Alarmists Gone Wild: Saving the Arctic Sea Ice from Oblivion With… Windmills!

Guest post by David Middleton

From the “Truth is Stranger than Fiction” files…

Windmills

Leave it to a researcher who studies icy moons in the outer solar system to come up with an out-there scheme to restore vanishing sea ice in the Arctic.

Ice is a good insulator, says Steven Desch, a planetary scientist at Arizona State University in Tempe. That’s why moons such as Jupiter’s Europa and Saturn’s Enceladus, among others, may be able to maintain liquid oceans beneath their thick icy surfaces. On Earth, sea ice is much thinner, but the physics is the same. Ice grows on the bottom surface of floating floes. As the water freezes, it releases heat that must make its way up through the ice before escaping into the air. The thicker the ice, the more heat gets trapped, which slows down ice formation. That’s bad news for the Arctic, where ice helps keep the planet cool but global warming is causing ice to melt faster than it can be replaced.

The answer to making thicker ice more quickly? Suck up near-freezing water from under the ice and pump it directly onto the ice’s surface during the long polar winter. There, the water would freeze more quickly than underneath the ice, where it usually forms.

In theory, Desch says, the pumps used for this top-down approach to ice growth could be driven by technology no more sophisticated than the windmills that have long provided water to farms and ranches on the Great Plains.

Desch and colleagues envision putting such pumps on millions of buoys throughout the Arctic. During winter, each pump would be capable of building an additional layer of sea ice up to 1 meter thick over an area of about 100,000 square meters…

[…]

Now is the time to begin detailed designs and build prototypes, Desch says. The Arctic Ocean’s end-of-summer sea ice coverage has decreased, on average, more than 13 percent per decade since 1979. “There’ll be a time, 10 to 15 years from now, when Arctic sea ice will be accelerating to oblivion, and there’ll be political will to do something about climate change,” Desch says. “We need to have this figured out by the time people are ready to do something.”

051317_notebook_sea-ice_inline

Science News

Professor Desch and his colleagues estimate that each ice-making buoy would cost $50,000 (including shipping and handling).  They estimate that it would cost $500 billion to cover 10% of the Arctic Ocean with ice-making buoys…

Ice grows on the bottom surface of floating floes. As the water freezes, it releases heat that must make its way up through the ice before escaping into the air. The thicker the ice, the more heat gets trapped, which slows down ice formation. That’s bad news for the Arctic, where ice helps keep the planet cool but global warming is causing ice to melt faster than it can be replaced.

So… Thicker ice traps more heat (insulation), causing the ice to melt faster, preventing the ice from keeping the planet cool (high albedo).  Makes perfect sense.

“There’ll be a time, 10 to 15 years from now, when Arctic sea ice will be accelerating to oblivion, and there’ll be political will to do something about climate change.  We need to have this figured out by the time people are ready to do something.”

“Accelerating to oblivion”?  Oblivion?

Oblivion

Since we know that the current Arctic sea ice extent is much larger than that of most of the Holocene, “oblivion” is probably not the place to which Arctic sea ice is heading.  If anything, it is returning to normal.  So, I don’t think these ice-making buoys would be the best place to “invest” $500 billion.

The Arctic was probably ice-free during summer for most of the Holocene up until about 1,000 years ago.  McKay et al., 2008 demonstrated that the modern Arctic sea ice cover is anomalously high and the Arctic summer sea surface temperature is anomalously low relative to the rest of the Holocene.

chukchi
Figure 1. “Modern sea-ice cover in the study area, expressed here as the number of months/year with >50% coverage, averages 10.6 ±1.2 months/year… Present day SST and SSS in August are 1.1 ± 2.4 8C and 28.5 ±1.3, respectively… In the Holocene record of core HLY0501-05, sea-ice cover has ranged between 5.5 and 9 months/year, summer SSS has varied between 22 and 30, and summer SST has ranged from 3 to 7.5 8C (Fig. 7). (McKay et al., 2008)

Stranne et al., 2013 demonstrated that the modern day Arctic sea ice extent is more comparable to that of the last Pleistocene glacial stage than to that of the Holocene Climatic Optimum (9,000-5,000 years before present).

