I'm pretty sure someone mentioned these while I was away in slowinternetistan, but the visuals are so stunning that I'm posting them two weeks later. These videos, uploaded to YouTube by noiv, were shot by folks on one of the helicopters of the Polarstern research icebreaker. I don't know when they were shot exactly, probably somewhere in August, in the area that we refer to here as the Laptev Bite:
Melt ponds anyone? Or how about some rotten ice for your Martini?
There are a couple more videos like this one (here and here). And here's one showing the Polarstern.
Two weeks ago Noiv also uploaded a video that shows preliminary sea ice thickness measurements by the ESA's SMOS satellite (which I wrote about back in February):
This animation is now accompanied by an official ESA press release:
ESA satellites looking deeper into sea ice
5 October 2012
This year, satellites saw the extent of Arctic sea ice hit a record low since measurements began in the 1970s. ESA’s SMOS and CryoSat satellites are now taking a deeper look by measuring the volume of the sea-ice cover.
Measurements from ESA’s Soil Moisture and Ocean Salinity (SMOS) mission show that ice has thinned significantly in the seasonal ice zones, with extensive areas less than half a metre thick.
Sea ice has a large influence on the heat exchange between the ocean and the atmosphere. The heat flux can change depending on the sea-ice thickness and the air temperature. Sea ice is also affecting atmospheric circulation at mid-latitudes.
Although not originally designed for looking at ice, the SMOS satellite’s data are being evaluated to monitor Arctic sea ice.
The results reveal that radiation emitted by the ice allows SMOS to penetrate the surface, yielding ice-thickness measurements down to 50 cm – mainly the thinner and younger ice at the edge of the Arctic Ocean.
This allows improved evaluation of the volume of the young ice, which is the basis of old ice in subsequent years. Thick, multi-year ice indicates the health of the Arctic sea-ice cover.“The amount of thin ice expected during the next freeze-up is about 12 million sq km, covering a larger part of the Arctic Ocean than ever before,” said Lars Kaleschke from the University of Hamburg’s Center for Earth System Research and Sustainability.
“The thick ice that has survived the summer, however, covers only 2.2 million sq km.”
The advantage of SMOS is it covers the entire Arctic Ocean on a daily basis, though the resolution is relatively low, at 35x35 sq km per pixel.
For a more detailed look at thick sea ice and ice shield thickness, ESA’s dedicated ice mission, CryoSat, uses a different technique and higher resolution along its ground track – about 300 m.
Earlier this year, the first seasonal variation map of Arctic sea-ice thickness from CryoSat was revealed. It was the first map of its kind generated using data from a radar altimeter and at such a high resolution.
Read the rest of the press release at the ESA website.
Another cool video that hasn't been uploaded to YouTube (so I can't embed) is in a NOAA ClimateWatch Magazine article from three days ago, discussing this year's melting season and the declining trends of multi-year ice and sea ice volume, with accompanying animations.
Edit: a commenter has uploaded it to YouTube.
And commenter Andy Lee Robinson has updated his excellent 3D Piomas graph video:
The AWI page for the expedition is here:
http://www.awi.de/en/news/newsflash/2012/august/
where they refer to two more running blogs (one in German one in English). Apparently they are even now deep in the growing ice. From the style of the images it reminds me of this blog entry,
http://www.geo.de/blog/geo/polarstern-expedition/wissenschaft/im-kalten-fliegt-s-sich-besser-von-stefan-hendricks-arbeitsgruppe-meereisphysik-awi?LTblog=26d6c765186d98d337c7ebff6abcc637
which would mean it was end of September. Once there, one should note the last blog entry,
http://www.geo.de/blog/geo/polarstern-expedition/leben-an-bord/polarstern-hovercraft-sabvabaa-huckepack?LTblog=26d6c765186d98d337c7ebff6abcc637
highly impressive photos of current conditions up there. From the interview with the hovercraft ice researcher, I translate:
"Q: Yngve [Kristoffersen], you were very long out here during the new ice minimum. How did this extreme ice recess appear to you?
