I think that there needs to be a weighting of multi-year(?) sea ice melting at 
the core of the Arctic Basin in comparison to the any melting of (seasonal ice) 
at the periphery of comparable size.  If the core continues to destabilise, 
question is why?
Nuclear reactors melt at their core, same with old overgrown mushrooms - or 
trees. But that if the Arctic Ocean sea ice melts a hole into the middle, this 
would mean the periphery which will melt later in season, that very little ice 
could be left.
Let just hope that this deepening hole near the Pole of Inaccessibility is just 
a temporary anomaly that would disappear and freeze over rather than get 
enlarged. But in any case, melting or ice disintegration at the centre of Polar 
Sea Ice cap must have higher rating than similar advanced melting anywhere 
around the ice edges.
The sunshine factor of many hours from end of April to summer solstice is 
important. Let just hope this would be an anomaly and a sort of lead that would 
disappear.
Rgs, Albert

Hi David,
 
Many thanks for a good diagram! 
 
The issue at the moment is the decrease of sea ice at the very core of the ice 
over large area. On contrary, the Barents Sea and some other areas are holding 
plenty of ice, but knowing that by summer periphery melts more than the centre, 
it is not good-looking.
 
But I doubt re-freeze occurring easily, there is notable darkening of sea as 
well. I would make the question where? rather than how much? But by summer 
these will be answered. 
 
At this point of time the graph contains loads of volatile seasonal ice at the 
periphery, by the autumn it is core built around the Arctic Basin. I have 
discounted the periphery ice's significance and account far more weighting to 
the multi-year ice on the Arctic Basin.
 
I am finding it disturbing that the ice is destabilising at the core (the Pole 
of Inaccessibility) so early in the season (we just moved from April to May 
during the Bank Holiday weekend).
 
Kind regards,
 
Albert
 
 
And then there is the AMSR-E data:

From: j...@cloudworld.co.uk
To: dwschn...@gmail.com; albert_kal...@hotmail.com
CC: geoengineering@googlegroups.com; indian...@googlegroups.com; 
p...@cam.ac.uk; eha...@sheffield.ac.uk
Subject: Re: [geo] Re: Arctic Ocean Sea Ice Shows Extensive Weakening around 
the Pole of Inaccessibility‏ - Albedo
Date: Tue, 5 May 2009 18:29:19 +0100










 
Hi Albert,
 
Thanks for finding that picture.  Where did 
you find it?
 
The weakening is extremely worrying, considering 
the sun must still be low (<25 degrees?) at its noon elevation, north of 
80 degrees latitude.
 
I usually follow this report:
http://nsidc.org/arcticseaicenews/
It is interesting to look at the temperature 
anomaly picture, which shows unusual cold over the Arctic.  Presumably the 
trend of polar amplification continues by general warming of land mass and sea 
volume, while the air temperature fluctuates wildly.  Is that right?  
Could it be the underlying sea temperature which is causing that weakening 
around the pole of inaccessibility, coupled with the sea ice being single-year 
perhaps?  It is difficult to reconcile the weakening with a cold 
temperature anomaly.  Could cloud cover be an important factor?  When the air 
temperature is cold, there may be little cloud, so the sun gets through to melt 
the ice.
 
Cheers,
 
John
 
 

  ----- Original Message ----- 
  From: 
  David 
  Schnare 
  To: albert_kal...@hotmail.com 
  Cc: Geoengineering FIPC ; Indianice FIPC ; Peter Wadhams ; Edward 
  Hanna 
  Sent: Tuesday, May 05, 2009 3:28 PM
  Subject: [geo] Re: Arctic Ocean Sea Ice 
  Shows Extensive Weakening around the Pole of Inaccessibility‏ - Albedo
  

  And then there is the AMSR-E data:
   
  [deleted]
   
  2009/5/5 Albert Kallio <albert_kal...@hotmail.com>

  
    Further to the previous:
 
This image with albedo, near 
    natural light conditions suggestive of albedo-induced warming occurrence 
now 
    being likely around the Pole of Inaccessibility due to early (light) 
    season.
 
Rgs, Albert
 

    
    

<<arctic.seaice.bandw.003.png>> 

[snip]

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