Another day on the ice
Anyways, we jumped into the helicopter at about 13:00 after having eaten our packed lunches on the ship, and headed towards the Greenland coast to try and bag some of the most westerly samples that we will collect. As we approached the coast, a distinct line was visible in the ice running north-south as far as it was possible to see in either direction (see picture below). This is the boundary between sea ice drifting slowly southwards over the East Greenland Shelf (left hand side ) and 'fast-ice' which is sea ice that is permanently frozen to the coast, and pinned in have run aground (right hand side). The ridge is the result of the moving ice being pushed up against the stationary ice.
Theoretically one could walk to Greenland from the western side of the ridge, as the ice doesn't drift and there are very few leads (areas of open water). In fact, there were so few leads that we couldn't find anywhere to deploy our instruments and had to turn around after searching for a while.
We did manage to land in the two other places we had planned to though, and both sites turned out to be quite spectacular, with big pressure ridges and blocks of ice, which had been pushed up as floes had collided.
The flying team is now generally made up of two oceanographers and one sea-ice specialist. Today Gorm came with Edmond and I so that he could make some ice thickness measurements. This basically involves drilling a hole in the ice with a very big and very long drill bit, then measuring the depth of the hole. You can see him and the drill bits in the the picture below. The ice is quite easy to drill through, so he can just use an pretty ordinary cordless drill at the end of that thing even when all the sections are stuck together.
Still, hopefully the weather will be kind to us!
Paul
