Profilers are deployed some 135 miles from the South Magnetic Pole but still fall within its influence, so a special "pole compass" is used as a kind of calibrator to correct their data.
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