ARCTIC SEA-ICE –Another Blip–

A blip on the “extent” graph has separated the decline of sea-ice this year from past years, making it look like there is more sea-ice this year. Is this true, or an illusion?

The melt is far from over, and the amount of the end-of-summer melt can vary considerably. Just in recent years it can be seen, in the above graph, that roughly twice as much “extent” vanished in 2020 as did in 2021. (The x-axis gradations in the above graph represent 2 million km2. Therefore 2020 saw a loss of 2 million km2 and 2021 saw a mere million km2 melt.) As our extent is currently roughly 0.8 million km2 above what it was in 2020, we’d have to lose that much more to reach a level approaching the 2020 minimum.

The most amazing reduction of “extent” was in 2012, due to a big summer gale that formed over the Pole and caused some major stirring of the Arctic Sea. That year there was a thick, cold “freshwater lens” over slightly milder and saltier water, and when the stirring brought up the milder water the sea-ice vanished with startling rapidity. Or at least I was startled. That April I was expecting the sea-ice to make a comeback, for it was nowhere near the lowest that records had seen; in fact, it was 27th lowest. Yet by August it was lowest ever seen. I was so amazed I confess I actually suspected fraud was involved.

But one nice thing about that time, (only ten years ago but now seemingly a different universe), was that you could write a polite email to scientists and get a polite reply, and I contacted scientists who were actually up in the Arctic at that time, and I got a wonderful reply from a gentleman who had actually been on flights over the Arctic Sea, and he described how amazed he was that so much ice had vanished so swiftly.

Also, scientists back then were not so swift the blame Global Warming and leave it at that. I recall discussions about how a shift in the AO had caused a shift in where the outflow of the Lena River wound up, and how this caused a thickening of the “freshwater lens” towards Canada. While such articles tended to have an obligatory genuflection towards Global Warming in the final paragraph, the body of the paper was full of fascinating wonders. Here is one about that shift, from January 2012, (if I’d been more on-the-ball, I’d have suspected the “freshwater lens” might affect the melt the following summer.)

After that amazing melt in the summer of 2012 everyone seemed made more aware of the effect a summer gale might have, and therefore Alarmists were expecting great things (in terms of melting) when an equally impressive gale developed the summer of 2013. To the surprise of many (including myself) far less sea-ice melted. In fact, the sea-ice seemed to slosh around and hardly melt at all.

I never saw a paper explaining why the sea-ice failed to melt; perhaps it was given a good leaving-alone because it did not support the narrative concerning Global Warming. However, it seems apparent the water under the sea-ice must have been altered. Perhaps the 2012 gale demolished the “freshwater lens”, and also “used up” the heat and salinity stored in the stratified water beneath.

It seems apparent that there are variations in the layering and makeup of the waters of the Arctic Sea which may rival the changing makeup and layers in our atmosphere. Perhaps there are the equivalent of warm fronts and cold fronts, and even watery “jet streams” at various levels.

Last summer I spent some time attempting to envision what changes might be brought about by a major eruption of lava on the Gamal Ridge. (Basically, it would screw up preconceptions and mess up carefully crafted maps of existing currents, by creating a plume of ascending water where water ordinarily should be descending.) This subject is another which seems to have been given a good leaving alone, at least since 2008.

https://volcano.si.edu/volcano.cfm?vn=377020

To return to the subject of the “extent” of the sea-ice this summer, I think we cannot have a good idea of how the extent will diminish without a clear map of the sub-ice currents. We need a clear idea how the stratification of the water has proceeded. How thick is the “freshwater lens” and how has it shifted? How stratified is the water, and what is the temperature and salinity at various levels. We need more buoys. Lots and lots of buoys! Send much more money, please. (It is a far more worthwhile investment than the Clinton Foundation).

In the meantime, we have little to go on. I have noticed an abundance of small storms (“Ralphs”) over the Pole this summer, though so far none rival the gales of 2012 and 2013. Their cloudiness perhaps explains why temperatures have largely been below normal. (The lone spike above normal occurred as a high pressure’s sunny spell drifted over the top of the earth.)

The current dip in temperatures occurred as yet another small low drifted past the Pole.

This is occurring just as the temperature map shows the reappearance of the sub-freezing isotherm at the Pole; the surface thaw is ending.

Back when we had buoys with cameras up there, we could see the meltwater pools atop the sea-ice start to freeze over, but also we witnessed that the melt continued from below the sea-ice, and often saw areas of ice crumble even as temperatures above the ice dropped below freezing. Typically, more sea-ice melts than freezes until mid-September. So, where should we be looking? We should look where the sea-ice is most thin, and for this I like the NRL (Naval Research Lab) maps.