A: (I noticed) especially the very warm air temperatures. I really hadnt counted on this: it was so warm that my fresh food turned bad (victuals). Usually, I just put them outr there in chests, nature cares for the cooling. But we had severe plus-centigrades, and the vegetables just didnt keep themselves. Also, the ice has gotten very soft, one coud see it strongly melting everywhere. And it rained, even in the middle of September I experienced incredible rains, (it was) as if I would be back in the mountains."
their english blog is actually very good reading too!
Posted by: Enno | October 05, 2012 at 23:12
I enjoyed the video that came up after the first one finished!
http://www.youtube.com/watch?feature=player_embedded&v=ARJK0MWAITM
Posted by: Alan Clark | October 06, 2012 at 00:31
I'm a "street artist" (freeways, actually) that reaches about 250,000 people daily - probably more:
http://freewayblogger.com
Am very interested in slogans/texts regarding the Arctic sea ice as prelude to catastrophe. The best I've gotten so far came from a commenter here (paraphrased) "We should reflect on the arctic ice because pretty soon the sun won't be."
Great stuff. Need more. You wouldn't believe what I can do with cardboard, paint and an overhead projector.
Posted by: scarlet p. | October 06, 2012 at 03:44
not a video but a webcam I posted about during the slurry of melt records may have went unnoticed: currently located in beaufort gyre, i guess. http://obuoy.datatransport.org/monitor#buoy8/webcam
Posted by: Otto Lehikoinen | October 06, 2012 at 03:52
The end of the second video simply shows the mid September melt outline well in advance in February. 2012 was essentially a melt of the thin ice present at Maxima. The red thin ice in February also outlines the tracks of Southern in origin cyclones which penetrated Arctic Ocean fortress winter almost at will.
Posted by: wayne | October 06, 2012 at 03:58
Neven,
That NOAA ClimateWatch Magazine video has just been uploaded to YouTube, so you can embed it now, if you want to edit your post.
http://youtu.be/cQ3QUdIxvxg
Fortunately, US Gov't products are public domain, so I shouldn't get in trouble for uploading it to YouTube.
Steve C
Posted by: Steve C | October 06, 2012 at 06:46
The multi-year ice video in the NOAA ClimateWatch Magazine article is fascinating to watch in slow motion. Three distinct processes behind the disappearance of MYI can be observed:
Posted by: Yuha | October 06, 2012 at 07:50
Thanks, Steve C! I've updated the post.
Posted by: Neven | October 06, 2012 at 13:25
Scarlet P--How about:
"It's not your father's Arctic--and still less, your child's."
Posted by: Kevin McKinney | October 06, 2012 at 14:43
"Someone mentioned these while I was away"
That would have been me Neven!
In view of the current circumstances I wondered if I might enquire what you make of my use of the ice thickness video (amongst others) to try and enlighten the folks over here in South West England about what's going on?
http://econnexus.org/why-should-i-care-where-the-arctic-sea-ice-went
Posted by: Jim Hunt | October 06, 2012 at 14:55
Only been coming here for a few months. I was wondering if SIE rebound......
http://www.ijis.iarc.uaf.edu/en/home/seaice_extent.htm
....is behaving as expected, given the new low attained in September. Should we expect the extent to eventually match other years in the past decade in January through March or will we see a shift downward in maximum extent?
Posted by: Djprice537 | October 06, 2012 at 16:44
Freeway Blogger.......
I catch your comments on Atrios periodically.....hang tough.
Posted by: Djprice537 | October 06, 2012 at 16:46
As a newbie here I ask a question that I hope is not too dumb. I would hazard a guess that first year ice (I guess that is FYI) is not as thick as multi year ice, thus making it easier to melt and get mushed up in the arctic storms. So my question(s) is: Did the little bit of rebound in years 2008-2011 due to the multiyear ice left in the refreeze season, or was it the weather that caused what little rebound it had? And, is it possible to see the same rebound the next few years?