Microsoft Word - Arctic sea ice -QSR revised
Figure 2.  Annual mean sea ice thickness for the three different simulations (Panel a) compared with results from published paleo-sea ice studies (Panel b). Black curve: constant surface albedo; red curve: dynamic surface albedo parameterization. The simulation implemented with a dynamic surface albedo parameterization was run from present time and backwards to address the importance of the initial state of the sea ice cover. The annual mean sea ice thickness from this simulation (orange curve) reveals a hysteresis of ∼1000 years. The annual mean insolation at 80°N shown with a stippled curve is based on the algorithm presented by Berger (1978). To compare the results from different paleo-sea ice studies a scale of sea ice concentration was inferred using the approach by Jakobsson et al. (2010). This scale must be considered as highly qualitative because none of the paleo-sea ice proxies provide absolute measures of past sea ice concentrations. The number preceding each bar representing the result of a paleo-sea ice study corresponds to the following references: 1: Hanslik et al. (2010); 2: Cronin et al. (2010); 3: de Vernal et al. (2005); 4: England et al. (2008); 5: Funder et al. (2011); 6: Bennike (2004); 7: Dyke et al. (1996); 8: Vare et al. (2009); 9: Belt et al. (2010); 10: Müller et al. (2012). MY = Multi Year; LF = Land Fast Ice. (Stranne et al., 2013)

 

holocene-1
Figure 3.  The Little Ice Age was one of the two coldest phases of the Holocene in the Arctic.

Funny thing about Science News

1975-03-01
Figure 4. “The Ice Age Cometh.” (Science News, March 1, 1975)

From March 1975 to May 2017, Science News has gone from “the Ice Age cometh” to “Arctic sea ice… accelerating to oblivion”… Ohhhhhh Noooooooo!!!

MrBill
Figure 5. Ohhhhhh Noooooooo!!!

References

Alley, R.B. 2000. The Younger Dryas cold interval as viewed from central Greenland. Quaternary Science Reviews 19:213-226.

Desch, S.  et al. Arctic ice management. Earth’s Future. Vol. 5, January 24, 2017, p. 107. doi: 10.1002/2016EF000410.

McKay, J.L., A. de Vernal, C. Hillaire-Marcel, C. Not, L. Polyak, and D. Darby. 2008. Holocene fluctuations in Arctic sea-ice cover: dinocyst-based reconstructions for the eastern Chukchi Sea. Can. J. Earth Sci. 45: 1377–1397

Stranne C, Jakobsson M, Björk G, 2014 Arctic Ocean perennial sea ice breakdown during the Early Holocene Insolation Maximum. Quaternary Science Reviews 92: 123132.

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Not Chicken Little
May 3, 2017 10:12 am

I don’t know what the problem is. If it gets too warm we can just have everyone open their refrigerator and freezer doors for several hours a day, and open the doors to the outside to cool things down. Problem solved! Where’s my grant money?

May 3, 2017 10:14 am

The usual, common unix command goes
‘unix requiry, command’ 2>/dev/tty/null
Yields
– unix require -> results
– superfluous output -> /dev/tty/null, cloud 9, OBLIVION
__________________________________________
some operations yield 10-100 times oblivion / result

Richard
May 3, 2017 10:32 am

Has this genius figured out yet that:
1) sea ice is made up fresh water with very little entrained saline water?
2) water pumped from beneath the ice will be saline, in fact, it will be concentrated saline compared to normal sea water?
3) saline water pumped onto the sea ice surface is likely to accelerate ice melting at much lower temperatures then currently?
4) ignoring the actual physics (as compared to climate science physics), does he realize that biological organisms actually live on the fresh water ice and might be adversely impacted by salty ice?

Bengt Abelsson
Reply to  Richard
May 3, 2017 10:48 am

Well, the good professor Desch knows how to make a chondrule. Not kidding.

Gary Pearse
Reply to  Richard
May 4, 2017 7:52 am

And seals’ holes in the ice would be filled in and polar bears would have nothing to eat. Plus as astute commenters point out, you’d be stupidly pumping salt enriched sea water on top of freshwater ice! I can’t but be disgusted that a PhD astronomer (what goes for a physicist these days! ) was graduated that thinks like this! He even has the smarmy hubris to offer HIS ‘engineering’ calculations of costs: 50,000 for each buoy all-in including delivery and installation to hold up a windmill in that environment and against the crushing and ridging of ice. A couple of million wouldn’t do it! Where TF are the engineers in his university? This should be a huge embarrassment to the university. This guy’s planetary work should be reviewed if he is this stupid.

Merovign
May 3, 2017 10:35 am

This reminds me of those low-budget early color sci-fi movies where they couldn’t tell the difference between a galaxy and a solar system, or a planet and a star.

