There already was a suspicion that this year would become a record year for Greenland ice melt, after all the real-time information we received from Dr. Jason Box with regards to the reflectivity of the Greenland Ice Sheet (see Dark side of Greenland), the extremely high temperatures in much of Greenland leading to above freezing temperatures at the 3200 m high Summit Camp in the middle of the Greenland Ice Sheet, leading to 97% of the ice sheet showing signs of melting at one point (see Unprecedented Greenland ice sheet surface melt), and huge amounts of water coming down the hill in Kangerlussuaq on the west coast of Greenland (see Wet side of Greenland).
The first results of a remarkable melting season in Greenland have rolled in (hat-tip to Tenney Naumer for alerting me):
Greenland melting breaks record
four weeks before season's endMelting over the Greenland ice sheet shattered the seasonal record on August 8 – a full four weeks before the close of the melting season, reported Marco Tedesco, assistant professor of Earth and atmospheric sciences at The City College of New York.
The melting season in Greenland usually lasts from June – when the first puddles of meltwater appear – to early-September, when temperatures cool. This year, cumulative melting in the first week in August had already exceeded the record of 2010, taken over a full season, according to Professor Tedesco’s ongoing analysis.“With more yet to come in August, this year’s overall melting will fall way above the old records. That’s a goliath year – the greatest melt since satellite recording began in 1979,” said Professor Tedesco.
This spells a change for the face of southern Greenland, he added, with the ice sheet thinning at its edges and lakes on top of glaciers proliferating.
Professor Tedesco noted that these changes jibe with what most of the models predict – the difference is how quickly this seems to be happening.
To quantify the changes, he calculated the duration and extent of melting throughout the season across the whole ice sheet, using data collected by microwave satellite sensors.*
This ‘cumulative melting index’ can be seen as a measure of the ‘strength’ of the melting season: the higher the index, the more melting has occurred. (The index is defined as the number of days when melting occurs multiplied by the total area subject to melting.)
Dr. Thomas Mote, Professor of Geography at the University of Georgia and colleague of Professor Tedesco, confirmed that the cumulative melt in 2012 had surpassed that of 2010 using a similar analysis.
The August 8th record differs from NASA’s announcement of unprecedented melting in mid-July, reported by Professor Tedesco and other researchers. Then, they found that the Greenland ice sheet had melted over 97 percent of its surface.
“That event was exceptional in the sense that it was an extremely rare event,” said Professor Tedesco. “Imagine Rio de Janeiro under a layer of snow and you get the idea.”
The extreme melting detected in mid-July, on the other hand, generated liquid water that refroze after a few days. “This changed the physical properties of the snowpack – making a slushy layer that turned into an icy crust after refreezing – but very likely it did not add to the runoff of meltwater that makes sea levels rise.”
The cumulative melting index, on the other hand, does account for water flowing to the ocean. The same meltwater can affect ice dynamics by lubricating the base of the ice sheet and speeding its slide toward the sea.
This year, Greenland experienced extreme melting in nearly every region – the west, northwest and northeast of the continent – but especially at high elevations. In most years, the ice and snow at high elevations in southern Greenland melt for a few days at most. This year it has already gone on for two months.
“We have to be careful because we are only talking about a couple of years and the history of Greenland happened over millennia,” cautioned Professor Tedesco. “But as far as we know now, the warming that we see in the Artic is responsible for triggering processes that enhance melting and for the feedback mechanisms that keep it going. Looking over the past few years, the exception has become part of the norm.”---------
* The National Snow and Ice Data Center provided satellite data from the United States Air Force Defense Meteorological Satellite Program.
Note that this is a measure of number of "ice days" of melting (scaled by area): probably reasonably correlated to actual cm3 of melt, but not precisely.
-M
Posted by: M | August 15, 2012 at 19:31
In the old days, water vapor (latent heat) from the south tended to condense on the sea ice.
Now the open ocean water tends to add to the latent heat in the air flowing over GIS (and other sea ice.)
Local temperature and local insolation are no longer good indicators of melt potential. We need to look at total available energy including latent heat and potential energy from the fact that some of that ice is kilometers above sea level.
