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 rebound has been fully negated after a couple of relatively warm months (the flipside of cold outbreaks in the US) and 2014 will start out at approximately the same level as previous years.
After the last minimum ended up being 1700 km3 above that of record year 2012, the current modeled volume for March 31st is 241 km3 below last year's. The difference with 2011 was +401 km3 at the end of February, and has even increased to +480 km3. Other than that volume is now lower than all the other years in the record. Who would've thought this back in September? Well, the Arctic does as the Arctic will.
The graph produced by Wipneus shows a bit more clearly how 2014 is just below the other trend lines, with 2011 some further below:
With CT sea ice area numbers also being relatively low during March, average thickness (crudely calculated by dividing PIOMAS (PI) volume numbers with Cryosphere Today (CT)) hasn't gone lowest, although the 2014 trend line moved away from 2010 during the first two weeks of March, and joined the other low years.
Here's average thickness for March 31st in metres, with change from last month between brackets:
- 2005: 1.98 (+0.19)
- 2006: 1.92 (+0.11)
- 2007: 1.87 (+0.21)
- 2008: 1.84 (+0.17)
- 2009: 1.84 (+0.18)
- 2010: 1.76 (+0.12)
- 2011: 1.70 (+0.11)
- 2012: 1.68 (+0.11)
- 2013: 1.69 (+0.17)
- 2014: 1.73 (+0.13)
If you want to have a look at the data yourself, you can download the spreadsheet I use and update from GoogleDrive.
The Polar Science Center thickness graph looks slightly different, with 2014 jutting out above the other post-2010 years:
So, again, the recovery in volume seems to have disappeared due to a warm winter. A priori this would imply that the 2014 melting season could go every which way, as 'high' as 2013, or as low as 2012, depending on weather and distribution of volume across the ice pack.
This is something I will discuss in the 2013/2014 analysis that will be posted later this month. Just a few more weeks for volume to reach its maximum, even though the melting season has already started area/extent-wise. In the meantime I recommend reading this recent PIOMAS-related blog post by Chris Reynolds: What caused the volume loss in PIOMAS
It's all back to zero now. Could've been better, but could've been worse as well.
Early snowmelt in Siberia and much warmer temperatures on the Siberian side of the Arctic combined with southerly winds have thinned the Siberian Arctic ice. However, the Canadian Arctic has been cold and ice has compacted to the thickest levels in years there. Some of this thick ice is now beginning to be pushed down the coast of Greenland.
Could this be the beginning of a dipole pattern with strong ice export from the Arctic? We'll see.
Early warming in Siberia will tend to continue, once started, because heat will continue to build up in dark snow free areas. And there are also likely to be the warming affects of the developing El Nino. I don't expect to see the ice stick around on the Siberian side as long as it did last summer.
Posted by: D | April 08, 2014 at 04:02
Thank you for another great, and anticipated, update Neven!
While I would not agree that "last year's rebound has been fully negated after a couple of relatively warm months", there is certainly not much left, and we are basically back to relying on weather - which in any case is still the most prominent factor in determining summer minimum ice area and volume.
The two positive points:
- We have significantly more second year and MYI than a year ago
- For main melting areas in April and May (Barents, St. Lawrence, Bering, and Okhotsk), we had last year about 300km3 more ice than this year (assuming average thickness of .75M and using CT area numbers)
The negative points:
- Baffin has about 300km3 more ice this year compared to last year, which will melt out nearly completely in June/July, but will the increased ice cause any protection from ice discarting from the Hudson Bay and nearby strait?
- I don't like the compaction of ice east of Severnaya Zemlya, as this opens up the possibility of open water earlier in the summer than last year - prefer any ice cover compared to open water in main summer months.
To speak of the weather, it does seem the Arctic pressure area is disconnecting itself from the Siberian weather
http://ocean.dmi.dk/arctic/weather/arcticweather.uk.php
(as the snow is melting fast over there), which I think is a good thing, exactly as we saw last year, and it may - if all goes well - help to insulate high and low areas over the Arctic from adjacent continental pressure areas.
