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Unprecidented warmth in Arctic

Discussion in 'Environmental Discussion' started by bwilson4web, Oct 24, 2013.

  1. icarus

    icarus Senior Member

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    "The ice must have receded 225 to 4,285 years ago.
    Meaning it was as warm or warmer 225 to 4,285 years ago as today .(assuming temp is the only affect on ice caps which is a silly premise)" Mojo


    Please explain the logic in the above example. Just because thte was moss groing on
    Baffin in the previous 4000 years, it doesn't logically follow that it "must have been as warm or warmer than now. ( and ergo CO2 was not a cause of warming!)

    It simply means (absent any other info) that it was warm enou to support mosses!

    Icarus
     
  2. mojo

    mojo Senior Member

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    The logic you question is the method and premise of the study.
    But if you accept Millers logic and his conclusions,you have to accept that the newer mosses were grown during a period warmer or as warm as today.
    If you dont accept that logic then you cant accept any of Millers conclusions.

     
  3. tochatihu

    tochatihu Senior Member

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    Still haven't collected the paper (just sayin'). But I know that moss will grow wherever it does not get quickly buried in snow. It grew wherever/whenever it could. After that, the old dead buried moss could be preserved, unless its snow/ice cover melted away and then it would 'become CO2' and disappear. If the snow/ice cover was not lost for a very long time, then very old moss could become exposed. This is my thinking.

    So, what specific concerns concerns have you about the study results? Knowing those would help me to read the paper more closely.
     
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  4. austingreen

    austingreen Senior Member

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    It seems to me that given the entire globe once had ice free oceans in a previous interglacial, the artic warmth is not unprededented.

    The most the IPCC seems to have been able to say looking at the data, is during the mideaval warming period or MCA if you prefer, the global temperature was colder in any 30 year period. We don't have proxies that have the resolution that say it was colder every year then today. Also clearly some places are colder and some warmer than 100 years ago. It seems quite likely that even in the last 4000 years some places in the arctic were warmer than today. We have some proxies that say some places were warmer even during the mideaval warm period.

    We have this proxy study, from eastern canada part of the arctic, that appears to be warmer than it has been in millenia, but we also have proxies from greenland, that were warmer more recently. You need to put all the arctic proxies together to figure out if the arctic was warmer or cooler. There is no inconsistancy if one spot was warmer than today, and anouther cooler, that is how warming and cooling works, it is not uniform.

    The other thing speculated on by miller is that the mideval warming period was caused by volcanic eruptions. The question then becomes the old one. How much of today's warming is caused by those gasses dissipating, how much by other natural forcing, and how much by ghg.
     
  5. bwilson4web

    bwilson4web BMW i3 and Model 3

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    Thanks for the reference:
    I just bought the paper and took steps to removed the 24-hr limitation.

    Sad to say, the following is the type of "cherry picking" that can lead many to be fooled . . . <something> by omission:
    The ancillary data is available without buying the paper. But embedded within the paper is this curious table:
    [​IMG]

    All of this nonsense about "225 to 4,285 years" is derived from an ancillary table without the text from the paper explaining why it is important. Worse, embedded within the paper is this table with a much older range of dates. In effect, the "225 to 4,285 years" is a 'freebie' table that is and has been too easily (aka., lazy!) quoted as the paper. It is a favorite trick by deniers.

    Now about buying a paper from Willie . . . what a miserable business model. They sell "24 hour access" so embedded in the PDF is probably some 'date/time' range that Adobe reader will honor. At $35, this 16 page report is nearly $2/page for a single day access. So to open my window so I can read and study the paper:
    1. Screen shots - done. Physically large, it is better to have the 16, quarter of a megabyte files than not 25 hours from now.
    2. Adobe 'conversion' service - done. Saved as both ".rtf" and ".doc", the time limits should now be filtered out and I can copy-paste accurately without having to just retype from the image.
    So I've got my copy of the paper and within 'fair use' will study it in more details at my leisure. But this particular table was important to point out why "quoting out of context" is at best, not very bright. Then to cite the incomplete data, to further misrepresent the paper, well it suggests "hook, line, and sinker."

    Bob Wilson
     
  6. bwilson4web

    bwilson4web BMW i3 and Model 3

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    From the paper:
    The table "Mojo" cited was used as a reference, part of a comparison to the actual, new data from the paper. This is why it is so important to read the paper.

