De-Coiling of Canadian side of Pole causes pan-Arctic sea ice expansion in extent

  Other effect of Transpolar Stream being nothing but a loose gathering of pack ice floating about with the winds,  is de-coiling of the densest pack ice left:

  The Canadian side of the Pole is literally breaking apart.

This has huge consequences throughout the Arctic,  namely expansion of the loose pack towards Russia, Fram Strait bulging and Canadian Arctic Archipelago invasion of decompressed sea ice:

The tide current in the CAA is uninterruptible ,  no matter where the winds originate.  The Straits cause a funneling of massive area (not height)  of Arctic Ocean daily tides pushing against the Archipelago NW shores.  If sea ice becomes looser in its densest pack,  more free flowing sea ice gets carried by tidal currents. WD September 13,2016 

Plenty of melting not that it shows numerically

Franz Josef Land has near 0 C temperatures, but with sst's +2 C

Goodbye Waves a plenty,  and some opposite Transpolar Stream action effectively returning the loose pack towards the North Atlantic on its Eastern sector:  

JAXA chart  keeps on showing expansion of sea ice,  which is exactly following the 15% rule.  

There is likely no freezing,  mainly moving loose sea ice in contrary direction of the Transpolar Stream:

Looking carefully,  even with colder sea water and air near the Pole,  there is a presence of Goodbye Waves.  But far skinnier than near Franz Josef Lands.  

  The apparent open water gap filling sea ice is nothing but pack ice having plenty of dispersing room.  Note a huge sector of denser pack ice as well moving towards Russia,  likely part of de-coiling of Canadian side sea ice.    The 15% rule is very bad in describing this event pictographically. The sea ice provenance area has more expanded open water,  this does not show at all on JAXA chart,  because there is a great deal of shattering,  sea ice moving one way,  transpolar current moving the other,  plenty of stress, movement and collisions, but what the chart doesn't show is the vastness of open sea water.  Much greater than ever before near the North Pole.  WD September 11,2016

Titanic case reopened!

~National Geographic excellent presentation about likely reason for R.M.S.  Titanic collision with Iceberg has only one problem:  Its not possible.

~ Actually said so after it was presented,  and now proof

~  Water walls are the rarest refraction effect ever,  never seen in the land of refractions.

Massive De-coiling Canada Greenland sector continues

   The thickest densest sea ice left in the Arctic is unravelling at its faults lines.

18z CMC Sep 9 2016 surface chart has no significant meteorological reason for this.

     This is what less sea ice does when missing megatons of pressure does not push towards Greenland. The flow is almost always Eastwards,  but a tempered jammed Eastwards.  WD Sep 10, 2016

Dispersion of very melted broken up sea ice makes the 15% rule obsolete

     Russian sector of the North Pole had clearly a net expansion of extent,  but not because it was freezing,  much rather from the poor condition of extremely thinned breaking up sea ice.   All while there was melting.  So it is very difficult to judge either how fast the melting is unless dispersion is taken into account.    The other way to judge is by Goodbye Waves:

    Dispersing more rapidly Goodbye Waves are a sign of melting amongst winds and currents.   Judging melting correctly would be to factor in,  not exclude by an arbitrary rule,  every parcel of open water and sea ice as accurately as possible.   WD Sep 9,2016

Atlantic Front Franz Josef Lands melt/retreat Northwards, dispersion of broken apart sea ice will eventually thin further and give dramatic extent drop

  We see thinning of sea ice loose packs almost everywhere in the Arctic Ocean,  here North of Franz Josef Land Russia, is a retreat of sea ice Northwards.  This flow has no solid pack to recoil on and therefore is breaking apart.   Note Goodbye Waves to the South of the Front indicate great melting.  The new open water areas, numerous as they may be,  are highly likely not recorded by extent numbers 15% per grid regulation.

   Superimposed JAXA map September 5 (white black) September 7 (in colour).  The colour gains,  on the Leeward side (winds counterclockwise) of sea ice shores outnumber the black and white september 5 map by a far greater extent,  black being mixed with colour on the largely steady compacted windward side.  This masks the real melt numbers further.  Eventually,  further dispersion will show dramatic melt results. WD September 8,2016

De coiling sea ice , a sea ice momentum reprieve North of Greenland.

Some of the toughest thickest sea ice is also decompressing North of Greenland,  the pressure from
the usual sea ice momentum given by the Transpolar Stream Current is non-existent.  The response is a de coil action Northwards then an easier flow Eastwards.   This action is not noiseless,  luckily not many people live there,  there should be some thunder rumbling to be heard.  WD Sept 7, 2016

N.P. to Ostrov Komsomolets once ice bridge in taters, dispersing greatly as well as melting

   It was the strongest ice bridge in summer 2016, was from the Pole to Russia,  principally because there was a thinner snow layer which created the thickest ice possible given the warm winter just past.   Now its moving apart rapidly,  look at the central open water ridge moving fast Eastwards. Goodbye Waves a plenty can also be seen on the Leeward side on Sept 7 (left shore).   The Ostrov  Komsomolets ice bridge was huge apparently invincible:

   And now dispersing with the winds,  becoming larger in the process and distorting the melt view.  WD Sep7,2016

A lot of confusing action explains extent drop stall

   Apparent to all is the Transpolar Stream fill,  in a mere day,  affecting extent readings,
there is also false snow reflections particularly in the Canadian Arctic Archipelago, fallen floating snow appears as sea ice.

 There was no real fill of the Transpolar Stream,  just counterclockwise movement enabling by stress more shattering of larger ice pans,  in other words greater scattering affecting the 15% sea ice grid numbers to rise.  WDSep6,2016

Some effects of open water Transpolar Stream Current

It is not so obvious,  there is the Atlantic front,  where there is far less sea ice momentum pushing slowly to the North Atlantic:

  August 26 to September 4  East of Spitsbergen.    Appearing steady or moving North with a lot of melting.

  Fram Strait substantial extent gains with likely the most solid dense ice left unencumbered by TPS sea ice ,  hence the stretching out sea ice peninsula not with numerous Goodbye Waves,  but heading certainly to melt at a much slower rate than Atlantic Front sea ice.WD Sept5,2016