Posted by: Aaron Lewis | August 15, 2012 at 20:26
Petermann 2012 is changing her mind now turning south:
http://rapidfire.sci.gsfc.nasa.gov/cgi-bin/imagery/single.cgi?image=crefl2_143.A2012228135000-2012228135500.250m.jpg
Posted by: Espen Olsen | August 15, 2012 at 20:30
So this is what it's like when the Arctic still has significant (albeit reduced) sea ice cover.
Posted by: Chris Reynolds | August 15, 2012 at 21:40
Could this melting be the first sign of a Walker cell developing between rising moist air over the open part of the Arctic ocean (and Atlantic, for that matter) and the descending katabatic (density) winds pouring down the slope of the Greenland Ice Sheet. The air that pours down Greenland has to come from somewhere.
Posted by: William Hughes-Games | August 16, 2012 at 06:58
What does GRACE have to say about this?
Posted by: www.google.com/accounts/o8/id?id=AItOawn4S99JJRLrNfgA838BLqx0pzoN7lqRBgI | August 16, 2012 at 08:40
William, thanks for that piece you wrote 4 years back. It was very informative and educative.
Posted by: Neven | August 16, 2012 at 09:45
Area crossing 3 million line at 2.986 and anomaly at 2.271!
Posted by: Espen Olsen | August 16, 2012 at 11:31
Neven, thanks for this post. Greenland seems especially hard hit this year, and may even be unprecedented in a 1000 year history :
http://www.meltfactor.org/blog/
But the 'skeptic' in me does not see any more info here than what you already posted before.
For example, I understand that this post originates here :
http://www.greenlandmelting.com/
where they refer to the "melting index" :
OK. But where is this "melting index" defined ? And it this quantified in any way ?
Which scientific paper defines this melting index ?
Posted by: Rob Dekker | August 16, 2012 at 11:35
>"OK. But where is this "melting index" defined ? And it this quantified in any way ?
Which scientific paper defines this melting index ?"
Um in the article above. I guess it isn't yet published.
"To quantify the changes, he calculated the duration and extent of melting throughout the season across the whole ice sheet, using data collected by microwave satellite sensors.*
This ‘cumulative melting index’ can be seen as a measure of the ‘strength’ of the melting season: the higher the index, the more melting has occurred. (The index is defined as the number of days when melting occurs multiplied by the total area subject to melting.)"
>" does not see any more info here than what you already posted before."
Lost on that. This seems to me to originate 15 Aug and therefore Neven is quick off the mark. This is not the same as widespread melting for a few day blogged about before.
Posted by: crandles | August 16, 2012 at 11:49
Sorry - too quick to react and post. That definition isn't sufficient as negative numbers shouldn't come out of that formula. Perhaps that graph just shows annual anomalies in the index? Maybe normalised?
Posted by: crandles | August 16, 2012 at 11:57
Some googling resulted in this:
Melting Index (MI)= Area * number of melting days
Standardized Melting Index (SMI) is calculated from MI by subtracting the mean for the period 1979 - 2012 and dividing by the standard deviation for the same period.
In other words: if the SMI over 2012 eventually ends at 2.0, we have a 2-sigma event.
Posted by: Wipneus | August 16, 2012 at 12:15
I see differences between the new "SMI index" figure
http://neven1.typepad.com/.a/6a0133f03a1e37970b0167694a8ba3970b-pi
and this old one published in 2011:
http://www.greenlandmelting.com/uploads/1/3/0/5/13056389/7577718.jpg?1343568281
2007 was the second highest melting years, but not in the new figure...
Change in methods ?
Posted by: Philippe Terrier | August 16, 2012 at 12:30
The same story told in maps and plots here:
http://www.greenlandmelting.com/browse-maps-and-plots.html
Posted by: idunno | August 16, 2012 at 12:32
Thanks Wipneus. 9 out of first 10 years are negative and 9 out of last 10 years are positive. About a 1 in 4970 chance if distribution is just random. So I think that passes a 95% chance there is a trend.
So should we conclude that this year is only slightly worse than should be expected and most subsequent years will be worse than this?
At what point should you start calculating standard deviations as residual from trend rather than anomaly from average?
Posted by: crandles | August 16, 2012 at 12:42
Not to get off topic, but is that a CT area record I see this morning.? Also 4 weeks early. As they say here is Newfoundland, "she's gone, b'ys. She's gone."