May 3, 2017 10:40 am

Duh – out of time – every /dev/tty/null
replace by
/dev/null/tty
___________________________________________
all other contents OK

Ron Williams
May 3, 2017 10:42 am

Seriously? Spending $500 Billion on this may be premature if it turns out less polar sea ice is not the problem they say it will be. Or if ocean currents turn south and it gets cooler water at the north pole, the ice is just going to freeze up again and probably faster than it melted. Like all in one winter if it stays colder than melting the following 2-3 seasons and then we have multi year ice already.
If we had $500 Billion to spend on climate mitigation measures, I would spend it on asteroid/comet identification measures and deflection mitigation. That will be our greatest contribution humankind can offer, since one large bolide collision with earth will really make our day. (colder)

Marque2
May 3, 2017 10:53 am

Couldn’t this actually make the problem worse if implemented? The sea ice has a lower salinity than the surrounding water, and the water close to the bottom of the ice (if the hypothesis of how ice freezes stated above is correct) should be slightly more saline than the rest of the ocean. Pump this salty water on top of the sea ice and the greater salinity introduced could actually cause the ice to melt faster, because it will start melting at lower temperatures and then the run off would cause the natural ice to melt faster as well.
Also probably the quickest way to add ice would be to use ski slope snow makers.

Tom in Denver
May 3, 2017 11:12 am

“Suck up near-freezing water from under the ice and pump it directly onto the ice’s surface during the long polar winter.”
Actually this has been done for several decades. Ice Islands have been constructed in the Beaufort Sea for winter drilling. They simply pump seawater onto the ice until the ice finally rest on the bottom. Then they move a rig out and drill during the winter and move the rig off the ice before breakup.

philjourdan
May 3, 2017 11:22 am

And I thought this movie was just a comedy, not a prophecy:
https://youtu.be/Xm8vVNKrg9c

sam
May 3, 2017 11:22 am

Wouldn’t it be better to grab the 34 degree water from just below the ice and bring it up to an exposed heat exchanger and then return back at 32 degrees so it could freeze faster? Does he even know that icebergs and sea ice have no salt in them?

RACookPE1978
Editor
May 3, 2017 11:41 am

For those who are interested in the daily totals of direct solar radiation energy (theoretically) deposited on the southern edge of the Arctic sea ice over the course of a year, this table is provided.

Date 	DofY	    TOA      	Arctic 	 	         Daily Total	DREAD Index
                    Rad         Latitude      Sea Ice      Radiation  (Daily Radiation
                                at Edge        Albedo      on a Flat   Energy Absorbed
                                of Sea                       Surface    Difference)
                    W/m^2       Ice                         Watt-Hrs     Watt-Hrs
2-Jan	  2	    1408	   72.1	        0.830	           0	        0
12-Jan	 12	    1407	   71.8	        0.830	           0	        0
22-Jan	 22         1405	   71.5	        0.830	           0	        0
2-Feb	 33         1401	   71.2	        0.830	           0	        0
12-Feb	 43         1396	   71.0	        0.830	          15	        3
22-Feb	 53	    1390	   70.9	        0.830	         113 	       43
2-Mar	 61	    1385	   70.9	        0.830	         292	      144
12-Mar	 71	    1378	   70.9	        0.830	         651	      378
22-Mar	 81	    1371	   70.9	        0.830	        1146	      728
2-Apr	 92	    1362	   71.1	        0.830	        1813	     1223
12-Apr	102	    1355	   71.3	        0.830	        2493	     1741
22-Apr	112	    1347	   71.6	        0.823	        3207	     2272
2-May	122	    1340	   71.9	        0.824	        3919	     2825
12-May	132	    1334	   72.3	        0.818	        4595	     3310
22-May	142	    1328	   72.7	        0.796	        5201	     3637
2-Jun	153	    1323	   73.2	        0.749	        5740	     3742
12-Jun	163	    1320	   73.8	        0.689	        6053	     3580
22-Jun	173	    1317	   74.4	        0.620	        6151	     3212
2-Jul	183	    1316	   75.2	        0.553	        6012	     2725
12-Jul	193	    1317	   76.2	        0.498	        5630	     2218
22-Jul	203	    1318	   76.9	        0.466	        5028	     1783
2-Aug	214	    1321	   77.7	        0.464	        4159	     1415
12-Aug	224	    1325	   78.3	        0.499	        3261	     1171
22-Aug	234	    1330	   78.7	        0.566	        2368          957
2-Sep	245	    1337	   78.9	        0.666	        1497	      698
12-Sep	255	    1344	   78.9	        0.761	         864	      441
22-Sep	265	    1351	   78.5	        0.830	         414	      208
2-Oct	275	    1359	   78.0	        0.830	         146	       57
12-Oct	285	    1366	   77.3	        0.830	          28	        6
22-Oct	295	    1374	   76.5	        0.830	           1	        0
2-Nov	306	    1382	   75.6	        0.830	           0	        0
12-Nov	316	    1389	   74.8	        0.830	           0	        0
22-Nov	326	    1395	   74.1	        0.830	           0	        0
2-Dec	336	    1400	   73.4	        0.830	           0	        0
12-Dec	346	    1404	   73.0	        0.830	           0	        0
22-Dec	356	    1406	   72.6	        0.830	           0	        0
			                                       70797	    38517

