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David Horton at 11:46 AM on 12 January 2010Skeptical Science now an iPhone app
John, this post could have begun "There is a dramatic hot spell sweeping across Australia" (44oC in Melbourne yesterday for example). A major tool of deniers has been to exploit the shift in seasons. "Hot in the northern hemisphere in July? Well, yes, it's Summer, whaddya expect, besides, it's cold in Australia". "Hot in Australia in January? Well, yes,it's Summer, whaddya expect, besides, it's cold in Europe." Seasonal variation is a gift that has kept on giving to deniers for many years. -
shawnhet at 08:00 AM on 12 January 2010Why does CO2 lag temperature?
It is I think important to remember that prior to human industrial activity CO2 was, for all practical purposes, a feedback not a forcing. Given that we know that the CO2 increase by ~15ppm per deg C., we can calculate that at the depths of the ice age there was a CO2 feedback of 1.12(assuming CO2 concentrations of 205 and 190 respectively). (ln(205/190)/ln2)*3.7w/m2 gives ~ 0.4/W/m2 ~temp increase is ~.11+ .11^2+.11^3.... is approximately equal 1.12. IOW if the sensitivity of the climate not counting CO2 was 3 deg. K/W/m2, the sensitivity of the climate including CO2 should be ~3.36K/W/m2. Cheers, :) -
Ned at 06:40 AM on 12 January 2010Why does CO2 lag temperature?
You know, I wish this thread had a different title. CO2 lags temperature sometimes. See, e.g., Milankovich cycles. CO2 leads temperature sometimes. See, e.g., flood basalt episodes, vaporization of carbonate rocks during bolide impacts, and combustion of fossil fuels. Somebody or other once compared CO2 and temperature to two individuals handcuffed together. Wherever one goes, the other has to follow. Right now, we're very much in a situation where CO2 leads temperature. -
beegdawg007 at 06:17 AM on 12 January 2010Why does CO2 lag temperature?
An interesting article which explains why a period of extreme global glaciation could also be simultaneously a period of extremely high levels of atmospheric CO2. There is one point which the article does not make as clear as possible. When the earth is extremely cold, humidity is also extremely low. What happens in a cold climactic setting is that the effect of CO2 as a greenhouse gas is amplified simply because CO2 and H2O both absorb energy from the two of the same spectral bands. Currently H2O exists at levels 50 times greater that CO2 (20-25,000 ppm vs 387 ppm). So, now, most of the IR energy for the overlap bands is absorbed by H2O. However, if the air was nearly bone dry while CO2 concentrations were in the range of say 10,000 ppm, CO2 could actually become a much more influential greenhouse gas. To view the overlap spectra of CO2 vs H2O use this link... half way down the article shows a graph of the impact of various greenhouse gases on the IR spectra of energy that is reflected from the earths surface .. http://forthegrandchildren.blogspot.com/2009/03/best-global-warming-discussion-ever.html Link to the entire article http://www-eps.harvard.edu/people/faculty/hoffman/snowball_paper.html “”In the late 1980s, Joe Kirschvink at the California Institute of Technology pointed out that during a global glaciation, what he termed a "snowball" Earth, the supply of carbon dioxide to the atmosphere and oceans from volcanism would continue because of plate tectonics. However, if the Earth were so cold that there were no liquid water on the continents, weathering reactions would effectively cease, allowing carbon dioxide to build up to incredibly high levels. Eventually, the carbon-dioxide-induced warming would offset the ice albedo, and the glaciation would end. Given that solar luminosity 600-700 million years ago was about six percent lower than today due to stellar evolution, Ken Caldeira and Jim Kasting at The Pennsylvania State University estimated that roughly 0.12 bar of carbon dioxide (about 350 times the present concentration) would have been required to overcome the albedo of a snowball Earth. Assuming current rates of volcanic carbon dioxide emissions, a Neoproterozoic "snowball" Earth would have lasted for millions to tens of million of years before the sea ice would begin to melt at the Equator. A "snowball" Earth would not only be the most severe glaciation conceivable, it would be the most prolonged.”” -
beegdawg007 at 05:23 AM on 12 January 2010Why does CO2 lag temperature?