Posted by: NLPatents | August 16, 2012 at 13:04
Philippe:
Lots of differences: 1987 is the lowest in the old, unremarkable near zero in the new figure.
Crandles:
You assume uncorrelated data for the 1 in 4970 chance calculation (nitpick).
Nobody will prevent you from calculating trends. It is the conclusions that you might draw from that, e.g. did you consider cycles (AMO,AO)?
Posted by: Wipneus | August 16, 2012 at 13:09
I know someone has answered this before, but what is the time lag on CT ? One day? Or is it an average?
Posted by: NLPatents | August 16, 2012 at 13:15
Rob Dekker, I haven't had time to look into this properly (too busy with some other stuff), but I thought it'd be a good starter for the 7-course meal of records that is to come. I'm sure more info will appear in the coming weeks.
Posted by: Neven | August 16, 2012 at 14:15
NLPatents, no CT record as of yet. The latest value of 2.986 million km2 is for August 14th.
Posted by: Neven | August 16, 2012 at 14:17
With yesterday's drop in CT SIA of 111k km2, 2012 area has dropped to 2.986 million km2. Some stats:
Posted by: Jim_pettit | August 16, 2012 at 14:50
Thanks, Jim. That'll come in handy when the record is broken.
Posted by: Neven | August 16, 2012 at 15:26
Update projection and "still to melt": http://bit.ly/CTNHM2 with 94% of prior years minima already surpassed and 2-3 weeks, and who knows more days of melt reduction, limbo, and redistributions to go [compact/spread as the wind blows]. Projection worst case: 2.55M Km^2... Dire Straits, no not Mark Knopler and co but cold commerce: http://www.cpreview.org/2012/05/dire-straits/
Posted by: Seke Rob | August 16, 2012 at 15:51
>"Projection worst case: 2.55M Km^2"
I have largest decline from day .6191 in a leap year (.6165 in non leap year) as 1.15 to give a worst case projection of 1.83. I consider this very unlikely.
The best case projection of 2.986-0.196=2.79
Isn't 2.55 a 'near' best case projection (where near means one sixth of possible outcomes would be more extreme)?
I think the forecast weather will throw out that one sixth probability except strictly in the sense intended that if the area is equally likely of follow any one of the past 33 years paths with equal probability and not anything else then ....
I think the forecast weather is making a value nearer the best case 2.79 more likely than the worst case 1.83.
Posted by: crandles | August 16, 2012 at 16:54
Rob, that is if Russia's plans are not stopped by burning peat and a bubbling sea of methane.
Posted by: Jim Williams | August 16, 2012 at 17:07
Jøkelbugt North East Greenland:
A very interesting situation is unfolding in the Joekelbay. A massive fast piece of ice (5 - 6.ooo km2) is stuck in the sea of the coast +/- 50 km. When blinking the 2 links below (images from Modis) you will see that this "piece" did not move an inch over the last month, it proves that something is holding it back, and it can not only be Tobias Ø (Island found 1993)?
Open the images in 2 different tabs in your browser! And then blink them!
http://rapidfire.sci.gsfc.nasa.gov/imagery/subsets/?subset=Arctic_r02c03.2012229.aqua
http://rapidfire.sci.gsfc.nasa.gov/imagery/subsets/?subset=Arctic_r02c03.2012204.aqua.1km
Posted by: Espen Olsen | August 16, 2012 at 17:18
>NLPatents, no CT record as of yet. The latest value of 2.986 million km2 is for August 14th."
I thought we had had it confirmed that .0027 is Jan 1 which seems to me to make
2012.6191 -2.2705851 2.9863231
August 13.
I could be wrong, I have thought I had got it sussed at least 3 times then seemed to find I was wrong.
This makes the interactive chart a bit weird with its horizontal year axis running from 31 Dec to 30 Dec. But it does label 2.986 as day 226 which would be 13 April in a leap year.
So what is the source to trust? Are the maps two days later than the latest available number? Is this to allow a 5 day average?
Posted by: crandles | August 16, 2012 at 18:05
Should take a couple of years for this to start showing up on the sea level rise. But it reminds me of what Stephen Schnieder used to say, that we know there are tipping points but we just dont know where they are.
We may have already crossed a tipping point but it could be decades before it becomes obvious and when it does, it will be far too late.