Amazing spectacle!
Posted by: John Christensen | April 08, 2014 at 09:57
D said:
"Early snowmelt in Siberia and much warmer temperatures on the Siberian side of the Arctic combined with southerly winds have thinned the Siberian Arctic ice."
The ice has not thinned due to warmer temperatures or melting, as it seems you are suggesting. The ice has been moved north due to prevailing offshore winds in Laptev over the past weeks, as you see here:
http://www7320.nrlssc.navy.mil/hycomARC/navo/arcticictn_nowcast_anim30d.gif
If that pattern had persisted I would agree that more ice would go out via Fram, but luckily (if it holds) it seems the weather has now changed to a weak central Arctic high, which causes westerly winds in the Fram Strait, hopefully slowing down ice export:
http://ocean.dmi.dk/arctic/weather/arcticweather.uk.php
Both HYCOM and the DMI weather chart seem to support some strengthening of the ice west of Severnaya Zemlya in the coming week, but it is very late in the season for ice build-up..
Posted by: John Christensen | April 08, 2014 at 11:16
Here's a MODIS image of the "thin ice" offshore in the Laptev Sea:
Some more can be seen on the forum.
Posted by: econnexus | April 08, 2014 at 12:19
Hi Jim,
I see from the Forum that you are suggesting this ice is "falling apart" and not refreezing, is that correct?
Since it is -15 - -20C in this corner of the Laptev Sea (from the DMI 60N weather chart) would you agree that the open water is caused by the pack compacting towards the North, or are you suggesting this temperature is too high for refreeze, or the data is incorrect on DMI?
Posted by: John Christensen | April 08, 2014 at 13:17
John - I agree the pack is compacting towards the North, leaving a fair few isolated floes and some open water behind. By definition open water is above the freezing point of water! If you compare the various images you will note some refreezing has taken place over the last day or two.
However according to the CCI's visualisation of the GFS forecast 2m air temperatures above freezing are due to arrive on the Laptev coast in the not too distant future: http://cci-reanalyzer.org/Forecasts/index_gfcst.php
Posted by: econnexus | April 08, 2014 at 13:30
Offshore winds have pushed Siberian ice towards the Canadian side of the Arctic. The air along the Siberian shores of the Arctic ocean has been much warmer than normal but below 0 C. Thus, new ice has formed but it's much thinner than normal for this time of year in the Laptev and Kara seas. This ice will melt out quickly this year because it's very thin and Siberia will continue to warm up ahead of climatology. Is that clear now?
FWIW, I don't comment much here but I follow this blog and the Arctic very closely. I appreciate the constructive nature of the comments here. I post as FishOutofWater at Dailykos and my first name in real life is George. Typepad accidentally gave me the login name of D when I tried to login here once, but I use the name D nowhere else on the internet or in real life.
Siberian snow cover is one of the key factors in cold winters and warm summers. When snow begins early in September the cooling effects of the high albedo tend to continue through the fall leading to a cold winter in Eurasia. Early spring snow melting is apparently one of the key factors that leads to a build up of heat over Siberia that precedes a hot summer. Thus, the early retreat of Siberian snow that has already started this year http://climate.rutgers.edu/snowcover/index.php is a key factor that will likely lead to early melting of sea ice on the Siberian side of the Arctic.
Posted by: D | April 08, 2014 at 15:31
Thanks for your comments George and agreed on the ice notions.
Regarding the impact of early snow melt in Siberia, it will be very interesting to see if this will lead to early melting of ice on the Siberian side of the Arctic, or if the opposite will happen, namely that the temperature difference between ice-covered AO and heated surrounding continents will create a repeat of last year..