CO2 lags temperature change for one obvious reason. The ocean contains 93% of all of the CO2 in our biosphere in one form or another. Some of the CO2 which is locked up in the ocean in the form of soluble gas is exhausted into the atmosphere when the ocean warms and it is reabsorbed by the ocean when the ocean cools. Out-gassing... This phenomenon of the change in the solubility of gases in liquids as a function of temp and pressure has been of course been measured many times over and can be proven with the simplest lab experiments. In other words, on this issue, the science is really truly and honestly "settled". This phenomenon is also the reason that ocean CO2 concentrations are greater in the polar regions than in the tropics and this is why tropospheric concentrations of CO2 in the atmosphere are greater in the tropical regions than in the polar region. As my daughter would say, its a "Henry's Law" thingy... http://en.wikipedia.org/wiki/Henry's_law That is why warmer climactic periods usually result in higher levels of atmospheric CO2. Of course, that is not necessarily true. Periods of exceptional volcanism can temporarily create a climate which is simultaneously cold and rich with CO2. -
keysersoze at 03:44 AM on 12 January 2010CO2 lags temperature
I would like to ask a question that I would regard as common sense (the true deficiency of our planet IMHO). If temperature increases, whether from co2 or other sources, and that in turn causes the release of more co2 wouldn't that cause what is known in my industry a "feedback loop" which is a perpetual increase where it reaches a limit according to a viability of materials to handle such a load. So basically, it would either keep increasing until something "breaks" or would reach an equilibrium of perpetual continuance. That "balance" would look like; temperature increases with co2 until enough water vapor (the biggest greenhouse gas) would block enough incoming radiation to halt the increase of temperature resulting in a new perpetual balance between co2's greenhouse effect and water vapor's? I'm looking for an answer to what ended other warm periods in our history like the Paleocene period. Because if co2 levels lag temperature by roughly 800 years so would it's greenhouse effect, continuing it's "greenhouse" warming creating a cooling buffer but it doesn't, it just drops off like a fat lady falling off her chair at an all you can eat buffet.Response: Good question - I considered addressing this in the original article above but opted to keep things simple and address it in a future post. In the case of Milankovitch cycles, just as orbit changes initiate the warming, they also end the warming. Towards the end of the deglaciation, orbit changes cause the amount of June sunlight falling on the northern land masses to change by several tens of percent (not an insignificant change). Gradually over time, northern ice sheets start to grow again.
For greater time scales (eg - over millions of years), rock weathering is another factor that keeps the climate regulated. Rock weathering is the phenomenon where CO2 is scrubbed out of the atmosphere by chemical reactions with rock surfaces. As temperatures warm, the rate of rock weathering increases - this acts as a natural thermostat to keep CO2 levels from getting too high. However, this process occurs over millions of years so don't expect rock weathering to bail us out of our current situation (although interestingly, there is research into using artificially accelerated weathering as a technique in sequestering CO2). -
RSVP at 00:29 AM on 12 January 2010Why does CO2 lag temperature?
Ned I dont think I have introduced anything tangentially into the discussion, and any comments, opinions, or deductions have been based on the material as presented on this website. Usually these comments address aspects of the apparent "fundamental harmonic" of what is being presented. For instance, in #15, using the data as given, I imply Milankovitch cycles have tens times the weight of CO2 in affecting climate. I am not inventing anything here, just commenting on what the data seems to suggest. Is that so out of order? -
Ned at 23:48 PM on 11 January 2010Is the airborne fraction of anthropogenic CO2 emissions increasing?
Still further thoughts on the problems with Lindzen's 2009 paper here. Trenberth et al. seem to have really demolished that hypothesis. -
Ned at 23:33 PM on 11 January 2010Is the airborne fraction of anthropogenic CO2 emissions increasing?