Posted by: dorlomin | August 16, 2012 at 18:38
Mmm,
I use the part after the decimal point to multiply 365, then add 1, because the entire timeseries starts with 1979.000. As does each year, so that must be 1/1/xxxx
That said, day 2 of the series is 1979.0054 which is day 3! Still I overlook this anomaly, my calculation gives me day 365 correctly, at the end of each year.
So I work out 2.9863231, the figure released today noon (UK time), as relating to day 227, which is yesterday - 15/8/12.
Have I dropped a clanger somewhere?
PS, the graphics seem to update almost a day later.
Posted by: Chris Reynolds | August 16, 2012 at 19:31
Oh I should clarify.
This year I'm working the dates out as 2011. This is because every year in the CT series ends .9973, or day 365. So the CT series seems to drop a value during the leap year.
That also makes it tie up neatly with PIOMAS which also ignores leap years.
Posted by: Chris Reynolds | August 16, 2012 at 19:36
Day 227 is August 14th in a leap year, right? Does CT count the leap year day? My god, I can't believe we're having this dicussion again. This has driven me insane multiple times.
You can do whatever you like, I'm not changing my spreadsheets again. I have 2986323 km2 for August 14th and that's that.
Posted by: Neven | August 16, 2012 at 19:38
And I'm not changing MY spreadsheets, so there. Blrgh! ;)
Posted by: Chris Reynolds | August 16, 2012 at 20:18
To add to Jim's post, and for what it's worth, we're also 164972.5 km2 from setting the melt season CT area loss record.
2008 10.8871598
2010 10.739908
2012 10.7221873
2009 10.4284585
2007 10.3977587
2002 10.2877698
1993 10.2820811
And just in case you're curious, the biggest freeze season gainers in the CTA record:
2007 10.9712765
2008 10.8495002
2011 10.8037708
2009 10.38744
2000 10.3575464
2002 10.3043513
2010 10.0722902
Posted by: Dave Leaton | August 16, 2012 at 20:41
And 2012 has now equalled 2010's record of 46 century breaks.
That's according to my CT SIA spreadsheet. :-p
Posted by: Neven | August 16, 2012 at 20:45
Not to wade deep into the off-topic weeds here--again--but the problem is the inconsistent way CT has handled leap years over the course of the record.
- In 1980, a day .1631 was added between .1616 and .1644
- In 1984, a day .1658 was shoved in between .1644 and .1671
- In 1988, 1992, 1996, 2000, and 2004, there were two consecutive days marked .1644
- In 2008, there were two consecutive days marked .4438
- This year, the values for days two days numbered .1644 were combined into one. Those were then broken apart, then the values for two days numbered .1671 were instead combined.
- Non-leap year wise, 2007 was (for some reason, though I suspect that some day earlier in the year was omitted) given two consecutive days numbered .9808, while 2009 was given two consecutive days numbered .4274
WhewThe bottom line, obviously, is that with the leap days being accounted for near ice maximum when the least daily change usually occurs, it seems fair to me to simply ignore any daily loss/gain during that period, and focus instead on the total ice coverage, which will be accurate despite what CT has done with the calendar. And graph-wise, I tend to just ignore the leap days as well, since every bit of the true ice loss I track occurs subsequent to leap day, anyway.
(FWIW, unless there's more calendar manipulation by CT, December 31 will be day .9973, the 365th day in the CT record [because of the aforementioned combining of two days numbered .1671].)
We have to strive for accuracy and precision, of course. But if our data sources are themselves a bit idiosyncratic, we have to accomodate and compensate for those idiosyncracies as best and honestly as we can. That's my goal, anyway... ;-)
Posted by: Jim_pettit | August 16, 2012 at 21:05
That would be correct. ;-) 46 century breaks this year, and 7 double century breaks. By comparison, 2011 had, respectively, 39 and 3, while 2007 saw 41 and 6.
Posted by: Jim_pettit | August 16, 2012 at 21:16
Funny is that last time Neven quoted the century count, he had one more than I had, *and* I made no change to my sheet [LoL]
*and*, or *to include* (Just like dotting the eyes at times ;>)Posted by: Seke Rob | August 16, 2012 at 21:36
I've just looked at the area records again. Around this time of year, 1979 (and 1996) went below 6m, 2004 went below 5m, 2009 went below 4m and 2012 is going below 3m. You can see the melt speed up in the PIOMAS volume record, but it also clearly shows in area now.