Posted by: John Christensen | April 08, 2014 at 16:59
I am refering to this excellent blog entry by Neven last year:
http://neven1.typepad.com/blog/2013/06/on-persistent-cyclones.html
And a key abstract from that entry:
The Summer Cyclone Maximum over the Central Arctic Ocean
Mark C. Serreze and Andrew P. Barrett, 2008, Journal of Climate
From the abstract:
A fascinating feature of the northern high-latitude circulation is a prominent summer maximum in cyclone activity over the Arctic Ocean, centered near the North Pole in the long-term mean. This pattern is associated with the influx of lows generated over the Eurasian continent and cyclogenesis over the Arctic Ocean itself. Its seasonal onset is linked to the following: an eastward shift in the Urals trough, migration of the 500-hPa vortex core to near the pole, and development of a separate region of high-latitude baroclinicity. The latter two features are consistent with differential atmospheric heating between the Arctic Ocean and snow-free land.
Posted by: John Christensen | April 08, 2014 at 17:03
Greater ice thickness over the larger Canadian Archipelago area has already affected CAA weather to be mainly anticyclonic for more than a month. So 2013 lack of compaction of sea ice is highly unlikely. The NW passage will open late under a cloudier cover if El-Nino becomes strong. However it is strangely already here to some degree, consider the near entire North Pacific anomalously warm effectively being like an El-Nino for the Northern Hemisphere, the sea ice will melt quicker from the extra heat, thicker sea ice anticyclonic period will be lasting a while further, surrounded by cyclones in the open water regions bordering land without snow.
Posted by: wayne | April 08, 2014 at 18:44
The warmer temperatures are absolutely key in retarding ice growth, but in themselves will contribute very little to the coming melt. As Neven indicated, the coming weather will now be the key factor, and with it, how much heat arrives directly, via insolation, or indirectly, via rain and fresh water outflow. Without sun, the transfer of heat to ice from air is not sufficient to permit rapid phase change.
Posted by: jdallen_wa | April 08, 2014 at 20:11
The data from Rutgers Uni shows NH snow cover now tracking 2012, the record year for early snow melt. It's early days mind. (The graph here (usually 2 clicks to "download your attachment) shows the 2014 anomaly against previous decadal & the 2010-3 averages).
UAH should update for March soon so we'll know whether the Arctic's Lower Troposphere record temperatures remain or have dropped down a little.
Posted by: Al Rodger | April 08, 2014 at 21:26
The link that hopefully now works.
Posted by: Al Rodger | April 08, 2014 at 21:27
@Neven
In Google Drive doc (PICT-CAPIE) you have an error: you "lost one day" of data CT area. 10 march: 13 007 717 km2, no 13 052 584 km2 http://arctic.atmos.uiuc.edu/cryosphere/arctic.sea.ice.interactive.html
http://arctic.atmos.uiuc.edu/cryosphere/timeseries.anom
Data CT:
12 887 309 - 9.03
13 007 717 - 10.03
13 052 584 - 11.03
13 159 343 - 12.03...
.... 13 041 841 - 6.03 last data, 96-th day.
Posted by: Hubert Bułgajewski | April 08, 2014 at 21:56
George, FOOW, what you wrote 15:31 made perfect sense to me.
Remember the AWI-map on ice thickness in the Laptev March 2012?
It would be nice to have a corresponding recent map. But this situation was a result of winter ’11-’12, which produced a mean temp anomaly of just under +3 dC in that region.
Last year the anomaly stuck around zero over there. But this winter, it is close to ’11-’12 again, just about +2 dC. If my musings on ‘winterpower’ have any relevance at all, it should be no wonder to see a rapid breakdown in the Laptev.
Oh, the red was >+50cm thickness.
Posted by: Werther | April 08, 2014 at 22:06
Werther - At a somewhat coarser resolution, here's Wipneus' homebrew SMOS map for March 31st:
Posted by: econnexus | April 08, 2014 at 22:20
Werther, I would very much like to see a map like that for this March. Last year was strongly affected by the sudden stratospheric warming in January. Strong subsidence over the N pole followed that warming into mid-spring. Then the very weak jet stream re-consolidated around the Arctic ocean leading to the month of Arctic storms from late May to late June. This year a SSW started but didn't quite make it and the jet stream has held together better.
