Smaller southwards bound Cold Temperature North Pole Vortex bends Jet Stream Northwards

~There is a windy reason why very cold air matters.

~Apparent single  near North Pole -30 C 700 mb cold zone in the entire Polar vortex not typical.

   CMC February 8, 2017 700 and 250 mb chart,  the 700 mb chart identifies the coldest zones,  where the atmosphere is densest and influences Global Circulation. On the Russian side, the coldest air is beyond the limits of this map further Southwards (at about -25 C at center).    The 250 mb chart (with blue arrows),   highlights the jet stream,  a segment of which is very unusually to the West of North Greenland.  The coldest air of this world,  I call it the Cold Temperature North Pole (CTNP),  is hovering over center of the Arctic Archipelago, 2 more vortices,  one over Newfoundland the other South Central Russia,  represent tonights outlook of the entire Polar Vortex.  Note the counterclockwise circulation around the 700 mb coldest air zones  (close enough to 600 mb, which is the approximate mean height representing the average temperature of the entire troposphere).    The Newfoundland one is steering the jet Stream Northwards as well,  as we know,  yet another Atlantic big Cyclone will penetrate the Arctic Ocean but for these reasons in a few days.  The coldest air zones are smaller,  usually to the South of where they use to hang out.  Contrast this with an imagined  huge 600 mb cold zone,  spanning from Alaska to Greenland,   the Jet would steer further Eastwards not Northwards.  The smaller densest cold atmosphere vortices affect the weather to be wilder near them as well. A huge CTNP area,  as common in the past,  made weather fluctuate less, because smaller CTNP's move about quite a lot.  WD February 8,2017

Barely familiar Arctic sea ice.

~Only lately does one segment of the pack look a bit normal.

   December 17 2016  to January 27 2017 NOAA ir HRPT .   The last picture in the animation sequence, January 27,  has the only recognizable feature North of Ellesmere Island,  long Tidal leads not quite the same as 20 years ago or so.  The round ring between Northeastern Ellesmere and Northwestern Greenland showed up at times as well.  What is abnormal is Smith Sound floe edge very fluid  sea ice moving with the current and dominant wind,  North to South,  many marine wildlife depend on that area especially East of Jones Sound (extreme Southeast Ellesmere Island).  We can see a strong current from barely frozen fluid ice moving in Barrow Strait  to Lancaster Sound  ending up still very swift Eastwards to North Baffin Bay.   Kennedy to Nares Strait never froze as well.  The biggest change is the lack of deep freezing North of Ellesmere Island, this area usually can have temperatures as low as -55 C.     Infrared 'white signature zone can be recognized at times,   mainly Southwest of where it should be,  this location change is quite significant.   North of Ellesmere had a faint start of cooling mid December from the presence of a High,  but it did not last.  Pervasive clouds made selecting fewer pictures,  this is not the regular long night view,   clouds rarefy with the drying process of radiation escaping to space in darkness without sunlight replenishing heat.    Throughout this GIF sequence, Arctic Ocean pack ice leads direction features changed rapidly with the winds,  indicating the presence of thinner sea ice and more open water The area North of Ellesmere Island is known having the densest-thickest most stable ice history,  this is the area to watch,  the ring between Northern Ellesmere and Greenland usually should vanish slowly while remaining in place,  what we observe here is its destruction by fluid ice movement.  30 years ago,   just off Northwest Greenland sea ice buoys remained immobile throughout the winter season. WD January 28,2017