Posted by: Mary A Bein | October 06, 2012 at 16:59
Djprice537:
The winter maximum is in a declining trend, just not as dramatic (yet) as the summer minimum. See this image from Cryosphere Today:
http://arctic.atmos.uiuc.edu/cryosphere/IMAGES/seasonal.extent.1900-2010.png
That plot goes through 2010. I wish they'd update it. You can also look at the sea ice (area) anomaly to see the long term decline:
http://arctic.atmos.uiuc.edu/cryosphere/IMAGES/sea.ice.anomaly.timeseries.jpg
Posted by: Bruce Worden | October 06, 2012 at 17:16
Mary,
You'll probably get a few opinions here, but my take on the data is that 2007 was exceptional because of exceptional weather (superimposed, of course, on a long-term declining trend). The "recovery" that followed in 2008 and 2009 was simply a "dead cat bounce" back toward the trendline, perhaps enhanced by somewhat cooler weather in those years. The arctic really, really wants to freeze and stay frozen, but that tendency is being overwhelmed by the changing climate.
This year was not driven by particularly exceptional weather, it was the result of the long term erosion of the ice volume (a steady decrease in the multiyear ice that you mention) brought about by a dramatically warming arctic.
So its hard to say what will happen next year. If it's a warm year, the record could be broken. If it's cool, or the wind blows the ice around at the end of the season, we could see a somewhat greater extent. No matter what the extent does, one thing is almost certain: there will be less ice volume next year than there was this year.
Posted by: Bruce Worden | October 06, 2012 at 17:28
Mary, 2008 maxima was exacerbated by a cool La-Nina which reduced clouds at the North Polar region. There can be severe winters again in the Arctic, but the timing of - AO must be just right. No clouds during the long dark night is essential, several years decline must be compensated by several years recovery, the odds of refurbishing the ice to former health over a decade is quite low though, almost impossible.
Posted by: wayne | October 06, 2012 at 17:30
Mary Bein:
I too am a newbie and therefore won't answer your question. It took me a week to realize that NH did not stand for New Hampshire! I think Neven would be doing a great service by listing the top 100 (200?) acronyms with simple definitions. What does CAB stand for?
Posted by: Conrad Schmidt | October 06, 2012 at 17:31
Also Cryosphere soon to be record slow recovery:
http://arctic.atmos.uiuc.edu/cryosphere/IMAGES/seaice.anomaly.arctic.png
Encourages further incursions of low pressure cyclones from the South. Which bring heat, so somewhere South of the Arctic they will complain "its cooler". All while cyclones keep the Arctic warmer. The shape of the surviving ice pack is not conducive for a quick refreeze.
Doesn't look good for a 2013 recovery, only La-Nina may play a role.
Posted by: wayne | October 06, 2012 at 17:57
wayne, I've been betting on a slow recovery too, but right now the dice are still rolling across the table.
Posted by: Jim Williams | October 06, 2012 at 18:08
CAB: Central Arctic Basin
Posted by: Jim Williams | October 06, 2012 at 18:09
Bruce, Wayne, Conrad,
Thank you for your valuable input. And Conrad, I am still trying to figure all those acronyms; although when I do finally figure them out I think(hah) that I am just 1% smarter. And yes, it took me a while to figure out NH.
Posted by: Mary A Bein | October 06, 2012 at 18:10
FYI also has a higher salt content than MYI, and whilst this means that it melts at a marginally lower temperature, it is mechanically weaker.
Sorry about the acronyms.
Here are some of the most commonly used:
FYI -First Year Ice.
MYI - Multi Year Ice.
Geographic:
NH - Northern Hemisphere
SH - Southern Hemisphere
CAB - Central Arctic Basin
CA - Canadian Archipelago
NZ - Novaya Zemlya
SZ - Severnaya Zemlya
GIS - Greenland Ice Sheet
Many of out abbreviations are the initials of organisations which produce the data available on the Daily Graphs page, above:
NASA - NASA (I've forgotten - National Aeronautical and Space Agency?)
