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: [email protected] 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 <[email protected]> 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] --~--~---------~--~----~------------~-------~--~----~ You received this message because you are subscribed to the Google Groups "geoengineering" group. To post to this group, send email to [email protected] To unsubscribe from this group, send email to [email protected] For more options, visit this group at http://groups.google.com/group/geoengineering?hl=en -~----------~----~----~----~------~----~------~--~---
