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William Hughes-Games
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I wonder if the opposite could also happen. Think to the future when much more of the Arctic Ocean is ice free for longer periods in the summer and hence has accumulated much more heat. Toward fall, as the incident radiation on the surrounding land decreases, at some point, snow falls and doesn't melt. The land cools off very rapidly since only the top foot or so is involved. Now you have a very cool area surrounding the ocean, with the air above the land cooling off and falling. Over the ocean, by contrast, the heat accumulated in the summer is warming the air and putting much water vapor into the air. You have a positive AO from the surrounding land to the ocean and Coriolis starts this body of air rotating counter clockwise. It would seem to be a formula for some very strong cyclones in late summer and fall. Since in an anticlockwise rotating system, Coriolis is away-from-the-centre, if the ocean is spun counterclockwise by the storm, ice and fresh water should be pushed toward the exits from the Arctic ocean, making the surface water shallower and bringing the deep, salty, slightly warmer Atlantic water closer to the surface. The longer, higher waves from such storms will then be able to mix these layers more effectively, further pushing the Arctic toward an ice free condition.
On persistent cyclones
As the persistent Arctic cyclone - or PAC-2013 - of the past couple of weeks winds down, I want to discuss what I've found on the subject in a couple of research papers. But first want to refer to two excellent blog posts from last week doing just that, on the Robertscribbler blog and FishOutofW...
At some point we should start to see large storms in the fall as the freezing of water and the giving out of latent heat keeps the air above the ocean relatively warm, relative to the land that is rapidly cooling off. Large Storms are generated by pressure differentials and in the tropics require water temperature above 25 degrees C. This is because over an open ocean, all the pressure differential is generated by the storm itself. In the Arctic, they require sufficiently high pressure over land relative to the pressure over the sea. I suspect the storm of 2012 was such a storm. It is likely that this year there is not enough open water to generate a mega storm.
SEARCH 2014 Sea Ice Outlook: July report
The second Sea Ice Outlook of this year has been published. The SIO is now organized by the Sea Ice Prediction Network (as part of the Arctic research program 'Study of Environmental Arctic Change', or SEARCH), and is a compilation of projections for the September 2014 Arctic sea ice extent, ba...
This is probably simplistic but aren't we seeing a negative feed back amongst all the positive ones we have been focusing on. Thinner ice and a lot of cracking at the beginning of the melt season led to increased heat and water vapour entering the atmosphere (and of course, cooling the water/ice). This causes rising air and low pressure systems with clouds which shades the ice. Storms, when the ice is fairly wide spread can't have the effect on the sea as they do later in the season when they can create large waves and ice scattering. A storm a the height of the winter, for instance, hardly causes waves at all.
Gaia is fighting back and while the over all trend will undoubtedly continue, we could see more of these odd years. At some point the ice at the end of the freezing season will be so thin that early storms will shatter it.
ASI 2013 update 6: major slowdown
During the melting season I'm writing (bi-)weekly updates on the current situation with regards to Arctic sea ice (ASI). Central to these updates are the daily Cryosphere Today sea ice area (SIA) and IJIS sea ice extent (SIE) numbers, which I compare to data from the 2005-2012 period (NSIDC has ...
The rate of melting increased sharply following the storm of Aug6. Was this due to a mixing into the surface waters of the deep, warmer Atlantic water. a single meter of water which is one degree above the melting point of ice contains enough heat to melt 12.5mm of ice. There is more than enough heat in the artic water to melt all the ice many times over. Have any salinity measurements been made to see if such mixing did occur.
Peeking through the clouds 4
Commenter dabize has sent me the latest 'declouded' version of the False-Colour Composite images Environment Canada makes of the LANCE-MODIS satellite images. They give us an excellent view of week to week changes. Due to some resolution incompatibilities I had to exclude last week's image (it's...
Could this melting be the first sign of a Walker cell developing between rising moist air over the open part of the Arctic ocean (and Atlantic, for that matter) and the descending katabatic (density) winds pouring down the slope of the Greenland Ice Sheet. The air that pours down Greenland has to come from somewhere.
Greenland melting breaks record 4 weeks early
There already was a suspicion that this year would become a record year for Greenland ice melt, after all the real-time information we received from Dr. Jason Box with regards to the reflectivity of the Greenland Ice Sheet (see Dark side of Greenland), the extremely high temperatures in much of...
So what happens when enough of the Arctic ocean is open water and becomes a giant solar collector such that it becomes an area of rising air instead of falling air. Presumably the Polar Hadley cell reverses and joins with the Ferrel cell (polar cell and polar jet stream disappears). The next jet stream down moves to about 45degrees North and takes up the job of pushing weather patterns around the globe. Heat is pulled by the northern most of the now two cell system toward the Arctic, melting what is left of the permafrost etc etc. A warm foehn wind blows over Greenland.
http://mtkass.blogspot.co.nz/2008/07/arctic-melting-no-problem.html
Arctic storm part 1: in progress
This is what I meant when I said 'flash melting' yesterday: Now it's there on the Uni Bremen sea ice concentration map, the next day, poof, it's gone. Mind you, not all of it is gone, the sensor is thrown off a bit due to that crazy cyclone downstairs, but it ain't exactly good for the ice if ...
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Oct 29, 2010
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