This year's set up going into the melt season looks a lot like 2012, in my opinion, except for the likely El Nino. BoM.gov.au has the probability of El Nino at 70% in the latest ENSO outlook posted today.
The Beaufort sea is the one area with much thicker ice this year than in 2012. Perhaps that thick ice will help strengthen the Beaufort high, by reflective cooling, in the coming months.
Posted by: D | April 08, 2014 at 22:23
Regional breakdowns of PIOMAS gridded data and thickness distributions for Beaufort/ESS/Central here:
http://dosbat.blogspot.co.uk/2014/04/piomas-march-2014.html
Posted by: Chris Reynolds | April 08, 2014 at 22:27
Well Jim, that pic shows that, if AWI would fly the area with their 'e-bird' again, it would reveal almost the same map as in March '12.
Not surprising, the temp record on Ostrov Kotelnyj and in Tiksi also hint on less 'winterpower'. While all winter was a tad less cold than last year, the 'heatwave' during March was remarkable. Even noticeable on remote Kotelnyj.
Posted by: Werther | April 08, 2014 at 22:28
Wipneus, thanks for updating your graph, I've added it to the blog post now.
Hubert, thanks a lot for catching that error, AND for telling me exactly where it is. I try to dutifully enter new data points in my spreadsheet every day, but failing to do so even once means a lot of intent searching, especially with CT and its unhandy numbering (for muddlers like me).
Posted by: Neven | April 08, 2014 at 22:47
Years of Living Dangerously Premiere Full Episode.
https://www.youtube.com/watch?v=brvhCnYvxQQ
Posted by: Colorado Bob | April 09, 2014 at 01:34
It's worst then we all feared.
Posted by: Colorado Bob | April 09, 2014 at 04:25
D/George,
Beaufort Sea ice may appear thicker, however it is highly fractured, which may facilitate warming and melt later in the summer, depending on the weather.
The fracturing pattern after the last few days makes much of it appear like a giant smoothie.
Posted by: Apocalypse4Real | April 09, 2014 at 04:36
Thanks to Chris for a great regional PIOMAS update!
One item I noticed in particular is the considerable difference between your gridded view of ice thickness compared to HYCOM: 'Your' view has a lot more ice in the Central AO, while HYCOM is showing a significant branch of thicker ice in the Beaufort and Chuckchi Seas. I hope you have it more accurately placed than HYCOM, as the lower latitudes showing on HYCOM does not bode well for summer melting rates (depending on your view point).
And your statement: "I don't expect 2014 to beat 2012, but I do expect a more exciting year than 2013". What is this? ;-)
I found 2013 extremely exciting like the thriller where the hero is up against impossible odds, but starts out amazingly well, then almost succombs, and finally makes it through with few casualties.
I always favored the underdog..
Posted by: John Christensen | April 09, 2014 at 10:04
It's a bit cloudy over the Laptev Sea this morning, but here's the view from Terra:
More on PIOMAS and Siberian snow at:
http://GreatWhiteCon.info/2014/04/the-arctic-sea-ice-recovery-vanishes-even-more/
Posted by: econnexus | April 09, 2014 at 11:41
John - The Navy's ACNFS seems to capture the extent of the multi-year ice in the Beaufort/Chukchi better than PIOMAS. See for example this IJIS RGB image:
However I remain to be convinced that ice is as thick as CICE claims.
Posted by: econnexus | April 09, 2014 at 11:54
Thank you for sharing Jim, and I agree that this view does seem to be overstating the MYI, while being in better agreement with HYCOM on structure.