The lilac, especially the light lilac and white, represents the thinnest and most-likely-to-melt ice.

For comparison I’ll include a NRL map for the same day in 2020

One increase that jumps out at me is the increase in sea-ice in the East Siberian Sea, between Wrangles Island and the New Siberian Islands. This seems to happen when the PDO is colder and during La Ninas, though I can’t claim to understand the dynamics. In 2020 this area was largely ice-free by September, but I doubt it will happen this year. First, because the ice is thicker to begin with, and second, because that water was ice-free in 2020 it was exposed to cold air during the refreeze, which seems to “shock the system” and disturb any warm and salty layer beneath any freshwater lens. (I say “seems” because I haven’t seen any actual study.) Therefore it “seems” that, even if there was a big gale, the effects would be more like 2013’s rather than 2012’s.

A comparison of the two maps also shows an increase of thicker ice north of Greenland. While this makes no difference in terms of “extent” graphs, it does make a difference in terms of “volume” graphs.

The “volume” graphs involve many variables and the difficulties of modeling, so I tend to be a little leery of their accuracy, but they have given Alarmists a problem in recent years by refusing to show the expected decreases. The PIOMAS graph does show a sharp decrease between 1997 and 2010, but the curve has seemingly bottomed out since 2010.

Despite a mysterious subtraction of 2,000 km3 of sea-ice (see previous posts) the DMI model shows a recovery of volume to levels near 2018’s.

In conclusion, it seems highly unlikely that this year will see the long trumpeted ice-free Arctic Ocean we’ve been promised. But this is not to say the researchers don’t deserve more funding. They do. Much that influences weather further south occurs up there and is worthy of our wonder.

Stay tuned.

ARCTIC SEA-ICE –Volcano Under The Ice?–

One thing I’ve learned, as I have attempted to fact-check Alarmist’s sensationalist claims over the past decade, is that sea-ice exists in a sort of teetering balance between a single power that chills, and a multitude of powers that warm.

The single cooling power is the loss of heat to outer space, which continues at a quite regular rate 24 hours a day 365 days a year. Although clouds, and sea-ice itself, form insulation slowing the escape of heat at the surface and from waters beneath the ice, the hungry maw of outer space is constant in its demands. It is the loss of heat to outer space that creates the sea-ice.

Countering this chilling are warm forces constantly attempting to melt the sea-ice. These forces include many that operate even in the dead of winter, including warm air masses, warm currents, the temperature of the Arctic Sea itself, and rising warm plumes of water over undersea volcanoes. But the force that gathers the most attention is sunshine, which only operates six months a year.

The theory called the “Death Spiral” worries that, once the sea-ice is melted, the darker water will be able to absorb more sunlight than the white sea-ice, due to “albedo”, and this will cause the water to warm, and warm water will melt more sea-ice, and this will become a vicious cycle until there is no sea-ice at all, which will cause dramatic, disastrous warming over the rest of the planet.

This worry is needless for a number of reasons. Perhaps the most obvious is that the Arctic Sea has been ice-free in the past, perhaps as recently as the Medieval Warm Period, (and perhaps, on the Atlantic side, as recently as 1817), and there was no vicious cycle seen. If it didn’t happen then why should it happen now? Other reasons the worry is needless are less obvious, but have been fascinating to study.

The first is that when the sun first rises at the Pole the snow is at its most pristine and Albedo is at its highest. Also the ice is chilled to as much as forty below, at the surface, and even when the surface is warmed the chill lingers down deeper in the ice. The sea-ice is so cold salt can’t melt it, and a surprising amount of salt-dust is mixed in with the snow in places. Then, as the sea-ice is warmed from both above and below, the salt starts to melt the sea-ice, which actually is a process which uses up available heat. (Think of an old fashioned crank-operated ice-cream-maker.) All in all there is so much resisting the warming that it often isn’t until the days are already starting to grow shorter that slush starts to form on the surface, and melt-water pools appear

Melt ponds in the Beaufort 14 July 2016 NASA sm

Because these pools are darker, at first they indeed have a lower albedo and absorb more sunlight, however as August proceeds they start to skim over with ice, because the sun is dipping towards the horizon, and, once the angle of the sun gets low, water (especially when it is glassy) reflects sunlight (think of the late-day glare which requires sunglasses). Water then has an albedo as high as sea-ice, especially dirty sea-ice. Therefore the sea-ice melt seen in September is largely caused by the warmer water under the sea-ice, and not the sunshine above. Lastly, because the open water largely appears when the sun has ceased to penetrate the water, the sunshine cannot be heating the water and cannot contribute to a “Death Spiral”.

