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Looking at Greenland mass balance on http://nsidc.org/greenland-today/ in late October, it is clear that GrIS is suffering significant melt event in periods where there is limited direct sun light on the ice. Thus, the melt is the result of atmospheric water vapor transport. (1 gr water vapor can melt 7 gr ice resulting in 8 gr runoff). Thus, we can deduce that atmospheric water vapor transport has become a major source of heat for GrIS melt. We can also deduce that atmospheric water vapor transport has become a major source of heat for sea ice melt, regardless of conditions of direct sun light.
I proposed this situation some 15 years ago and had the then-current model Arctic Energy Budget explained to me - repeatedly.
Aaron Lewis
aka "Agres"
PIOMAS October 2017
To make up for this somewhat belated PIOMAS update (below), I have for you Andy Lee Robinson's latest update of his Volume ice cube 3D video: ----- Another month has passed and so here is the updated Arctic sea ice volume graph as calculated by the Pan-Arctic Ice Ocean Modeling and Assimilation...
I suggest that with all the heat from the last big El Nino wandering around, trapped by 409 ppm, that heat collected by tropical oceans will end eating the Arctic Ice this summer. (1 gr of water vapor can melt 7 gr of ice. TPW in the Arctic has gone from near 0 to 7 kg/m^2 in the last 20 years.)
Moreover, I suggest the 5-year cycle is very closely related to the 5-year minor El Nino cycle offset by a lag for travel time. The more GHG in the atmosphere, the more strongly Arctic sea ice and El Nino are linked.
And, I think we owe a huge debt of honor to Professor Wieslaw Maslowski for his bold prediction of Arctic Sea Ice loss.
PIOMAS May 2017
Another month has passed and so here is the updated Arctic sea ice volume graph as calculated by the Pan-Arctic Ice Ocean Modeling and Assimilation System (PIOMAS) at the Polar Science Center: It's no surprise 2017 is still lowest on record, according to the PIOMAS model. If during the last we...
Has everyone seen: https://www.climate.gov/news-features/blogs/enso/your-eight-minute-speed-date-pacific-meridional-mode ?
I think the increasing PMM and AMM are the result of convection resulting from a warmer and moister Arctic atmosphere.
Global sea ice records broken (again)
Sabbatical or not, records must be reported (like I did last year, here and here, albeit a month later). According to NSIDC data, the Global sea ice area record for lowest minimum has just been broken, as shown on this Wipneus graph (world famous now because of what happened after September last...
On the other hand, OPEC knows that AGW will wipe out the oil market before they can pump and sell all of their oil. Thus, they intend to sell as much of their oil as possible, as fast as possible, and are willing to lower their profit margin.
The Arctic Oil will always be more expensive than Middle-Eastern Oil.
OPEC is very likely to keep oil prices low enough that Shell cannot sell that Arctic Oil at a profit. Developing Arctic Oil is a waste of Shell Oil's shareholder's capital.
In addition, climate is changing so fast in the Arctic that there is no way to develop a basis for engineering design. Engineered structures will either be horrendously expensive or will collapse in the first weather that comes in outside of basis of design. e.g., http://www.nrdc.org/energy/shell-arctic-drilling.asp
For example, all the sea ice is moving much faster than ever before. Not many engineered structures can withstand the impact of 1 meter thick ice flows moving at speed that arctic sea ice can move these days. Nor is that sea ice solid enough and stable enough to put drilling equipment on. Nor can they use permafrost to support staging facilities as was done in the 1960s and 70s when the geological studies were done and the Alaskan pipeline built.
Shell will not be able to pump Arctic Oil at competitive prices - even in an "ice free" Arctic. I would bet that they wreck 2 more drill rigs and call it done!
Bill McKibben nails it
This simply has to be shared, as Bill McKibben expresses my thoughts exactly. This sentence just about says it all: "It’s as if the tobacco companies were applying for permission to put cigarette machines in cancer wards. And the White House gave Shell the license." I haven't seen such a good m...
Looking at pictures of the Norwegian Expedition, there seems to be a lot of loose snow on the ice. This may have fooled the PIOMAS sensors/model.
PIOMAS May 2015
Another month has passed and so here is the updated Arctic sea ice volume graph as calculated by the Pan-Arctic Ice Ocean Modeling and Assimilation System (PIOMAS) at the Polar Science Center: According to the PIOMAS model Arctic sea ice volume reached its maximum in the past month (always a b...
Timely story.
However, Britain and Europe already seeing extra rain as North Atlantic warms, to say nothing of Pakistan, Nepal, and the snow fields above the Himalayan glaciers. Already flood repair is draining infrastructure budgets.
Water vapor contains more energy than rain and (unseen) water vapor condensing on the surface can melt a glacier faster than rain. (condensing wv can produce wind, see http://www.atmos-chem-phys.net/13/1039/2013/acp-13-1039-2013.html) 1 gram of water vapor can melt 7.5 grams of ice, resulting in 8.5 g of runoff.
Floods sure, but do not forget the hail. Warm moist air hitting cool moist air can generate tremendous thunderstorms. We are already seeing hail storms that destroy cars and houses. Hail is also very hard on crops.
