edited by Sam Carana
The loss of Arctic sea ice appears to be flattening out at the moment. The above image shows Arctic sea ice extent (total area of at least 15% ice concentration) for the last 7 years, compared to the average 1972-2011, as calculated by the Polar View team at the University of Bremen, Germany.
Paul Beckwith, B.Eng, M.Sc. (Physics), Ph. D. student (Climatology) and Part-time Professor, University of Ottawa |
Paul points at the image below, from weather.unisys.com/gfsx, showing a 9 day GFSx model for Arctic region.
The model shows that an Arctic cyclone is amplified as a result of Leslie and a strong high pressure ridge is also generated over the Beaufort Sea. As the Arctic cyclone decreases in strength a strong cyclone is generated over Alaska.
“Needless to say this scenario would be very destructive to Arctic sea ice if it plays out,” Paul adds. “Also, there is no apparent decrease in Arctic sea surface temperatures in projections out to September 12th, and no apparent salinity change. I will be amazed if this melt season does not last until the end of September or even into early October.”
View Paul Beckwith's September 8 presentation by clicking on the following link:
https://docs.google.com/file/d/0ByLujhsHsxP7QndrZjdKX2szTHM/edit
Or, view the presentation in the window below (it may take some time for the file to fully load).
The way storm like Hurricane Leslie starts track across Atlantic to make great sweep upward to the North and likely join up with storm circulation in Arctic is something on a scale not likely seen before. It's due to sea ice loss in Arctic induced by fossil fuel use of man that this can now occur.. It doesn't bode well for Earth's chances of reversing global warming even with all our efforts put to trying to stop the transition that's happening..
ReplyDeleteHate to think what is in store when methane from Shallow continental shelf of Arctic Sea starts to hit surface en mass. Seems like the lessening of heat differential between high latitudes and the equator is likely to cause maybe conjoining of storms previously unable to really happen.