Marcus writes: By contrast, though it has still to be independently verified, Lindzen's hypothesis regarding "The Iris Effect" is based on quite sound scientific principles (yes, I have read the paper, & understand enough of it to make this judgment)-even though Lindzen is a noted Skeptic. Actually, there really isn't good evidence for Lindzen's iris; in fact, there's now quite a bit of evidence against it: Chambers et al. 2002 Lin et al. 2004 Rapp et al. 2005 Trenberth et al. (in press) There's some good discussion of this here and here. -
Marcus at 23:19 PM on 11 January 2010A visual deconstruction of a skeptic argument
Also, nofreewind-to date only a couple of scientists (Lindzen & Spencer-both noted skeptics) have proposed that GHG-induced warming will lead to a negative feedback as a result the so-called "Iris Hypothesis". Yet many other scientists have failed to find supporting evidence for their hypothesis, instead finding evidence that the decline in cirrus clouds resulting from sea-surface warming actually has a net *positive feedback* effect. This view has been backed up by data from the CERES satellite (louds and the Earth’s Radiant Energy System), that shows that any increased heat-escape potential generated by the decrease in cirrus clouds in the canopy is more than made up by the increased sunshine allowed in by the decrease in Earth's albedo. According to scientists working on CERES, the countervailing forces results in a modest, *positive* forcing caused by the Iris Effect. -
Marcus at 23:06 PM on 11 January 2010A visual deconstruction of a skeptic argument
You've got to give nofreewind points for bravely waving the anti-science banner here on behalf of the fossil fuel industry. The reality is that the ice core data quite clearly shows that CO2 levels have remained at around 260-280ppm for the better part of 30,000 years-yet we're supposed to believe that the sudden rise in CO2 emissions-by more than 100ppm-in the last 50 years is *purely* coincidental with the sudden rise in burning of fossil fuels in our cars & power-stations. He also expects us to believe that CO2 will saturate at a low level, when a simple look at the geological record shows a strong correlation between atmospheric CO2 levels of greater than 2,000ppm & average global temperatures of roughly 22 degrees C (compared to roughly 15 degrees throughout the bulk of the Quaternary Period)-in spite of the sun being about 10% *cooler* at that time, no sign of "saturation" there. A basic knowledge of geologic history would also reveal that the relatively low CO2 levels (& cooler climate) of the Quaternary Period are because these vast quantities of CO2 (mostly from tens of millions of years of volcanic activity & land-forming processes) were sequestered out of the atmosphere by the world-spanning forests of the Carboniferous period-& again in the Cretaceous period. These great forests later died & were fossilized deep under the ground. In the last 150 years, we've managed to dig out large quantities of these fossils, & are burning them for energy. You don't need to be a genius to work out what the final result of that will be-most likely the re-release of pre-Quaternary CO2 & the warming of the planet to levels closely approximating pre-Quaternary levels. -
Ned at 23:04 PM on 11 January 2010Why does CO2 lag temperature?
RSVP: "The CO2 level lagging suggests, CO2 is subject to the Milankovitch cycles and not the other way around." It works both ways. If you force a temperature change first, CO2 will follow (and amplify the temperature change). If you force a change in CO2, temperature will follow (and amplify the CO2 change). Milankovich cycles are an example of the former. But there are plenty of examples of the latter, too, including: [a] Weathering during tectonic uplift (which removes CO2 and cools the planet; see, e.g., Ruddiman 1997). [b] Chris's examples of the vaporization of carbonate-rich rocks from a bolide impact, or outgassing of CO2 during massive flood basalt episodes, both of which add CO2 and warm the planet. [c] Rapid release of fossil carbon from methane clathrates, or from combustion of coal and oil. With all due respect, RSVP, there are commenters on this site who have a great deal of expertise in earth system science. I for one really appreciate their taking the time to participate here -- it's what makes this site stand head-and-shoulders above most other climate blogs. You could learn a lot by paying more attention to what some of those commenters have to say, rather than just tossing out one argument after another. -
RSVP at 22:13 PM on 11 January 2010Why does CO2 lag temperature?