Several columns are self-obvious.
TOA radiation levels are from Svalgaard;s latest SORCE data.
Arctic sea ice albedo is from Perovich and Judith Curry’s SHEBA ice station reports.
Latitude is calculated for the southern edge of the sea ice 3 times a month, using the 1979-1990 average sea ice area from Cryosphere, Univ of Illinois.
Direct radiation levels are calculated using a 0.75 atmosphere attentuation factor, based on the attenuation through the Kasten-Young Air Mass calculated for sun’s Solar Elevation Angle at each hour of the day, then totaled for the 24 hours.
The last column is the Daily Total of DIFFERENCE between the solar energy absorbed in water at each hour, minus the solar energy absorbed by the sea ice at that same hour of the day and day of year. (Sea ice albedo gets substantially darker through the year, so more energy is absorbed as the summer gets longer.)
[Corrected formatting. .mod]

mikewaite
May 3, 2017 11:42 am

Q:(from scruffy sceptic) Why do we need to do this ?
A: (from distinguished professor); To provide stable ice platforms so that Polar bears can catch seals after emerging from hibernation.
Q : How do they catch seals?
A: They wait for seals to come out on the ice and then ambush them
Q: How likely is it that a seal will approach an ice floe throbbing with wind turbines and sucking up gallons/sec of water and spraying it all around ?
A: We believe that they will just love it and of course the noise will mask the sound of the bear’s stealthy approach . Win all round really , well except for the seal , and the US taxpayer and the US Navy men and women who go out to do the maintenance on 50 million devices in the middle of winter in a howling gale.

Chimp
May 3, 2017 11:49 am

Arctic sea ice will “recover” all by itself. It has gone through many cycles much warmer than now.
This year’s unusually slow melt continues. Starting from a lower maximum, thanks to the El Nino, sea ice extent is now higher than at this time in 2015 and 2016.
http://nsidc.org/arcticseaicenews/charctic-interactive-sea-ice-graph/
Having slightly more open water this winter meant that more heat was lost from the Arctic Ocean and adjacent seas than normal. The cooler water is retarding the thaw.

hunter
Reply to  Chimp
May 4, 2017 9:12 am

Shhhhhh! Don’t confuse the climate consensus with thoughtful fact based analysis. All that matters is that the eeeevil conservatives are to blame for the apocalypse their profits have declared.

Joel Snider
May 3, 2017 12:20 pm

You’ve got to hand it to them – they never pass up an opportunity for exploitation, in order to further their agenda.
Windmills in the Arctic. Boy, I ‘d love to be the guy chopping the ice of those things in mid-February.

Jer0me
May 3, 2017 1:10 pm

As I said last time this insanity was dragged up, I have no problem at all with this.
As long as they try this with their own money, not mine.
And their own planet, not mine.

May 3, 2017 1:15 pm

Hey!
Here’s an idea. Why not ship all the sawdust from make making those wood pellets being shipped to the UK (?) and mix it in with the salt water being pumped to make Pycrete!
It takes longer to melt than regular ice.

Resourceguy
Reply to  Gunga Din
May 3, 2017 2:38 pm

Great idea. Just don’t do it with drama this time…..
https://en.wikipedia.org/wiki/Pykrete
“Another tale is that at the Quebec Conference of 1943 Mountbatten brought a block of pykrete along to demonstrate its potential to the entourage of admirals and generals who had come along with Winston Churchill and Franklin D. Roosevelt. Mountbatten entered the project meeting with two blocks and placed them on the ground. One was a normal ice block and the other was pykrete. He then drew his service pistol and shot at the first block. It shattered and splintered. Next, he fired at the pykrete to give an idea of the resistance of that kind of ice to projectiles. The bullet ricocheted off the block, grazing the trouser leg of Admiral Ernest King and ending up in the wall. According to Perutz’s own account, however, the incident of a ricochetting bullet hitting an Admiral actually happened much earlier in London and the gun was fired by someone on the project—not Mountbatten.[8]”

Griff
Reply to  Gunga Din
May 3, 2017 11:08 pm

They seriously considered building an aircraft carrier (or landing field) out of it in 1943!