Posted by: AmbiValent | August 16, 2012 at 21:53
Epsen,
I believe that ice is grounded on the Belgica Bank. That area was just mapped in 2004.
http://www.agu.org/pubs/crossref/2006/2005GL025131.shtml
Posted by: James Benison | August 16, 2012 at 22:35
>"This year I'm working the dates out as 2011. This is because every year in the CT series ends .9973, or day 365. So the CT series seems to drop a value during the leap year."
There are 366 values for 2008 because one digital date is repeated
2008.4438 -0.9495078 9.2806721 10.2301798
2008.4438 -0.8914949 9.2806721 10.1721668
now that might just be a repetition of the 9.2806721 compensating for a missing 29 Feb.
However for 2004 there is
2004.1644 -0.4795871 13.6285448 14.1081324
2004.1644 -0.4727035 13.6381149 14.1108189
That seems like different data and according to my interpretation .1644 is both 29th Feb and 1 March.
So I think there are 366 lines of data for each leap year. Also repetition at .1644 looks good for my interpretation :o) (so I'm not changing my spreadsheet either :-P )
Posted by: crandles | August 17, 2012 at 00:32
One more small piece of esoterica that might have rhetorical value: CT Area has been below 50% of the 1979 daily numbers for the last week. It had never dropped below 50% before this season.
Posted by: Dave Leaton | August 17, 2012 at 02:27
here's a question for those mathematically inclined.
Given the U.S. lower 48 was 3.3 F above average in July, how much extra heat energy does that 3.3 F anomaly translate to? And, how much Arctic sea ice would that extra energy melt if transferred with 100% efficiency?
Posted by: Fairfax Climate Watch | August 17, 2012 at 05:02
Between 140E and 105E at 85N (just west of Severnaya Zemlya) are two large masses that seem to be seperating from the CAB pack. The current ice flow is moving counter clockwise around the south of the SZ islands towards the Kara Sea. What do you think the chances are that it changes direction and puches them in the the Laptev Sea?
Posted by: Frankd 1977 | August 17, 2012 at 07:03
crandles wrote "But it does label 2.986 as day 226 which would be 13 April in a leap year."
Look at the labeling on the first (leftmost) day in the interactive chart. You'll see it's labeled 'Day 0'. That's why you have to add 1 to CT days to match with MODIS usage, which has Jan 1st as Day 1.
Chris Reynolds wrote "because the entire timeseries starts with 1979.000"
uh, no. Look again at the data file. The first line is:
This is the data for Jan 1st, 1979 and the start of the time series.
Neven's CT date usage agrees with Larry Hamilton's. It would be helpful if we added a FAQ section to this blog over the Winter, I think.
Cheers,
Lodger
Posted by: Artful Dodger | August 17, 2012 at 09:05
Neven, crandles, sorry for coming in a bit harsh in my comment.
My point was that I did not find the source article (greenlandmelting.com) in the post, and when I found it, the article itself was not very well sourced. So naturally a little 'yellow' light went off inside of me.
Thanks to Wipneus the issue got cleared up.
In fact, the definition of the Melting Index (Area * number of melting days) makes a lot of sense, and Standardized Melting Index (SMI) definition even more. Wipneus writes :
This is actually a very helpful definition which puts the Goliath 2012 Greenland melting season into very clear perspective.
And, to complete my apology to Neven : Yes, this post DOES add information to your previous posts, since neither the albedo-change article nor the unprecedented 97%-of-Greenland melting present the crucial info about sea-level-rise and Greenland water run-off on exactly how much area overall melted for exactly how many days.
So, Neven, this post is not just presenting another record in Greenland, but in fact a very important and concerning one.
Posted by: Rob Dekker | August 17, 2012 at 09:15
Hi all,
Over the page on Daily Graphs, Arthropolis is showing a temp of 13C for Alert. This is about as hot as I can recall ever seeing.
Simultaneously, the DMI temp plot for latitudes above 80N is now dipping below freezing.
Any explanations?