Everything is connected. Today everything has microprocessors in it. Every microprocessor is embedded in a drop of "gray plastic" made at one of about 300 chemical plants - most of which are at sea level. They can be "jacked up" as sea level rises, but the high pressure pipe that is needed as they are reconfigured, is made at the Shaw plant outside of Houston, Tx. It does not take much to flood Houston.
Currently, organic matter sinks to to bottom of the ocean, and is converted to methane, but the bottom of the ocean is cold enough that the methane freezes into clathrates that just sit in the sea floor. If the bottom of the ocean warms a tiny bit, organic material from iron fertilized blooms will fall to the bottom, be converted to methane, and -- how much methane makes it back to the surface is a very interesting question. Methanogenesis has been shown to occur at low pH's (pH=3.0).
Today, we can dig and transport lime for agriculture because the mining and transport is subsidized by cheap oil - including the production of cheap gray plastic for mine machinery and truck parts. In the absence of cheap oil and good transportation (e.g., flooded roads and rail lines) lime is expensive. And, rye is a long day plant, it does not do well in the short days of winter. In fact, crop production remains difficult as long as the climate continues to change. Crop production needs predictable seasons.
Even after we stop emitting carbon there will be several decades of residual warming in the system - even if we are actively sequestering carbon. This ongoing climate change will affect crop production.
If all this sounds pessimistic, I read the Greek classics and they seem to have had very civilized life without any fossil fuel.
The day the ice cap died
The title of this blog post is actually the title of a piece of science fiction, a short story written by Paul Briggs. Just like a couple of weeks ago when I was asked for advice on an idea for a novel, Paul asked me for some feedback on his short story. I figured posting it here, will generate...
The climate was stable during Roman times and past ice would predict future ice. Then we had LIA and MWP. Now we have AGW. Each year we have measurably more heat in the system, and the system collecting heat faster. It is a heat engine with the throttle pushed a little bit forward each year.
Each year the engine runs a little differently as a result of the increased energy in the system. Since the energy of the system changes each year, past system behavior does not predict future system behavior. Since this is the first time we have observed the climate system under these conditions of changing heat levels, we cannot be certain how the system will respond. In particular, we are ignorant of system lags and feedbacks. At this point we know the system is going to a state with less ice than humans have ever seen before, and it is going there faster then we have ever seen climate change.
I remain convinced that the Arctic ice will retreat in a series of abrupt ice loss events, and that each successive event will produce gasps of surprise from the assembled observers.
2013/2014 Winter Analysis
With another interesting freezing season behind us, it's time to compare to previous winters and get an idea of this melting season's foundation. As we have seen in the last two years, the start of the melting season plays an important role, and so it might very well be that the end of the freez...
As we lose albedo, either from lose of sea ice or loss of snow cover, we also lose a condensing surface for water vapor from the atmosphere.
Thus, loss of albedo implies more water vapor in the atmosphere or a longer residence time for water vapor in the atmosphere.
Most of the climate models do not address this but when we express water vapor as ppmv as we do CO2, it is easier to visualize that water vapor is a major factor, and an extra day's residence time in atmosphere results in a significant increase in atmospheric water vapor.
Loss of albedo has at least 2 significant feedback effects, and we should consider both.
PIOMAS April 2014
Another month has passed and so here is the updated Arctic sea ice volume graph as calculated by the Pan-Arctic Ice Ocean Modeling and Assimilation System (PIOMAS) at the Polar Science Center: Last month's tentative conclusion has definitely been confirmed for now: It seems that last year's r...
Perhaps, Nevin will allow me to re-phrase his statement to "Look at the change in ALBEDO!".
Mission possible
The melting season has just about started (no, I'm not calling the max), but already scientists are out there in different parts of the Arctic doing their thing. Currently there are two eye-catching missions being carried out, both having to do with measuring ice thickness to validate satellite...
Note that many of the Greenland fjords, Umiivik and south, show open water.
Bromine, chlorine and mercury
After this 2012 blog post on Arctic pollution, it's time to return to the subject, if only because Arctic sea ice is proving to be a significant factor in changes in atmospheric chemistry, leading to increases in mercury concentrations in the Arctic. This happens through sea ice melting during s...
I like data expressed as standard deviations.
How could Arctic data be more friendly?
How might Arctic data, such as the iconic datasets followed so closely on this blog, be made easier to access and use? In connection with a new project called the Sea Ice Prediction Network (SIPN), I’d like to collect your suggestions and pass them along to Arctic researchers. Arctic Sea Ice blo...
My take on the situation is that heat that I expected to end up driving melt of the ASI went to warming the North Pacific, melting permafrost,and maybe warming Antarctica? Ultimately, I am not as interested in ice compaction as I am in storm mixing of surface fresh water with deeper salt water.
This is the first time we have actually had a chance to watch an AGW event, so I do not feel too bad about missing some of the couplings.
Today, there is more heat in the system than there was 6 months ago, so at some point, the sea ice will melt, and with more heat in the system, it will melt faster, and everyone will be more surprised at how fast
it does melt out. As long as the North Pacific is gaining heat, and supplying latent heat to Northern Canada, I do not see any chance of real ASI recovery.
Pinpointing the minimum
UPDATE September 16th: Given another uptick and the current weather forecast, I'm ready to call the minimum for IJIS SIE V1 on September 12th at 5,000,313 km2. Apparently the high was too big and the pressure gradient too low to prolong things (see below). --- This blog post should perhaps ha...
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