Here is a Greenland Sea animation of the last week, actually I don't see much evidence of an increase of the Fram transport. Some larger digital artifacts (squares bigger than the 3.125km pixel size) shows that the Arstist Sea Ice (ASI) algorithm has some trouble on the ice edge here.
I agree - certainly doesn't look like much movement at all out of the Fram.
Intuition/what I'm seeing suggests a refreeze; however, from what I've seen elsewhere regarding weather, neither the air or sea surface temps are low enough to support that. I wonder what's going on?
There is a 980mbar cyclone before the east coast, I think this causes the following to be applicable:
3.1. Weather Filters
One disadvantage of the 89 GHz channels is the pro-
nounced influence of atmospheric cloud liquid water and
water vapor on the brightness temperatures. Especially cy-
clones over open water can reduce the polarization differ-
ence to values similarly small as those of sea ice. Therefore
effective filters are necessary to remove spurious ice concen-
tration in open water areas. The weather filtering process
consists of three steps. All of them use the lower frequency
channels with lower spatial resolution. This does not lead to
a lower resolution of the marginal ice zone [Kaleschke et al.,
2001] but it may cause pixels along the ice edge to show too
high ice concentrations due to missing weather filters. If this
is the case the resolution of the ice edge is determined by
the resolution of the weather filter.
Spreen, G., L. Kaleschke, G. Heygster (2008), "Sea Ice Remote Sensing Using AMSR-E 89
GHz Channels", J. Geophys. Res., 113, C02S03, doi:10.1029/2005JC003384.
So, water vapor and liquid water in clouds (associated with weather fronts) cannot be compensated in the hi resolution over the very fragmented ice cover (it is all edge actually) of the Greenland Sea.
Wait for the clouds to clear, and the ice concentration should drop.