update on buoy drift, april-jul19
left a long name mosaic buoy in by mistake
Mosaic travelled a fair way west before heading south again recently
I know 'compaction' of the CAB is supposed to be the result of the GAAC, but when I look at this and other indicators of ice movement (eg blumenkraft), I see very little motion that is north/right of prevailing wind indications.
I know the rightward motion from wind direction has been documented in open water - but how strong is that pressure? In a generally full ocean it doesn't seem to be that great a force. Direction of least resistance (eg open water) or currents (?) would seem to be a stronger indicator of ice movement as observed.
Large leads/open water in the CAB in July don't seems to be the norm in any year - and sparse areas like those currently observed in the Beaufort, Chukchi, and ESS form rather randomly every year due to localized melt out and ice movement.
The GIF posted by JayW above shows ice movement that expands and compresses frame to frame as that arm of ice moves northward and melts - there are some other forces that are moving those individual blocks of ice in multiple different directions.
I am not trying to deny the science - just wondering if people are not over-emphasizing a rather weak force and reading too much into 'compaction', and not enough into continuous melting in the CAB.
Just another question - the reason ice skates work so well, in that ice under the pressure of the blade melts reducing friction. in a generally warm arctic environment with long term compaction pressure, is the ice on the edges of individual flows being pushed together actually melting under that pressure? Is the force applied strong enough to actually provide another source of melt?