NSIDC - National Snow and Ice DC
IJIS/JAXA - they're Japanese
DMI - Danish Maritime Institute?
CT - Cryosphere Today
MODIS satellite images are produced by NASA
GISS - Goddard Institute for Space Studies
WUWT is the most prominent skeptical site
PIOMAS is a computer model of ice volume
Oceanographic/Meteological
ASI - Arctic Sea Ice
SST - Surface Sea Temperature
SAT - Surface Air Temperature
Neven, perhaps you could open a thread that would allow regulars here to contribute to a list of our most commonly used bits of gobbledigook?
Finally, at the top of the page, there is a "Glossary" tab, which links to a very good list produced by the National Snow & Ice Data Centre.
Hope this helps.
Posted by: idunno | October 06, 2012 at 18:15
Mary, NH is mostly important when figuring out how to talk the graphing toys oriented towards showing either El Nino or U.S. into showing the Arctic instead. Of course, then they say "Northern Hemisphere."
Posted by: Jim Williams | October 06, 2012 at 18:15
See, I knew someone mentioned them. Thanks again, Jim Hunt, and sorry for the delay.
That's a very nice post you wrote, Jim. Videos are always good. You could perhaps put up a vid with Dr Jennifer Francis to explain how disappearing sea ice is actually influencing the jet stream and thus UK weather.
Posted by: Neven | October 06, 2012 at 18:23
BTW, I've added Andy Lee Robinson's latest 3D volume video to the post.
Posted by: Neven | October 06, 2012 at 18:24
Also:
SIA - Sea Ice Area
SIE - Sea Ice Extent
MASIE - is a measure of SIE produced by NSIDC
CIS - Canadian Ice Service
BTW - By The Way
Posted by: idunno | October 06, 2012 at 18:27
Jim, I agree with Einstein, "God doesn't play dice with the weather" :). There is chaos in the smaller regions of the world, but even then this chaos is like musicians in an orchestra, they play in a beautifully synchronized natural sequence. Somethings are easier to predict, Arctic sea ice being one of them. Unless the land coastal areas freeze very fast and suddenly due to Siberian hyper cold weather, it will be slow, so far, land snow extent shows all the signs of the Northern continents in a slow refreeze mode. So I leave the dice for casinos and check constantly if I understand the future.
Posted by: wayne | October 06, 2012 at 18:41
Mary
It's possible that the 'glossary' tab on the top line might prove useful.
FYI isn't just thinner, it also contains a lot of salt. The brine channels allow melting at lower temperatures and make it far more susceptible to mechanical breakup.
Another fairly recently discovered factor is that because of the high salt content, the melt water sinks to about 200m, stirring the water layers and not allowing a freshwater lens to form a thin skin above that's available for quick refreeze.
Old MYI used to be advected(transported) through Fram Strait, then when Nares Strait started opening on a regular basis a lot of the oldest ice advected through that channel. Most recently the CAA (Canadian Arctic Archipelago) - the passages between islands in the Canadian north - opened at the end of the 2011 melt season and this year the old MYI found a new way out through this labyrinth. "Found a new way out", is probably inaccurate because what we found was that as the MYI moved into this area it simply melted away.
For any kind of meaningful rebound the MYI needs to find a place where it can stay and grow while shedding it's salt content. This used to occur north of Greenland,
Ellesmere Island and above the CAA. Today all these areas are open to advection so MYI is either advected to warmer climes, or is melted as the Beaufort Gyre sweeps it into the now warmed waters north of Alaska, the Yukon and Siberia.
Atlantic currents, western storms, lowered albedo (reflectivity, changing weather patterns and the mixing effects of winds on the open water are all probably much more important feedbacks to the temperature rise that increasing GG (Greenhouse Gasses) provide, but the loss of MYI, at least in my opinion is reason enough to preclude a return to the Arctic that existed as recently as a decade ago.
Terry
Posted by: Twemoran | October 06, 2012 at 18:51
wayne, I think he was completely wrong about it. The fundamental nature of existence is pure chaos. We invent rules attempting to describe this chaos. Some descriptions are more useful than others.