Chris, The CO2 level lagging suggests, CO2 is subject to the Milankovitch cycles and not the other way around. As concerns eccentricity, obliquity, and precession, it would seem that precession would not affect climate at all, except in shifting seasons with respect to their relation to the stars. Furthermore, depending on the phase relation of eccentricity and obliquity, you could either have a reinforcing or cancelling effect. I did not see any mention of this in the article, however based on the sawtooth waveform, where the temperature rise is punctuated after a long and slow dropoff, this would seem to indicate a reinforcing where the orbital minimum coincides with less tilting. In any event, I agree that my perception appears "less than logical" to anyone who is bent on proving AGW. -
Riccardo at 21:01 PM on 11 January 2010What ended the Little Ice Age?
batsvensson, #17 it looks to me that you are taking the data "as is" without adding the physics of the processes involved in climate variations. We are not analizing an unknown signal, we are looking for the link between forcings and temperature. This is what "put into a perspective" present and past climate. #18 "larger than expected" refers to what is now widely accepted as the best estimate. And it does not come from nowhere, it comes from the analisys of many different phenomena. Climate sensitivity is not an abstract concept, it's the physical link between forcing and temperature variation. It can not take any value, it need to be contrasted with what we know had happend. Explaining the glacial cycles requires the knowledge of forcing and feebacks which, together with the climate sensitivy, gives you the temperature variation. Given the forcings and feedbacks (crudely, Milankovich cycles and ice and CO2 feedbacks) a increased sensitivity would results in a temperature variation higher than obeserved. So the problem is not that "I can not imagine how it can happen", it is that a high sensitivity cannot explain the glacial cycles. -
batsvensson at 17:06 PM on 11 January 2010What ended the Little Ice Age?
Riccardo you wrote in #4: "if a small sun variation can induced detectable increases in temperature it can only mean that climate sensitivity is much larger than expected ..." I assume "sensitivity" and "variability" in above are the same, and want to ask: "larger than expected" than what? Yuo also wrote: "it would be hard to explain the temperature difference between glacial and interglacial with such a huge sensitivity" Why would this be hard to explain with an increased sensitivity/variability? Statement like this sound to me like "since I can not imagine how it can happen then it can not have happen." What reason do we have to believe this to be true? -
batsvensson at 16:40 PM on 11 January 2010What ended the Little Ice Age?
Riccardo, thank you for taking time to make the answer in comment #13, however I am well aware of the techniques on how to calculate a bandwidth or variability or whatever label is preferred to use for this. What I am asking about is our knowledge of the variability in the past. Because the "conclusion" that "Meehl 2004 is also confirmation that past climate change tells us how sensitive climate is to radiative forcing." which is not a conclusion at all is a nonsense statement unless we can put into a perspective of past variability or "sensitiveness" (which is yet another label for the same thing). -
Bern at 12:16 PM on 11 January 2010Why does CO2 lag temperature?
Thanks all for the wonderfully informative posts & comments. I've learned a lot just from reading this one page! -
yocta at 10:53 AM on 11 January 20101998 DIY Statistics
RE: #26 Ricardo Thanks that is a helpful paper. I wanted to know how the variances were recorded. The methods in Section 3 "Aggregation of the Raw Data" seem to address that. -
boba10960 at 10:32 AM on 11 January 2010Why does CO2 lag temperature?
A couple of things to add to what Chris has posted: Ian - If the CO2 were coming from methane, then it would have a strong isotopic signature characteristic of the methane. Natural sources of methane are strongly depleted in carbon-13 relative to carbon-12. During the deglaciation there is a small excursion in the isotopic composition of CO2 recovered from ice cores (Smith et al., 1999), but much smaller than would be expected of the CO2 were produced by oxidation of methane. Rather, the carbon isotope signature of CO2 during deglaciation is consistent with the release of CO2 from the deep ocean (Spero and Lea, 2002). Smith, H.J., Fischer, H., Wahlen, M., Mastroianni, D. and Deck, B., 1999. Dual modes of the carbon cycle since the Last Glacial Maximum. Nature, 400(6741): 248-250. Spero, H.J. and Lea, D.W., 2002. The cause of carbon isotope minimum events on glacial terminations. Science, 296(5567): 522-525. David - In Greenland the annual layers of ice can be counted back for about 40,000 years. In older ice they become squeezed so much by the pressure of the overlying ice that they can no longer be identified. (I don’t remember exactly how far back people have counted annual layers, but it’s roughly 40,000 years). In Antarctica the annual layers cannot be counted so far back in time because the annual snow accumulation is generally much less than in Greenland. Therefore the layers start out thinner and it takes less time before they become indistinguishable. -
chris at 09:28 AM on 11 January 2010Why does CO2 lag temperature?