Posted by: John Christensen | April 09, 2014 at 12:25
John,
PIOMAS doesn't explicitly model FYI and MYI, and doesn't seem to be picking up the MYI being shown as being exported into Beaufort and Chukchi by the Drift Age Model (DAM). This may however be because the MYI isn't that thick, so it might not prove the impediment to melt I have said I expect.
HYCOM is showing the MYI export shown in the DAM, but it's showing seriously thick ice there. Comparison with IceBridge would be best, but at present I'm not convinced by this thick ice shown in HYCOM. I think for the grid cell average thickness is not at 3.5m to 4m thick in Beaufort, I think PIOMAS is more likely to be on the nail. But...
HYCOM is intended for shipping isn't it? So do those running it intend it to be high biassed in terms of thickness to stop ice breakers running into 'briar patches' of ice too thick for them to handle. Just a WAG.
It is hard to get where people are coming from with 'good melt' and 'bad melt'. I've said before I don't get why some follow a system in a death spiral and keep rooting for ice survival.
2013 was an interesting experiment, the experiment is over and the volume pulse lasted a lot shorter than I'd dreamt possible - the ice keeps proving me wrong. But I still find big awe-inspiring crashes more exciting. :)
Jim,
Check out ASCAT too.
http://manati.star.nesdis.noaa.gov/ascat_images/ice_image/msfa-NHe-a-2014098.sir.gif
The spur of whiter MYI is visible in Beaufort, but there are cracks in it and it's got nowhere near the brightness (high radar return) as the band off the CAA. That suggests it's dispersed - given that it came from the mass of white off the CAA its dielectric properties shouldn't have changed.
More images here:
http://manati.star.nesdis.noaa.gov/ascat_images/ice_image/
Posted by: Chris Reynolds | April 09, 2014 at 18:54
Al Roger, per your comment yesterday, UAH has indeed updated:
http://vortex.nsstc.uah.edu/data/msu/t2lt/uahncdc_lt_5.6.txt
.17, basically unchanged from last month (though that global mean figure is masking a switch from oceans being relatively warmer than land to a more equal distribution of the anomaly.)
Posted by: Kevin McKinney | April 09, 2014 at 19:14
Hi Kevin,
Yes. He has put his latest Global figure up here. But the page you link to with all the sea/land figures for different latitudes (ie the Arctic) is still only showing to February. It usually is updated quite promptly.
Nomad3 is updated for March with SST showing record warmth above 65deg & 80 deg. But it seems to me that ice is more affected by TLT figures.
Posted by: Al Rodger | April 09, 2014 at 19:59
Al,
D'oh!
Curious…
Posted by: Kevin McKinney | April 09, 2014 at 23:13
Sorry Neven, for deviating from the topic here - I will make this just one comment.
Hi Chris,
You stated " I've said before I don't get why some follow a system in a death spiral and keep rooting for ice survival."
My counter-argument is that it's not about the Arctic Sea Ice, but about the global eco-system that we have adapted to.
Consciousness about global warming and sea ice is not global; people in Syria, Haiti, Central Africa, Africa's Horn, and many other places have accute challenges of poverty, disease, and threats to their lives, which makes global warming a remote intangible concept of low priority.
I don't believe any population will remain in their huts, houses or caves made of dirt or straw at the risk of malnutrition, disease and exploitation from stronger powers in their area. They will eventually be educated and will want basic levels of social and economic freedom and stability.
It took the Western world about 200 years to reach a point where we start seeing energy consumption levels go down in some countries, as well as increase in transition to renewable energy sources. See example of Denmark:
http://www.ens.dk/sites/ens.dk/files/info/tal-kort/statistik-noegletal/aarlig-energistatistik/graphs_2012.ppt
It will take another 100-150 years to get the rest of the world to this point (probably quite optimistic), and this would even require many of the remaining countries to leap frog from subsistence farming to a modern society based on economic exchanges.