I'm also strictly non-theistic. I don't consider the notion of God to have any value as a descriptor -- either in terms of existence or non-existence. (I get into arguments with Atheists.)
Posted by: Jim Williams | October 06, 2012 at 18:51
Thanks to all for helping with the acronyms. And thanks for not making me feel like a really stupid person.
Posted by: Mary A Bein | October 06, 2012 at 19:02
Jim, Einstein being wrong is an OK concept, he was a few times incorrect, he was very human, and somehow us humans can come up with perfect things or concepts. I think he used God as a metaphor in this case. But I predicted many many events right especially this year, so much for chaos. It is a matter of focus, study and being in synch with the subject you study. Atheists are too certain, absolutists, and therefore are wrong by their stance.
Posted by: wayne | October 06, 2012 at 19:04
Djprice537 asked:
Bruce Worden wrote: The way I have heard it explained here before is that the Arctic Ocean is largely land-locked, so when the Arctic Ocean freezes, in most directions it can freeze only up to the land's edge. So even though winters warm more rapidly than summer or fall you are not going to see much of a downward trend in winter sea ice extent for a while.A nice contrast with this is the Southern Ocean around Antarctica. For the most part, the southern hemisphere is warming more slowly than the northern hemisphere. (Please see Tamino's Jan 11, 2008 "Hit You Where You Live" and Jan 17, 2008 "Down Under" available at Back from the Dead: Lost Open Mind Posts.)
This is about what we would expect, given the models. However, there are very few places where the Southern Ocean is actually cooling, and most are right up by the coast of Antarctica. Nearly all of the Southern Ocean is seeing some warming. (Please see Why is southern sea ice increasing? (intermediate) for a good map of land and ocean surface temperature anomaly trends.)
But the Southern Ocean is also seeing a freshening of the surface water due to continental ice melt. The fresh water has a higher melting point than the saltier sea water below, and given its lower density, it is resulting in greater stratification, so that the saltier, warmer sea water below has less of an effect on surface sea ice formation. And even then, most of the Southern Ocean is actually seeing a decline in sea ice.
The majority of sea ice growth has been in the more southern Ross Sea, where the East Wind Drift carries much of the fresh water melt from the West Antarctic Peninsula. Thus even though the Southern Ocean isn't land-locked, there has been a small upward trend in sea ice.
Posted by: Timothy Chase | October 06, 2012 at 19:25
Is nobody else having problems with the SMOS thickness retrievals?
Here is a still of the Feb 2011 and 2010 thickness plots from the video.
Here is the PIOMAS thickness plot from gridded PIOMAS data for Feb 2011. 2012 data is not yet available.
The SMOS 2011 image when compared to PIOMAS seems to imply much thinner ice. For example, in Beaufort PIOMAS shows thinnest of around 1.5m, yet SMOS shows around 0.4m! For the rest of the Arctic it's hard to say, as SMOS only goes up to 50cm, but there's a lot of pink in various regions implying <0.5m in areas PIOMAS shows just below 2m thick.
PIOMAS may be smearing the thickness somewhat, as the points are average thickness of each grid point.
But when you get to 2012...
Bear in mind that the SMOS thickness plot states it's for Feb 2012 - after the ice has done much of the thickening after the rapid growth in autumn. If we take 2011 as typical for PIOMAS - it's thinner than typical, then how come SMOS is showing much of the Arctic as pink shades - around 0.4m thick. Only a year before PIOMAS was reporting just under 2m thick!
It's also worth bearing in mind that the loss of thickness for PIOMAS over March to September 2011 is of the order of 2m. Plot.
I don't know what to make of this.
The Kaleschke et al 2010 paper is here.
Posted by: Chris Reynolds | October 06, 2012 at 19:52
Thanks for your kind words Neven, and thanks for your suggestion too.
I am familiar with the Jennifer Francis video(s) you refer to. However in this instance I figured they might be a bit too "sciency" for my assumed audience. I also wanted to get a Met Office vid in there somewhere, not least because the Hadley Centre is within cycling distance of where I'm sat typing these words to you.
