Talk about unpleasant surprises (see my previous posting below), look at 
this:

'Warm everywhere' in Arctic this winter

While parts of North America have been in the icy grips of an unusually cold 
and snowy winter recently, the Arctic has been downright balmy compared to 
past winters.

http://www.msnbc.msn.com/id/29038734/from/ET/

(with thanks to Albert Kallio for finding this)
----

'Warm everywhere' in Arctic this winter
Expert: Dec.-Jan. temps drop, both are 'crucial ice-growing months'

By Andrea Thompson
updated 5:13 p.m. ET Feb. 5, 2009
While parts of North America have been in the icy grips of an unusually cold 
and snowy winter recently, the Arctic has been downright balmy compared to 
past winters.

These warmer-than-normal temperatures mean that the sea ice in the Arctic is 
looking pretty anemic, despite the winter season.

Arctic ice goes through a normal cycle of summer thaw and winter re-freeze. 
In recent decades, however, sea ice has become overall less extensive and 
thinner, leading to forecasts that in future decades the polar region will 
be ice-free during summer. The trend looks to be continuing this winter, 
scientists now say.

Climate swings in any single season are part of Nature, of course. That's 
why records - warm or cold, wet or dry - get broken. For much of the United 
States, this winter has been an exceptionally chilly one.

The average temperature for the United States in December, 32.5 F, was 
almost 1 degree Fahrenheit below the average for the 20th century, according 
to the National Oceanic and Atmospheric Administration. Much of the West and 
Midwest had a particularly frigid month, with temperatures plunging several 
degrees below average.

This winter in the Arctic has been a completely different story.

"It's warm everywhere in the Arctic. It's anomalously warm," said Julienne 
Stroeve, of the National Snow & Ice Data Center (NSIDC) in Boulder, Colo.

Both December and January have been abnormally warm months, which impacts 
the cyclical re-freezing of sea ice over the years, because these are "two 
crucial ice-growing months," Stroeve told LiveScience.

Thinner ice, more melt
Arctic sea ice hasn't been reaching its former thicknesses and extents in 
recent years, especially after the dramatic meltdown observed in the summer 
of 2007, which opened up the fabled Northwest Passage. (This past summer saw 
the second lowest summer ice area on record.)

That record melting - which left 30 percent less ice in the Arctic than 
there was at the previous record low - caused the loss of substantial 
amounts of older ice, which is thicker and generally survives the summer. 
Older, thicker ice is typically 6.5 to 10 feet (2 to 3 meters) thick, while 
younger ice is closer to 3 feet (1 meter) in thickness.

Melting exposes more areas of open ocean, which absorbs incoming sunlight 
that the ice would normally reflect, so there is the potential for a 
snowball effect, or what scientists call self-reinforcing or feedback. Come 
winter, the ice that refreezes is thinner, first-year ice, which is more 
susceptible to melt in the summer, potentially exposing even more open 
ocean.

"That [thinner ice] typically can all melt out in the summer," Stroeve said.

This year, the future
That feedback seems to be kicking in, as now "the Arctic is just more 
dominated by that thinner ice," Stroeve said, adding that unless February 
and March are much colder than normal, this winter's ice could end up 
covering less area than normal and be thinner than even in recent years.

So far, this winter has been warmer than last, Stroeve said, and some odd 
weather patterns cropped up in both December and January that brought ice 
growth to a standstill. Pauses in the regrowth of ice aren't a new 
phenomenon - they have happened before, even in much colder winters - but 
they only exacerbate the current situation in the Arctic by adding yet 
another mechanism that stagnates ice growth.

In January, these weather patterns created different conditions in different 
parts of the Arctic. While ice grew southwest of Greenland, it retreated in 
areas east of Greenland and in parts of the Barents Sea, the NSIDC reported.

While ice is still re-freezing, ice coverage area at the end of January was 
still 293,000 square miles (760,000 square kilometers) less than the 
1979-2000 average, according to the NSIDC. This didn't break the record low 
for January ice area (set in 2006), but it put January 2009 in the top six. 
Including this year, January ice area is declining by about 3 percent per 
decade, the NSIDC reported.

Looking further into the future, unless there are several very cold winters 
and mild summers, Arctic sea ice is unlikely to bounce back in the coming 
decades.

"The idea of recovery right now seems pretty slim," Stroeve said. "You just 
don't get very cold temperatures like you used to."

Eventually, the sea ice is expected to melt out entirely in the summer, 
leaving only a cover of winter seasonal ice. The NSIDC predicts that this 
will happen around 2030, though Stroeve says it could happen earlier, as 
indeed some other scientists predict. That it will happen seems fairly 
certain: "There's no doubt in my mind about that," Stroeve said.