So yes, I am rooting for the ice, not to be naive about what is happening in front of us, but because I do not see how the entire world can transition to a different mode of energy consumption within years or a few decades given the social and economic situation of nearly a billion people:
From Worldhunger:
http://www.worldhunger.org/articles/Learn/world%20hunger%20facts%202002.htm#Number_of_hungry_people_in_the_world
The United Nations Food and Agriculture Organization estimates that nearly 870 million people of the 7.1 billion people in the world, or one in eight, were suffering from chronic undernourishment in 2010-2012. Almost all the hungry people, 852 million, live in developing countries, representing 15 percent of the population of developing counties. There are 16 million people undernourished in developed countries (FAO 2012).
The number of undernourished people decreased nearly 30 percent in Asia and the Pacific, from 739 million to 563 million, largely due to socio-economic progress in many countries in the region. The prevalence of undernourishment in the region decreased from 23.7 percent to 13.9 percent.
Latin America and the Caribbean also made progress, falling from 65 million hungry in 1990-1992 to 49 million in 2010-2012, while the prevalence of undernourishment dipped from 14.6 percent to 8.3 percent. But the rate of progress has slowed recently.
The number of hungry grew in Africa over the period, from 175 million to 239 million, with nearly 20 million added in the last few years. Nearly one in four are hungry. And in sub-Saharan Africa, the modest progress achieved in recent years up to 2007 was reversed, with hunger rising 2 percent per year since then.
Posted by: John Christensen | April 10, 2014 at 10:44
Link to the DMI ice drift map, which clearly shows the continued northernly flow in Laptev:
http://ocean.dmi.dk/arctic/icedrift_anim/index.uk.php
This would be a significant difference from the setup a year ago, where the ice was stable here, while quite similar to the situation two years ago leading to unprecedented ice melt during summer months.
The early opening of the waters in Laptev should have a negative impact on the ice both due to early access of sun radiation to the water surface as well as reducing chances of creating the cyclonic environment we witnessed last year.
Posted by: John Christensen | April 10, 2014 at 14:08
The feed from Aqua seems to be down today. Here's a lurid red (and still rather cloudy) view of the Laptev coast today, courtesy of Terra via Worldview:
Temperatures in Tiksi have now reached +1, and the winds are still from the SSW.
Posted by: econnexus | April 10, 2014 at 15:16
John,
I couldn't put it better than Nick Cohen.
http://www.theguardian.com/commentisfree/2014/mar/22/climate-change-deniers-have-won-global-warming
And to paraphrase Slartibartfast:
"Perhaps I'm old and tired, but I think that the chances of 'getting people to act on AGW' are so absurdly remote that the only thing to do is to say, "Hang the sense of it," and keep yourself busy."
Unlike Slartibartfast, I am happy. I'd rather be right than happy, but it's good that the two states are not mutually exclusive :)
Posted by: Chris Reynolds | April 10, 2014 at 19:28
Chris, that's a good piece in many respects. However, despair is not adaptive.
I will never, never give up--and I, too, am happy.
Posted by: Kevin McKinney | April 10, 2014 at 19:39
It's not despair Kevin, it's pragmatism. And no, don't give up, I rarely voice this opinion because I don't want to get in the way of those trying to work for change. So I just keep my doubts to myself, most of the time.
Posted by: Chris Reynolds | April 10, 2014 at 21:36
Nine months ago Rob Painting posted on Skeptical Science about ocean heat coming back to haunt us.
He couldn’t have foreseen the timing, which seems to be right now. But after about 15 years in a dominant negative mode, PDO did change face. Soon the March index will show whether the trend parallels the one from the beginning of 1997.
The re-emergence of El Nino will reveal consequences of fifteen years of inaction on mitigation, a period by some ludicrously seen as a ‘stop’ of global warming.
As Painting made clear in his SkS post, during the recent -PDO years, the ocean has been storing the ‘unbalanced’ heat in its deeper layers. Since the last moderate ENSO-event ’09-’10 the troposphere has progressively become disturbed.