I'll certainly post one or more videos of Jennifer in the near future. Have you seen these?
http://www.youtube.com/watch?v=D58xDmzMnpk
Posted by: Jim Hunt | October 06, 2012 at 20:10
Scarlet P
Check out the Global Warming bumper sticker sayings at:
http://www.zazzle.com/hobertshouse
Posted by: opensheart | October 06, 2012 at 20:12
PS
I had written:
Rather than leaving it at that, I should have mentioned that ocean has greater thermal inertia, and therefore warms more slowly than land. Since the bulk of the earth's land is in the Northern Hemisphere, we expect to see the Northern Hemisphere warm more quickly than ocean. This is the physics which is getting captured by the models.Posted by: Timothy Chase | October 06, 2012 at 20:26
Sigh...
Correction:
Posted by: Timothy Chase | October 06, 2012 at 20:30
Several people have wondered at what made 2007 different from 2008-2011 and 2012. I suggest looking closely at the eruptions of volcanoes in the Alaskan archipelago, in Alaska and Kamchatka. Cleveland and others erupted in the sporting and summer just in time to throw aerosols into the Arctic to disrupt the melt. These can happen any year. A lot of them erupted in 2008 - 2011.
Add we approach 2015 and the first ice fee Arctic summer, these can be importamt.
Posted by: Sam | October 06, 2012 at 20:55
That last should read 'spring and summer'. My spell checker was overly helpful.
Posted by: Sam | October 06, 2012 at 20:58
Chris,
you are absolutely right! Don't take the SMOS ice thickness as absolute value. There are large uncertainties and the thickness has always a low bias if there is thick ice (>0.5m) in the field of view.
By the way, you point to the 2012 GRL paper, not to 2010. This can be found here: http://www.the-cryosphere.net/4/583/2010/tc-4-583-2010.pdf
In this paper you find in the conclusions:
"We suggest that the retrieval should be interpreted as a lower boundary of the thermodynamic (i.e., modal or level) ice thickness."
With SMOS you can not distinguish if the ice is 60 centimeter or 6 meter thick because of the saturation of the emissivity (see Fig 1).
As an example, have a look at http://www.arcus.org/files/search/sea-ice-outlook/2011/07/images/pan-arctic/image009.png
There you see the so called "modal thickness" is about 3 meter but the average thickness is larger because of the shape of the distribution.
Unfortunately, the press release has not stressed the uncertainties. Here is some text which became not part of the press release:
"It has been shown that the measured L-band brightness temperature can be clearly related to the sea ice thickness for ice not thicker than half a meter. However, since it is not a direct measurement of thickness and the algorithm includes several assumptions, there are potential uncertainties. At first, the retrieval is influenced by open water and leads within ice cover. Because we assume a 100% closed ice cover, the ice appears to be thinner if open water is present. Secondly, the brightness temperature is influenced by changes of the ice temperature and bulk salinity. Thirdly, the brightness temperature is influenced by a snow layer on the sea ice. Despite the remaining uncertainties with respect to the absolute SMOS thickness, we can state that Arctic sea ice became significantly weaker between the years 2011 and 2012."
So, please be careful with the interpretation and comparisons to other data. Sea ice thickness is not always the same sea ice thickness. There are many thicknesses: mean thickness, modal thickness, effective thickness, and now we also have the "SMOS thickness". You have to take it qualitatively until we have more validation data which are very sparse.
Lars
Posted by: Lars Kaleschke | October 06, 2012 at 21:00
Lars.
Thanks for the guidance, and for your work on this.
Don't know how I got the wrong paper - Doh!
Given your finding of significant weakening from 2011 to 2012 it will be interesting to see how the PIOMAS gridded data reflects this when it's available next year. And indeed what next year's melt season is like.
Posted by: Chris Reynolds | October 06, 2012 at 21:26
Scarlet:
How about this:
If Earth were a coal mine, the polar bear would be our canary.