----

Cheers from Chiswick, where it has been unusually cold and snowy, as in 
parts of N America,

John



----- Original Message ----- 
From: "John Nissen" <[email protected]>
To: <[email protected]>
Cc: "geoengineering" <[email protected]>
Sent: Friday, February 06, 2009 6:43 PM
Subject: Re: [geo] Re: runaway arguments ripped to bits


>
> Hi dsw_s,
>
> You are right about the relative size of heat flux compared to albedo 
> effect, but it is the _change_ in heat flux which is important to compare, 
> e.g. any increased heat flux from the Gulf Stream entering the Arctic 
> Ocean.
>
> Anyway, whatever is the root cause of Arctic shrinkage, it is happening a 
> lot fast than IPCC predicted only a couple of years ago, and the trend 
> shows no signs of reversing.  Exactly the opposite - it has shown signs of 
> accelerating this decade.  There are recognised to be various cycles of 
> the northern hemisphere ocean-atmosphere system, but we certainly cannot 
> rely on such a cycle to rescue us by reducing heat flux into the Arctic 
> and switching off the sea ice retreat.
>
> We can indeed expect surprises, but we cannot rely on them being pleasant 
> ones!  Indeed, most have been extremely unpleasant, of late.  Thus the 
> urgency for geoengineering is, if anything, increased, taking into account 
> the precautionary principle.
>
> Cheers,
>
> John
>
>
> ----- Original Message ----- 
> From: "dsw_s" <[email protected]>
> To: "geoengineering" <[email protected]>
> Sent: Friday, February 06, 2009 1:04 PM
> Subject: [geo] Re: runaway arguments ripped to bits
>
>
>
>>The "forcing" from the sea ice albedo effect is of the order of 30 Watts 
>>per square metre, so you expect this to drive regional warming.<
>
> I expect surprises.  How does the total number of watts of forcing
> compare with variability in heat fluxes into and out of the region?
> What other feedbacks are there that we haven't thought about?  The
> vapor pressure over ice is less than over water at the same
> temperature, and the surface of ice can be cooler than the water
> below.  So evaporation will presumably be greater over open water than
> it has been historically over the sea ice.  If that water condenses
> elsewhere, that's a heat flux out of the region.
>
> Let's say we lose ten million square km of sea ice: that's 30
> terawatts of forcing.  But it looks as though there's over a petawatt
> of annually-averaged heat flux into the region, just by eyeballing a
> figure in a badly-out-of-date textbook.  So with even a modest
> relative change in heat fluxes, the effects of the forcing could show
> up somewhere else rather than regionally.  Or the regional effects
> could be an order of magnitude greater than the forcing would produce
> directly.  For a conclusion about that, I would be more convinced by a
> peer-reviewed analysis of a detailed model than by the simple-and-
> obvious argument.
>
>
> On Feb 6, 6:49 am, "John Nissen" <[email protected]> wrote:
>> Hi Andrew,
>>
>> It depends what kind of proof you want. I myself am convinced of things 
>> if there is a logical argument based on established facts.
>>
>> I am convinced by anthropogenic global warming because if you put an 
>> extra 100 ppm CO2 in the atmosphere, you EXPECT to have greenhouse 
>> warming. I don't need "proof" to be convinced. To be persuaded otherwise, 
>> I would need a convincing explanation of why the CO2 wasn't causing 
>> global warming, or how this was somehow neutralised. I would need to be 
>> PROVED WRONG.
>>
>> Similarly with methane runaway feedback. There's a vast amount of methane 
>> trapped in frozen structures. Nobody disputes this fact. If you put 
>> enough of this methane in the atmosphere, you expect global warming. You 
>> then expect positive feedback as a result of this, as the frozen 
>> structures unfreeze to release more methane until it's all gone. Unless 
>> there is an argument against this logic, I will remain convinced by it.
>>
>> Similarly with the Arctic sea ice and domino effects. The "forcing" from 
>> the sea ice albedo effect is of the order of 30 Watts per square metre, 
>> so you expect this to drive regional warming. Nobody is suggesting how 
>> this warming would reverse naturally. So, as the region continues to 
>> warm, you expect the domino effects of methane release and Greenland ice 
>> sheet accelerated discharge.
>>
>> This is all highly uncomfortable to contemplate, and I'd like to be 
>> proved wrong. However we do have a possible way out of this situation 
>> with geoengineering. So all is not lost.
>>
>> Please can we now persuade politicians and potential funding bodies of 
>> the inescapable logic of this situation, so that they fund the necessary 
>> geoengineering developments? Or prove me wrong.
>>
>> Cheers,
>>
>> John

[snip] 


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