Posted by: idunno | August 17, 2012 at 16:36
http://lance-modis.eosdis.nasa.gov/imagery/subsets/?subset=Arctic_r03c03.2012228.terra
Quite a lot of non ice covered land near Alert. That is going to give a higher temp than average of north of 80N most of which is ice covered with a little water only slightly above freezing point of about -1.5C. Land with little ice cover is only small fraction of the area.
Posted by: crandles | August 17, 2012 at 17:10
Historic data for Alert:
http://tinyurl.com/Alert-NU-climate-8-17-12
13 C there is warm, but far short of record warmth, FWIW.
crandles has the right of it; the northern tip of Ellesmere is just a tiny fraction of the total area N of 80.
Posted by: Kevin McKinney | August 17, 2012 at 18:12
idunno:
Alert is probably more affected by low albedo than NP - more likely with higher temperature in Alert than NP due to lower albedo in the neighborhood is my guess. NP will probably not have higher summer temperature until it has lower albedo i close vicinity.
Posted by: Oslo | August 17, 2012 at 19:25
Hi idunno,
The DMI temp plot is also the 24 hour average temperature. Alert's average temp for the day is what you should compare. Here's Environment Canada's 24-hour history page for Alert, Nunavut:
http://text.www.weatheroffice.gc.ca/trends_table/pages/ylt_metric_e.html
I find it even more remarkable that winds currently are SSW 51 km/h gust 63 km/h. That'll move some sea ice!
Lord Soth, what would it take to get a webcam up there at Alert?
Posted by: Artful Dodger | August 17, 2012 at 23:15
Many of the curves I've seen extrapolate more or less smoothly to zero ice extent or zero ice area or zero ice volume. But, isn't there a threshold thickness below which the ice cannot maintain its integrity under the combined forces of ocean and atmosphere dynamics, and essentially collapses. And, if so, how far are we away from that point?
Posted by: Superman | August 18, 2012 at 00:32
>"more or less smoothly"
most would be smooth with curves of different shapes. However second graph in Wipneus' outlook
http://www.arcus.org/files/search/sea-ice-outlook/2012/08/pdf/pan-arctic/klazes.pdf
Do you extrapolate with straight line through origin, straight line not through origin or a curve.
If you believe in "a threshold thickness below which the ice cannot maintain its integrity" then perhaps the trend switches from one straight line to the other creating a non-smooth point.
I think I am more inclined towards a curve gently bending one way then back the other way down toward origin turning increasingly sharply. That is based on not really believing in one sharp point ie break down in integrity will happen at different thicknesses for different sized pieces of ice so it doesn't just happen all at once. However that is pretty much just wild speculation without any evidence to support it rather than a confident prediction.
Posted by: crandles | August 18, 2012 at 01:06
More from Jason Box, as told to Bill McKibben:
http://www.rollingstone.com/politics/news/the-arctic-ice-crisis-20120816
Posted by: idunno | August 18, 2012 at 02:15
Today a 4,5 km2 calving appeared on Kangerlussuaq Glacier, SW Greenland.
the calving front was more or less stable during the last three years. When I put MODIS r02c02 under my CAD overlay day 230, the front was still intact.
This underlines the dynamic change all around and over the GIS this season.
Posted by: Werther | August 20, 2012 at 22:44
NASA has launched a new GRACE website for the 10th Anniversary of the mission.
No news on the Summer 2012 Greenland melt, yet...
Cheers,
Lodger
Posted by: Artful Dodger | September 04, 2012 at 06:00
http://i174.photobucket.com/albums/w109/frivolousz21/slr_sla_gbl_free_txj1j2_90.png?t=1346731909
first Sea Level Rise data with part of the summer.
Posted by: Chris Biscan | September 04, 2012 at 06:21
Wow, Chris B!
Sea level has returned to the trend-line established before the dramatic floods of Summer 2011. Do you have numerical figures in mm/yr for sea level rise this year?
Cheers,
Lodger
Posted by: Artful Dodger | September 04, 2012 at 06:30
http://ibis.grdl.noaa.gov/SAT/SeaLevelRise/LSA_SLR_timeseries_global.php
You can get them below in text files.
There is a huge jump in July it seems.
the other main sources haven't updated yet.
Posted by: Chris Biscan | September 04, 2012 at 06:37
Wowsers.
It looks like sea levels have more than recovered the temporary decline of Summer 2011, increasing about 13 mm above the dip a year ago. Now also over 4 mm above the linear trend line for the whole data series which begins in 1993.
