I am a Marine Biologist working with the British Antarctic Survey based at Rothera Research Station. This is mostly a blog about, of course, Antarctica but also station life, the people that keep it running and the research that we conduct.

Pancake Ice and Winter



Our training on the James Clark Ross (click to view a previous blogpost) introduced us to stoves and Tilley lamps which, at the time, seemed hard to imagine the use for while sailing through the tropics. However, when moving around Antarctica, the utility of devices to keep warm is certainly more relevant and much welcomed. On weekends and bank holidays, it is common for people to skin up to the caboose - a small red refuge hut (a reconverted shipping container) -  ski or snowboard in some fresh snow and warm up with a cuppa. Interestingly, melting a whole pot of snow yields only a minute amount of water, when expressed as a volume, the snow to ice ratio is 10 parts snow to 1 part water. Bearing in mind this is fresh snow and ice is denser and cutting ice blocks yields a greater volume than the equivalent volume of snow.





The caboose - at the bottom of 'Vals', a gentle ski slope


Snowboarding on Vals


An excellent place for a cuppa!


Primus stoves and Tilley lamps inside the Caboose

As the chilly winter kicks in, it's a great relief to go inside the refuge hut, and make us of the intended purpose of the caboose: re-warming with some melted snow and chocolate powder. On extra cold days, lighting the Tilley lamp generates enough heat to get the circulation going in your fingers again!


Klara (station doctor) in the caboose. 
Even inside the refuge it's cold, down jacket needed!

With increased snowfall, previously rocky areas have now become skiable routes. Nordic skiing is a new sport I've taken up and what a delight it is to have light skis on your feet compared to clunky traditional down-hill skiing boots. These thin skis, as exhibited by Jas in the photos below, are fitted with a small scaly artificial skin to help with grip but also allowing you to move with speed. Unlike downhill skiing, you don't need to remove the 'skins' when transitioning terrain. Nordic skiing is generally made for flat terrain and your feet are clipped in at all times. When you get really good at it, it's possible to move fluidly by sliding with your feet in a triangular formation. 



Jas Nordic skiing around the point


Nordic skiing with Rothera station in the background

We observed our first pancake ice on the 19th March. Pancake ice is a term used to describe circular formations of sea ice with rimmed edges as a result of colliding with other ice. It is commonly formed amongst frazil ice and grease ice (a thin layer of greasy looking ice). When the floating ice rinds of grease break up, pancake ice pieces form as a result. 

 Until now, we had observed only berg fragments and porridge ice (essentially a slushy layer of mostly unconsolidated ice) but this marks an exciting transition into the stages of sea ice formation. We have subsequently witnessed the process of 'rafting' where pancake ice pieces have joined together or pushed on top of each other forming solid young ice sheets,



The process of sea ice formation



Pancake ice formation around Anchorage Island, Ryder Bay

Back in the diving world, the sea has reached freezing point, with our most recent lowest water temperature record (3rd May) at -1.7°C. After about 20 minutes in the water, you can really start to feel that winter chill and you certainly don't want to remain stationary for too long! At the same time, there is something quite magical about getting kitted up in the snow before a dive...


 Kitting up in the snow with Ryan- Photo credit: Pete Hill


It's easy to keep track of the divers when the surface has frozen, Photo credit: Pete Hill

 
Ryan and I preparing to dive below the freezing water surface, Photo credit: Pete Hill
 

Post-dive thinking 'where's the tea?', Photo credit: Ryan Mathews

We don't always dive from the boats and as the sea ice starts to form, this will certainly be out of the question as the small RIBS are not equipped to break through ice. Whilst the water is free-flowing and free from fast ice, shore diving allows us to access local sites with minimal fuss. The set up is analogous to how we will operate on sea ice. All dive gear, including life lines and communication box is loaded into a trailer and pulled along by a skidoo to the shoreline.



Ryan and Pete shore diving


The Marine Team outside of the Bonner lab with diving gear in a box sledge fixed to a skidoo

We are loosing daylight fast but as a result, we are getting some excellent sunrises over the Antarctic mountains located on the peninsula.  As I write, the sun is rising at 11:00 am. Walking to work in the dark is a strange transition, though with clear skies littered with stars, it's worth it. Similarly, by the time the working day is over, the sun has already set (15:45 today!). 

In a few weeks time, will will say goodbye to the sun with a ceremony at the highest vantage point (the cross) to say goodbye to our star. 


Morning sunrise over North Cove


Late morning light - view from my office

In the meantime, on still days with low wind, sea ice is gradually forming around Ryder Bay.



Sea ice sheets in Ryder Bay encapsulating icebergs


Comments

  1. holy moly absolutely love reading these Nadia! The pictures are stunning and you're adventures sound epic!!! Much love xxxx

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  2. Thank you so much anonymous!! Who are you!!!

    ReplyDelete

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