    Bob Wilson
     
  7. bwilson4web

    bwilson4web BMW i3 and Model 3

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    Ah HA! So that is how they identified modern contamination:
    Source: ibid

    Now this makes sense and suggests alternate collection mechanisms. Instead of waiting for natural melt to expose the underlying, dead flora, spread out a plastic 'tent' over a collection site, well anchored to prevent external contamination. The melt water should flow out and if attention is paid to preventing air-born contaminates, a more pristine sample should emerge.

    Now there was some confusion about the ice cores from Greenland. This is what the paper has to say:
    Source: ibid

    This is a nice paper and aside from the publication expense, one I have enjoyed. I have not summarized how they covered the altitude effects in the paper. I find their description enlightening but not important until someone else gets a copy of the paper and wants to chat about this technical point. But overall, everything is well presented and clear that anyone should enjoy the read.

    Bob Wilson
     
  8. tochatihu

    tochatihu Senior Member

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    The supporting information is by no means ignorable. Publishers generally offer that now, and with an advantage that it is free to download. It is not printed in the journal's pages so it does not cost the publisher much. They have to keep there servers up anyway, hoping that people like Bob will come along and pay for full access.

    Table_S1 is correctly labeled. It lists the C14 dated samples that died during the Holocene (most recent 11,700 years). This is not all their dated samples. If a person doesn't know, or doesn't want to know what Holocene means, well yeah, it is possible to become confused.
     
  9. tochatihu

    tochatihu Senior Member

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    Most of the materials they collected and dated were younger than 4000 years. The ones that were much older were the main focus of the text. One cannot really fault them for collecting and analyzing samples that were not extremely old, cause they don't look different. They collected a lot of samples over quite a large area. Obviously spent a lot of money as well because Each AMS analysis is way more than USD$100.

    One can only speculate what is appearing in Miller's email inbox. He may be wishing that the public education system would teach the meaning of the word 'Holocene' :)
     
  10. tochatihu

    tochatihu Senior Member

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  11. bwilson4web

    bwilson4web BMW i3 and Model 3

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    One of the reasons for re-reading the original article is to ferrite out nuances. Then it makes sense to look at other commentary:

    In one respect, reading Marcia and Gifford is a dialog, a commentary with merit. But once you get into the subsequent commentary . . . well it is obvious many did not read the original paper. They came with their favorite 'ax to grind' and tried to noodle out some way to swing their obsession.

    So the data found in the freebie table, the Holocene era samples, says the sample areas were warm when the flora first grew. So even within the '225 to 4,285 years' of the original table, there was a 'cold period', frozen until collected in 2005-2011 (more about this later.) The samples could be collected because of melting, prima facia that the collection areas are recently warmer. But these were not the only samples.

    Serendipity, they found flora samples on four, melting ice caps at the limits of C14 dating. When compared with the Greenland ice cores, 600 miles away, the C14 limits push the last growth periods back to "~120 ka, at, or near the end of the Last Intergaciation." What they have done is reveal a methodology that can be applied to other melting areas to find more metrics.

    Doug pointed out the melting ice fields are revealing artifacts buried for thousands of years. But now we're seeing C14 timing helping to more accurately map the freezing . . . and the collection date . . . how long that area has been below 0C and protected by the snow and ice cover. That the sample could be collected give a threshold, a temperature rise.

    I see this paper as leading to similar efforts in Eurasia and perhaps the most southern tips of South America. More facts and data, a good thing. But the most important lesson is the difference between those who read the paper and those just wandering about with their dull ax looking for a grind stone.

    Upon reflection, something that bothers me are the time ranges:
    • ~4,000 years - spanning the 'deep freeze' events
    • ~6 years - spanning the 'melt' events
    The rate of cooling spans 10**3 years and the warming span less than 10 years. If the rate of warming were at similar rates to the original cooling, I would expect the 'deep freeze' range to be smaller. My analogy is an onion. We can take an onion and remove the layers, one-by-one just like the original onion grew, layer by layer. But if we take a sharp knife, we get all of the layers at once. I am piqued that the short sampling span from rapid melting is revealing a longer series of 'freeze events'.

    Bob Wilson
     
  12. austingreen

    austingreen Senior Member

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    Ok, question? What difference does it make if the arctic was warmer during the mwp or mca (as some have relabled it)?

    We know some places in the arctic were warmer than today during the mwp. It is difficult to reconstruct a temperature for the arctic given some proxies are warmer than today, some colder than today. It seems fairly clear within the bounds of the proxies, the mwp was warmer than the lia, and colder than today on a global scale, in any 30 year period. The proxies don't let us drill down further. Go out longer, say to the roman warm period, and its likely it was colder than today, but proxies have a large amount of uncertainty. I would not bet sebelius's job on that, although we are more certain that it was colder, than today, than healthcare.gov will be working by the end of November. Lots of uncertainty.