Wouldn't want to live in the low Countries (no matter how beautiful ;^) ...
Cheers,
Lodger
Posted by: Artful Dodger | September 04, 2012 at 07:35
Morning Lodger.
I've got a personal refuge on 430 m + in France... Should be safe yeah(if drought isn't gonna get me..)
No kidding, Chris B came up with the first signs of SLR that 'should' appear.
Spread 700 km3 melt of the GIS over 350Mkm2 oceans and its clear the count is on. El Nino is going top contribute too.
The first step, 15 cm in 10 years, south tip Greenland falling is in the make. This gets serious when it hits 4000 km3 a year (by 2016?). Should be visible by then on MODIS in general retreat of the sheet margin.
Posted by: Werther | September 04, 2012 at 08:00
No man is an island, Werther ;^)
You think 4000 km^3 Greenland melt by 2016? What would that make the time for the doubling?
Last time I looked, people were thinking a possible range of 6-10 years for the doubling, awaiting data. I think Hansen bases his 2100 SLR predictions on a 10 year rate.
Cheers,
Lodger
Posted by: Artful Dodger | September 04, 2012 at 08:09
Lodger, actually I didn't figure this out thinking in terms of doubling. As I studied the geographics of southern Greenland late 2006, this was what seemed to fit natural processes. It's a step-thing; melt concentrated on the south tip first, phase 1 up to 2050, steepest curve in the '30-s, then a slowing while forcing builds and the whole GIS gets involved.
I hold this to fit well into forecasts by Rahmstorf and Church.
Posted by: Werther | September 04, 2012 at 08:18
Oh...forgot to mention that my timing sucks... Had expected this all to happen a little earlier.
I hope that flaw continues and provides adaption time!
Posted by: Werther | September 04, 2012 at 08:20
Hi Werther,
I agree about the geographic progression of melt in Greenland. Clearly we're seeing it already. Luckily we have good people like Jason Box and colleagues watching the melt, so we shouldn't be blind-sided.
I've read elsewhere about kinematic constraints to acceleration of Greenland glacier flow. Basically the long, narrow and shallow fjords work to slow rapid advance of glaciers.
Antarctica, especially the WAIS, is another matter entirely.
Cheers,
Lodger
Posted by: Artful Dodger | September 04, 2012 at 08:40
For you Data-hounds and Chart-mongers: (h/t Chris Biscan)
Global mean sea level data in .csv format from TOPEX, Jason-1, and Jason-2 satellites, with Seasonal signals removed
Cheers,
Lodger
Posted by: Artful Dodger | September 04, 2012 at 08:49
Werther,
Greenland does indeed look like a hot-spot for SLR. (click the image to go to the NOAA webpage)
Posted by: Artful Dodger | September 04, 2012 at 09:04
Great sites through the links again, Lodger.
Could be fresh water = less dense = larger volume.
Same effect for Hudson, Bothnian Gulf in Scandinavia.
They remark that in the data isostatic rebound through ice loss isn't incorporated.
Indonesia: coriolis force and warm upwelling...
Pity there's no data for the Arctic. Would the fresh water bulge in Beaufort have shown up?
Posted by: Werther | September 04, 2012 at 09:41
http://sealevel.colorado.edu/content/2012rel4-global-mean-sea-level-time-series-seasonal-signals-removed
Form that page, there is links on the left side of the page to the 4 major sea level trend algorithmic sources. most updated through 2012.4518
the one posted here with the big spike goes further to 2012.6500 or so.
Posted by: Chris Biscan | September 04, 2012 at 09:52
An article has been posted on the record melting event in Greenland last summer:
http://onlinelibrary.wiley.com/doi/10.1002/joc.3743/abstract
The combination of an extended blocking high during most of the summer and a negative NAO created the conditions for this level of melting according to the article.
Posted by: John Christensen | June 18, 2013 at 15:27
Joe Romm has talked with Dr jennifer Francis about this over at climate progress:
http://thinkprogress.org/climate/2013/06/17/2169321/exceptional-2012-greenland-ice-melt-caused-by-jet-stream-changes-that-may-be-driven-by-global-warming/
Posted by: Boa05att | June 18, 2013 at 18:10