This coincides with strengthened forcing through greenhouse gases and gradual cease of the ‘rubber-band effect’ that lags/delays the climatic response. The diminishing temperature difference between the Poles and the Tropics could be traced in height gain on the 500hPa level over the Arctic.
This not only had an effect, as described by FI Dr. Francis, on the behaviour of the Polar Jet stream. Other influences could be identified FI in the constant SSW attacks on the Polar Vortex past winter. ‘Loaded', slow moving Rossby waves through the mid troposphere, a West Pacific warm pool spawning monster cyclones like Haiyan. All these signs preluded the powerful Kelvin Wave now propagating through the Pacific.
The coupled ocean-atmosphere system is out of balance and leads to more weather anomalies. That will also mark the ENSO-event that is now in progress. As I supposed last year on the character of the ’13 sea ice melt season: ‘action could well shift to the mid-latitudes’.
Now it gets to the Tropics.
What do I expect? A fascinating, though frightening series of events related to El Nino, an extended Arctic melt season, normal in the sense that it might not lead to a new minimum in SIE/SIA and volume this year.
Above all, a year that may violently surpass the ‘weird’ weather years experienced since 2010. With consequences that may present ’15 as a new record setting melt year for the Arctic sea ice and the Greenland Icesheet.
I find not much solace in climate predictions based on historical data and known processes.
The 'old' rules are progressively becoming irrelevant. The comfortable discussions on climate sensitivity will be challenged by reality.
Paintings’ stored heat is coming to haunt us, sooner and stronger than may have been foreseen.
Posted by: Werther | April 10, 2014 at 23:37
Increasing frequency of extreme El Niño events due to greenhouse warming
Cai et. al, PUBLISHED ONLINE: 19 JANUARY 2014 | DOI: 10.1038/NCLIMATE2100 Nature Letters
The 1997/98 episode, often referred to as ‘the climate event of the twentieth century . . . Such a massive reorganization of atmospheric convection, which we define as an extreme El Niño, severely disrupted global weather patterns, affecting ecosystems4,5, agriculture6, tropical cyclones, drought, bushfires, floods and other extreme weather events worldwide3,7–9. Potential future changes in such extreme El Niño occurrences could have profound socio-economic consequences. Here we present climate modelling evidence for a doubling in the occurrences in the future in response to greenhouse warming.
Posted by: Jai Mitchell | April 11, 2014 at 00:29
The evidence and consequences of much thicker CAA sea ice is in, the underside melting has just started 3 weeks late than previous 4 seasons. Anticyclones are much more pervasive than last year at this time. http://eh2r.blogspot.ca/
Posted by: wayne | April 11, 2014 at 07:25
There it is... as expected.... Jisao PDO index has updated for March:
2014** 0.30 0.38 0.97
Source: http://jisao.washington.edu/pdo/PDO.latest
Posted by: Werther | April 11, 2014 at 10:42
I added a picture of March 17 2014, it looks like the sea ice has pilled up for miles! But it is in fact colder thicker ice and sea water,
the two make the warming sun rays ineffective in warming the ice totally. http://eh2r.blogspot.ca/
Posted by: wayne | April 11, 2014 at 18:05
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.
Posted by: plus.google.com/102121405461486954917 | April 11, 2014 at 18:16
@Chris Reynolds ... "HYCOM is intended for shipping isn't it? So do those running it intend it to be high biassed in terms of thickness to stop ice breakers running into 'briar patches' of ice too thick for them to handle. Just a WAG."
... Likewise PIOMAS? - isn't that all about not denting the conning tower when busting up through the ice to launch the missiles?
Suspect the HGTG reference is lost on many these days, BTW - but not me - Here's another...
"R17 is not a fixed velocity, but it is clearly far too fast."
Posted by: epiphyte | April 12, 2014 at 10:17
@Chris^2 - The US Navy's ACNFS might well be concerned about denting conning towers, but I wasn't aware that the Polar Science Center is funded by the DoD?