    Is arctic warming unprecedented? No, it was warmer at some time in the past, and we are extremely confident of that. Was it warmer anytime in the last 4000 years? I don't really care, but its likely the east canadian arctic is warmer today, the rest of the arctic need other reconstructions. We've got moss, and ice, and sea creatures, and a lot of uncertainty. Lets just say the East canadian arctic is the warmest it has been in tens of thousands of years.
     
  13. bwilson4web

    bwilson4web BMW i3 and Model 3

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    Well taken from the paper:
    Source: ibid

    The reason this is important is the solar radiation is now 9% lower than the warmest Holocene period yet this area is warmer, significantly warmer than it was then. Something is making this part of the earth warmer so the authors go on to state:
    Source: ibid

    The great "Global Warming Pause" has been trotted out to claim there is none . . . a denier strawman. We still have deniers trying to claim that if we don't see every year some minimum increase in earth temperature then it proves there is no global warming. And then we get a report that provides quantitative data, a real metric, of how much the warming has exceeded the solar radiant energy.

    What this data point, this report, does is give a quantitative metric that the global warming in this area exceeds the 9% loss of solar radiation from the Holocene era. In effect, the solar heat retention from green house gasses is equivalent to at least a 9% warmer sun. As for a "Global Warming Pause", ice has that curious property of holding a liquid at a fairly constant temperature until it melts . . . and the ice is melting. It would give the illusion that heating has paused.

    Bob Wilson
     
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  14. austingreen

    austingreen Senior Member

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    Again, since the earth does not warm and cool evenly, why is this one proxy important? Isn't global temperature the important thing? To me this is a red herring if it is taken as important, since the next proxy found that is cooler today will be trumpeted.

    The only thing I see from this reasearch, other than the headline which is false, is one more proxy to help compute global temperature in the past. Who really cares if spot A was warmer, and spot B was colder. It certainly is not me.

    We have the same problem here though, don't we? If 1998 proved temperatures were rising faster than ever before as some claimed, and would do so in the future, then we have a pause. But if we look at the right metric, temperatures rising over many years, there is no pause, simply natural variability. We should not call it a pause, its natural variability on a long term trend. We do in the ice cores see temperatures rising as fast as today, and many suspect this is related to natural releases of ghg, just as this paper speculated on the lia starting with lots of cooling volcanic activity, than when dissipated, would cause a future warming.

    Again we have unequal warming and cooling. Yes these guys that wrote the paper are all excited about 1 proxy, although I fail to see it affecting many paleo climate models. All it does is validate them a tiny bit. It even validates the mwp and lia;-) something the hockey stick attempted to erase. Its just one data point. Don't base global temperature on a single proxy in a small geographic region.
     
  15. bwilson4web

    bwilson4web BMW i3 and Model 3

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    There are lots of proxies with great gaps in between both physically, time and methodology. But that is how science moves forward. There will often be a 'first experiment' but it is not important if others can not replicate the result using similar or even different methodologies. In one respect this is a 'first experiment' using material found in recently melting snow/ice cap.

    The importance is not just this one island in Canada but the methodology can be repeated in the Eurasian continent to establish more proxies at different physical sites but not just in the Arctic regions. Any high, snow covered mountains such as the Alps, Himalayans, African, and South American ranges might provide similar data. Possibly even some of the islands around Antarctica. It is 'death by a thousand cuts' when every additional proxy is added to complete the picture of what is going on our planet.

    The question "Isn't global warming temperature the important thing?" sure looks like a distraction from the insights this particular paper provides. Hummm, distraction, another word for "red herring" perhaps?

    If you want to propose a "global warming" paper, I'm OK. But as for this particular paper, by itself, it doesn't make or break global warming . . . something many deniers can't fathom because they don't know how science and its handmaiden, engineering, works.

    Rather this paper provides a methodology, a "first experiment", that can be replicated where similar snow, ice, and terrain might provide another data point. It also gives an idea that the forcing function has to be at least as strong as the missing 9% solar radiance. It also opens new areas of investigation or query.

    We know CO{2} had an ability to blanket thermal photons from the earth. Earlier experiments have shown it has a non-linear proportion to the fraction in the earth's atmosphere. So now I'm wondering if there is a table or formula that for any given CO{2} ppm we can use to calculate the equivalent increase in solar radiance?