Posted by: Robertscribbler.wordpress.com | October 07, 2012 at 06:45
Scarlet P.
I like to play with words, so how about?
Global Warming: Coming to a theater near you soon!
Posted by: Ggelsrinc | October 07, 2012 at 07:28
Though, my first impulse is Climate Change!
Posted by: Ggelsrinc | October 07, 2012 at 07:31
Scarlet,
Or how about:
A barrel of oil: $90
A doomed civilization: iceless
Posted by: james cobban | October 07, 2012 at 07:39
Current circumstances in South West England have now combined to allow me to include a Jennifer Francis video in a post that explains why, somewhat unusually for me, I didn't go surfing today:
http://econnexus.org/how-global-warming-causes-bugs-on-british-beaches/
Feedback welcome. Positive or negative!
Posted by: Jim Hunt | October 07, 2012 at 17:17
Jim,
Have you read my blog posts on the connection between the Arctic and UK's cool, wet summers since the crash of 2007?
http://dosbat.blogspot.co.uk/2012/09/summer-daze-2012.html
You'll find the first Summer Daze post outlines how unusual this pattern is.
There is more to it than Dr Francis's work on Arctic Amplification affecting the jetstream. However it seems to me that on top of this we've been having more lows that sit over the UK and dump large amounts of rain over the country. Lows normally (used to??) seem to me to move over the UK as a rule, not just sit there. That could be due to Francis & Vavrus finding a larger persistent kinks in the jetstream. However in summer the low pressure tendency outlined above is itself due to a standing wave driven by the effect of the Greenland high.
Posted by: Chris Reynolds | October 07, 2012 at 17:58
Hi Chris,
I'm relatively new here, and so I'm afraid I hadn't read your "Summer Daze" before. Thanks for the link, and now I'll have to go away and read up on the Greenland high and standing waves.
However I have to agree with you that subjectively the weather here in SW England changed post 2007, although back then I didn't associate it with changes in the Arctic. I even said as much in public:
http://econnexus.org/hurricane-hanna-helps-ecodriving-video/
As you so delicately put it - "Is this a coincidence? Is it F..."!
Posted by: Jim Hunt | October 07, 2012 at 20:28
Scarlet P -
I suggest "Winter Isn't Coming"
Posted by: no1der | October 10, 2012 at 16:50
Real Climate posted a first of 7 parts topic about a 7-set video on Climate change, evidence and effects.
http://www.realclimate.org/index.php/archives/2012/10/climate-change-videos-part-i/
Already posted the YouTube links in my favorite denialist thread. My posts there always start with something like: Not for those in willed bliss... (It's run by a reli-boy... CO2 is good for [all] plants, and puny man does not know enough)
Posted by: Seke Rob | October 10, 2012 at 18:05
On a not wholly unrelated note, I've recently been involved in a heated debate on the merits or otherwise of wind turbines on the ThisIsDevon web site, over here in South West England. Even David MacKay has also passed comment!
As a side effect of all that I've also just posted a comment on this article:
http://www.thisisdevon.co.uk/Recent-wet-summers-caused-warming-North-Atlantic/story-17050818-detail/story.html
I thought I'd pass it on, just in case anyone else here has strong views on such matters.
Jim
Posted by: Jim Hunt | October 11, 2012 at 16:04
Seke Rob: "Real Climate posted a first of 7 parts topic about a 7-set video on Climate change, evidence and effects.
http://www.realclimate.org/index.php/archives/2012/10/climate-change-videos-part-i/ "
Nice shows. You can see all of them simply by not doing anything when one ends.
In general, I think they overstate the state of our current understanding, and thereby tend towards a somewhat more rosey picture than is warranted.
Posted by: Jim Williams | October 11, 2012 at 19:26
BBC says nothing to see here. Move along please:
'Frankenstorm' bears down on US east coast
Comments?
Posted by: GeoffBeacon | October 27, 2012 at 00:34
Hi Geoff, please continue at the latest post: Looking for weirdness.
Posted by: Neven | October 27, 2012 at 01:13