A second fascinating thing to study is the drift of the sea-ice. It turns out the amount of sea-ice at the Pole can be decreased not by heat, but by simply exporting large amounts to warmer waters (which happened to such an sensational degree in the spring of 1817 that there was open water north of Svalbard and Greenland, yet icebergs grounding on the coast of Ireland.)

A third study is the wandering currents which feed warmer water into the arctic. These currents apparently vary in their temperature, depth and location, having something to do with a cycle of roughly sixty years called the AMO. (Atlantic Multidecadal Cycle). In the past fishermen have noted some dramatic shifts in the location of fishing grounds, and there are incidental reports in historical records of notable changes in water temperatures, and how much ice is along coastlines, and how far glaciers extend into the sea. While these historical reports are dismissed by some scientists as anecdotal and too scattered to be useful, scientists themselves only have scattered data back sixty years ago, when the AMO was last doing what it now (perhaps) is going to do again. But a “Cycle” is very different from a “Death Spiral”, and currently there is more evidence the arctic follows cycles than evidence it is headed down a one-way street to disaster.

A fourth effect has been studied even less than the AMO, and is the occurrence of under-sea volcanos. This has grabbed my attention now due to the appearance of a mysterious hole in the sea-ice, seen in the NRL maps starting roughly at the end of March, but only sizable and clear over the past thirty days. It is located roughly at 85 degrees north and 110 degrees east.

I have only seen this sort of event once before, roughly seven years ago, at roughly the same location. Back then a reader asked me what it was, and I had no answer. They suggested it might be caused by a plume of warm water rising from a volcano, but that particular event was so brief I could only shrug it off and say “perhaps”, but confess I had never read of such a thing. But this one has been longer lasting. It appeared to be associated with no above-freezing temperatures nor with a lead or pressure ridge in the sea-ice, and also to move in a very odd manner. For example, when the sea-ice drifted to the right it would drift more slowly and even seem to stand still, and when the sea-ice swung around and drifted the opposite way it would remain in the same place. Lastly it has persisted despite constantly sub-freezing temperatures, and even to be enlarging. To me this seems consistent with a plume of milder water rising and persistently melting the sea-ice from the bottom.

Now seems a good time for the Navy to plan some sort of long distance training flight, and also to drop some sort of buoy or sensor into that water. If I was a sea-ice scientist I’d be hectoring and wheedling for such an expenditure. I imagine such events (if it is truly such an event) are not that common.

It is also interesting to think about the effects of such an upwelling. Likely it would derange the system of currents at that location, at various depths beneath the sea-ice, and trouble the stratification of water with upwelling turbulence. This in turn would have an effect “downstream” in the temperature and even location of the currents involved, which in turn could effect other currents.

We have heard much talk about “tipping points”, and how bovine flatulence and curly lightbulbs are things the fate of our planet hinges upon. However here we may be seeing a far more meaningful event, which could have repercussions like dominoes, and lead to interesting changes. Likely it has happened before, but by studying what happens this time we may be able to to look backwards and say, “Ah ha! So that is why that happened!”

In any case, it gave me something to get excited about during a basically dull time at the Pole. There has been a “Ralph” sitting over the Pole, but it was weak and the air has basically stagnated up there, without any roaring gales. There has been a slow but steady flow of sea-ice south through Fram Strait, but the current sluggishness of systems has revealed something that isn’t always apparent: Despite 24-hour sunshine, the arctic is still losing heat to outer space, and still creating cold air. Otherwise the DMI temperatures-north-of-80-degrees-lattitude graph could never show a downturn like this:

This downturn demonstrates that the Pole’s temperature is an equation, basically a fixed amount of heat being lost, and a varying amount of heat being added. To be a bit overly simplistic, in the dead of winter 100 units are lost and 70 added, which gives you a temperature of 30 below. Now, with more sunshine and warmer landscapes to the south, 100 units are lost and 90 are added, which gives you a temperature of 10 below. It is a bit of a misnomer to state the arctic is warming, for in fact it is still losing. It just isn’t losing as much.

In fact sea ice is still forming at the Pole. The “extent” graph only starts its yearly crash because large areas of sea-ice in more southerly climes, such as the Sea of Okhotsk, melt away. This year we are a hair behind last year’s rate of decrease (not that it means much this early):

Despite the loss of all the ice to the south, the “volume” graph shows the loss is countered by an increase in sea-ice to the north, and the total volume never starts to drop until around about this time every May.

This graph demonstrates that, despite a possible volcano melting the underside of the sea-ice at one locale, we have more ice up there than last year.

I hope to post again soon, with some maps of the weather events up there, now that my taxes are done. (The dull period may be ending, as a bit of a Barents Sea Blaster may be brewing). But I figured I’d whip off this post to alert people to the possibility of an undersea volcano up there.

Stay tuned.