    I suspect this table for formula is embedded in the climate models but I'm new to this field. So I ask for simple engineering data tables like this. My question comes directly from the 9% greater solar radiation from this paper and how the current ice cap melt is occurring.

    Bob Wilson
     
  16. tochatihu

    tochatihu Senior Member

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    @32 "Lets just say the East canadian arctic is the warmest it has been in tens of thousands of years"

    I can totally live with that. Miller et al. would take it further, because their oldest moss dates to 40-50 kya when the C14 method punks out. That time was high glacial, so they suggest that the material actually grew during the previous interglacial. This is plausible but not directed established by their data. They argue that it was so and argued a strong CO2 link, and so (a) they hit the media and (b) other folks have hit back.

    If you must know :) their +/- on the old dates is not quite as narrow as it ought to be. May mean that they did not utilize the most fastidious collection techniques. May mean that some caribou took a leak on the overlying ice during the last few thousand years. The most interesting (few) samples were from 2010 and I'd hope the authors go back for more in 2014 summer.

    I collected soil charcoal through a depth series, hoping to establish a forest paleofire record in subtropical China. Supposedly the C14 AMS has been done, but I have not seen it :). Miller's study makes me wonder of we were fastidious. Wait and see. But for me the most interesting thing that popped up in our sampling was a cobble layer buried in the depositional surfaces. Ailao Mountain had one big whacking flood, and the charcoal ages above and below are going to reveal when that happened. I am sure it was long after Younger-Dryas, but it was Biblical. If I may dare to say so. We can teach others how to look for it, and discover its extent. It is really interesting, and not at all what we set out to find. A lot of science 'stumbling' is like that.

    But for me, and for Miller, we are examining paleo-points on a large diverse planet. Spatial extrapolations only work when there is concordance with other more remote studies. So, we should put them all into some bin, and give appropriate weight to other points where evidence shows discordant histories (such as, where earlier warm times were really warm).

    MCA and LIA and other observed paleoclimatic excursions happened somewhere, at some time, and people who study them are finally obliged to reconstruct a concordant global pattern. It is a thing we should all want to know. My advice (not that you necessarily want it) is to continue to spend research $$ on the activity. We might learn a lot more about what the oceans are capable of. In my mind this is the largest deficit of IPCC-summarized climate science. Paleo or right now.

    Data from any paleo-point means something. It won't mean a lot until the broader pattern is described in time and space. I reckon we'll get there in a few decades, and if we are lucky, the ongoing +CO2 won't strongly inhibit our global enterprise during the time. Perhaps more likely, a collapse of the Pine Island glacier (or something similarly lurid and large) will push us towards holding the line on +CO2. Where paleo and climate models have not.

    As we are not yet following the precautionary principle, we must hope that the ocean will save us. As it has, except when it has not, during major extinction events.
     
  17. austingreen

    austingreen Senior Member

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    Absolutely. That is what the paper says to me. Unprecidented? That was my problem. Arctic, I don't know. East canadian arctic, now we are talking.

    Yes. IMHO ghg link is to global not local temperature. To say that you would need to have it change drastically the other multi-proxy paleo data. I don't think it does that.

    Sure, we also have 100 year resolution, but are comparing it to less than 100 years present. We all expect temperatures to go up, but ....


    Yep, exactly my point. Glad you feel the same way.
     
  18. tochatihu

    tochatihu Senior Member

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    So, a new thread is required. Did IPCC AR5 , based on all available paleo data, build the 'best' space/time climate reconstruction, or did they not? If not, somebody will need to do better and (hint) it won't be me.
     
  19. austingreen

    austingreen Senior Member

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    Did it do the best they could? I have no idea, I didn't see a paleo reconstruction, only the temperature record going back to instrument times.

    AR4 was certainly better than IPCC AR3 (hockey stick)
    http://www.ncdc.noaa.gov/paleo/pubs/ipcc2007/fig614.html
    [​IMG]
    I know individual papers have improved on this.
     
  20. bwilson4web

    bwilson4web BMW i3 and Model 3

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    As a 'first experiment,' I would expect lessons learned that they and other investigators can avoid but at the risk of becoming scatological, "Does a Panda <something> in the woods on future samples?"

    All joking aside, to what extent can surface material compromise sub-surface samples? Is there a protocol other than say removing the first 1-2 cm and using a different set of tools to dig deeper?

    I've read lay reports of coal contamination from ground water bringing in modern C14. How extensive this is remains an open question. Just I'm curious how field workers who are at the limits of C14 are able to minimize modern contamination of the samples.

    Bob Wilson