Sommer
May 3, 2017 1:17 pm

Maybe they’re trying to figure out what to do with all of the industrial wind turbines in Ontario after they’re dismantled.

TA
May 3, 2017 2:20 pm

There will be numerous ice islands being propelled around the Arctic powered by their airborne propellers.

Steve R
May 3, 2017 4:23 pm

This is beyond stupid. It is 180 degrees opposite what the warmists claim to want!

Retired Kit P
May 3, 2017 9:31 pm

@Eugene
“Quite obviously you need an auxillary heating system to heat the water enough so that does not happen. ”
Actually that is what the utility thought. Saved them millions, used it as a bullet point on my resume. Showed them how to solve the problem for free. Somethings are easy on dry land and insane in the arctic.

Griff
May 3, 2017 11:07 pm

http://www.climatecentral.org/news/arctic-sea-ice-scraping-bottom-of-barrel-21418
Has a diagram showing how little multi year ice is left….
“Ice older than five years in age now only comprises 5 percent of the Arctic’s ice pack. It accounted for 30 percent of all Arctic sea ice in 1984, …..
Young ice has sprung up in its place and now accounts for nearly 70 percent of all Arctic ice, up from just 35 percent just three decades ago.”

Griff
Reply to  Griff
May 4, 2017 1:10 am

In fact that article has the 2016 diagram… situation in 2017 much worse: see comparison in
https://nsidc.org/arcticseaicenews/

May 4, 2017 5:48 am

Stranne et al., 2013 demonstrated that the modern day Arctic sea ice extent is more comparable to that of the last Pleistocene glacial stage than to that of the Holocene Climatic Optimum (9,000-5,000 years before present).
This model referred to in the OP shows a mean ice thickness for the present about 3m whereas measurements give somewhere between 1-1.5 m, comparable with the Holocene Climate Optimum values they show. Their calculations were based on the preindustrial conditions not present-day.

Butch
May 4, 2017 6:50 am

How often does the temperature get above freezing in the Arctic ?? I thought they melted from below…

RACookPE1978
Editor
Reply to  Butch
May 4, 2017 7:15 am

Butch

How often does the temperature get above freezing in the Arctic ?? I thought they melted from below…

It’s a good question, and the answers in the actual papers describing the two circumstances are themselves somewhat confusing. Best general rule is: Arctic sea ice melts from the top down (stagnant, shallow melt water ponds on the top of the floating sea ice, with air temperatures just above freezing at 3-4 degrees C during the short summer weeks. Below, the sea water is “not freezing” (not accumulating) rather than “actively and rapidly melting” with water temperatures between 2 and 4 deg C. Antarctic sea ice is above much water waters (4-5 deg C) and those waters are more active (circulating and flowing faster underneath each year’s sea ice). Around the Antarctic, almost all of the sea ice refreezes each year (very little is second and third year “fast ice” near the shores) and 100% of the sea ice far from the shores is first year ice.
The Antarctic sea ice melts from below, there are almost no stagnant melt water ponds on top of the sea ice, and so fresh snow accumulates on top very often through the whole year. As a result, the Antarctic sea ice has a higher albedo (cleaner, fresh snow instead of dirty polluted snow and dust and melt ponds) over the entire year. 0.83 on average, only going down slightly to 0.75 in December – January – Feb.

Butch
Reply to  RACookPE1978
May 4, 2017 7:19 am

..Thanks…I think …

Griff
Reply to  RACookPE1978
May 4, 2017 10:31 am

Bottom melting from warm ocean water is also a factor (increasingly so)
http://adsabs.harvard.edu/abs/2016EGUGA..18..268M

Reply to  RACookPE1978
May 9, 2017 7:38 am

RACookPE1978 May 4, 2017 at 7:15 am
The Antarctic sea ice melts from below, there are almost no stagnant melt water ponds on top of the sea ice, and so fresh snow accumulates on top very often through the whole year.

Also according to NSIDC:
“Antarctic sea ice tends to be covered by thicker snow, which may accumulate to the point that the weight of snow pushes the ice below sea level, causing the snow to become flooded by salty ocean waters.”