About two and half weeks ago the Alfred Wegener Institute for Polar and Marine Research (AWI) issued a press release to inform us of the fact that their research vessel and icebreaker Polarstern had arrived at the North Pole. In the blog post I dedicated to this news, I mentioned a snippet about their findings concerning ice thickness. I have finally come around to read a bit more on AWI's excellent Polarstern Blog, and have translated some more snippets about ice thickness. All the images come from the Polarstern Blog as well.
Schollensuche richtung Nordpol
the search for ice floes on the way to the North Pole
In order to document the ice conditions during our journey we observe the sea ice on an hourly basis. The ice conditions are logged following an international standard. Ice cover, type, thickness and the distribution and amount of melt ponds are recorded and documented with photographs. Ice thickness is estimated with a yardstick aboard the ship by observing the broken ice floes that are standing upright.
A broken ice floe with a thickness of approximately 1 m (image courtesy of Stefan Hendricks, Alfred Wegener Institute)
The first results from our observations show that the sea ice is relatively thin, young and unstable. Older multiyear ice, which used to be typical for this region in the past decades, makes up just 10 to 20% of the observed ice. Consequently we can travel and navigate through the ice much quicker than in the past, and do not get stuck. On top of that the journey is made easier by many stretches of open water which allow us to travel at a speed of 3 to 6 knots (5 to 10 km/h) from one measuring point to the other. This gives us more time for operating our ice and water stations.
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