I prefer the radio series obviously, but would you say there's an infinite improbability of normality being restored in the Arctic in the 21st century?
http://www.youtube.com/watch?v=zjbtZ4NgtdA
Posted by: econnexus | April 12, 2014 at 11:39
Yes, unless there's 'covert ops' involved, PIOMAS has nothing to do with DoD. See:
http://psc.apl.washington.edu/wordpress/about/
Posted by: Kevin McKinney | April 12, 2014 at 14:41
Voilà le loup ! (here's the wolf!)
http://weather.gc.ca/data/analysis/951_100.gif
First sight of the dipole pattern with a deep low close to the northern pole. Weather patterns seem to be frozen for month since 2007, therefore 2014 could be as bad as 2007 or 2012.
Models are stuck this way for the days to come.
Posted by: Thierry | April 12, 2014 at 14:56
I've been "outed" as a "cowardly cross dresser", and I wear that badge with pride!
Here I present some shiny new Arctic sea ice resources, including PIOMAS volumes and a variety of thickness info from the ice mass balance buoys and elsewhere:
http://GreatWhiteCon.info/2014/04/new-arctic-sea-ice-resources/
As recommended by no lesser authority than Anthony Watts, the self proclaimed "center of the climate blogosphere"!
Posted by: econnexus | April 14, 2014 at 02:54
"...the self proclaimed "center of the climate blogosphere"!"
Hence the phrase, "rotten to the core." Or maybe, 'from the core.'
/snark
Posted by: Kevin McKinney | April 14, 2014 at 14:27
Hi Neven,
Over on the ASIG page the pressure map for the arctic is not updating. It seems that this link is no longer valid. Can you fix it please (I would like to be able to track those great arctic storms).
http://www.uni-koeln.de/math-nat-fak/geomet/meteo/winfos/wetterk_arctic_world-e.html
Unfortunately my German is not good enough to figure out where the link has moved to or whether it still exists on that site. Can anybody else help with a new link?
Posted by: anthropocene | April 14, 2014 at 22:40
I'll see if I can find it, anthropocene. I wanted to update the ASIG anyhow.
Posted by: Neven | April 14, 2014 at 23:56
If updating ASIGs,
displaying piomas v2.1 and current year would be better; the image to display should be:
http://psc.apl.washington.edu/wordpress/wp-content/uploads/schweiger/ice_volume/BPIOMASIceVolumeAnomalyCurrentV2.1_CY.png
Thanks for this and all the work you do.
Posted by: crandles | April 15, 2014 at 13:45
Looking at the Bremen map, there appears to be a larger than typical for this season polyna south of the Nares strait. But perhaps I misremember. Is the ice bridge still in place?
Posted by: George Phillies | April 15, 2014 at 16:07
Hi George,
Yes, the bridge is still in place.
You can check this on the DMI ice temp chart:
http://ocean.dmi.dk/arctic/ice_temp/index.uk.php
Or one a DMI satellite image (ASAR has a nice view):
http://ocean.dmi.dk/arctic/kane.uk.php
Posted by: John Christensen | April 16, 2014 at 00:18
Neven -
An OT :
I have just finished the 3rd installment of, " Your Inner Fish ".
http://www.pbs.org/your-inner-fish/about/neil-shubin/"
Hosted by Neil Shubin
Paleontologist and evolutionary biologist
University of Chicago
Not one word about a landmark series.
This is " Deep Time for Dummies ".
PAID BY YOUR TAX DOLLARS
So watch this series and learn how a fish, gave us all, opposable thumbs.
Neil Shubin has made 400,000 Million years of rocks "fun".
Posted by: Colorado Bob | April 17, 2014 at 06:10
Wipneus
Thanks for pointing out the issue with the average thickness plot. The average thickness should indeed be weighted by the area of the grid cells which our code for generating this particular graph didn't. It is now fixed. Thanks for pointing this out!
Axel
Posted by: Axel Schweiger | May 09, 2014 at 01:43