Well yes, RSVP but I think you're falling for exactly the mistake that John Cook highlights in his top post. There's little doubt that during the glacial cycles of about the last million years or so, that CO2 concentrations tracked (and amplified) earth temperature changes that resulted from Milankovitch cycles. However it would be illogical to conclude from this that atmospheric CO2 levels respond to earth temperature changes in a more significant manner than earth temperatures respond to changes in CO2 levels. One could look at the last 1000 years for example [tiny changes in atmospheric CO2 during the temperature variations associated with the MWP and LIA, compared to the mach larger earth temperature rise in response to changes in (anthropogenic) CO2 levels)]. Likewise, inspection of the Phanerozoic temperature/CO2 record indicates that the Earth has responded in a very significant manner to changes in atmospheric CO2 levels. In fact the reason that we now inhabit an earth with very significant polar ice caps is the result of the decrease of atmospheric CO2 levels during the late Eocene/early Oligocene. Just because CO2 tracked earth temperature during a particular set of specific and rather well-understood climate phenomena (Pliestocene glacial transitions), it's illogical to conclude that earth temperature variations are the dominant cause of CO2 variations. In fact the evidence supports the opposite conclusion, namely that changes in greenhouse gas levels dominate earth temperature variations. We're experiencing an example of that during the present era.... -
RSVP at 09:14 AM on 11 January 2010Why does CO2 lag temperature?
chis From what I can tell from the curves above, CO2 tracks Earth temperature like a flea rides on an elephant. Its hard for me to be "less than logical" faced with something so obvious, but I guess you must have some kind of point. -
David Horton at 08:20 AM on 11 January 2010Why does CO2 lag temperature?
Interesting, I hadn't realised there was a considerable dating uncertainty in the ice record of CO2. I had assumed, because these are long continuous and fine-scaled records, that the dating was something equivalent to tree rings or mud varves. The error margin puts into perspective the constant refrain - "oh, but CO2 increase lags temp rise, how can it be cause and effect?" Seems to me that if there is an error margin on age, then the record should just be read as showing a very close (indeed astonishingly close as such things go) correlation between CO2 and temps over a very long time period as John's graph illustrates. Whether CO2 increase "leads" temp increase (as it is doing in modern times) or whether it is working as a feedback and amplifying mechanism seems irrelevant. Of no more than academic curiosity when we are considering the distant past. The close correlation shows that the two mechanisms are effectively just one, and that is the frightening conclusion as we continue to pump CO2 into the air in a never ending experiment to see just how far we can go before catastrophic change ensues. -
chris at 07:47 AM on 11 January 2010Why does CO2 lag temperature?
re #15, there's a less than logical element to your description of temperature>CO2 and CO2>temperature causalities RSVP. This relates to the likely accessible range of temperature and CO2 variations. So, in fact during glacial-interglacial transitions the global temperature change of around 5-6 oC results in a repartitioning of CO2 between the oceans/terrestrial environment and atmosphere equivalent to around 90 ppm (i.e. something like 15-18 ppm of atmospheric CO2 rise per oC of global warming at equilibrium). However the potential for CO2 rise from non-temperature-dependent repartitioning (e.g. from extraterrestrial impact into carbonate-rice sediments, or massive tectonic events like flood basalt release, or anthropogenic burning of fossil fuels) is much larger than the 90 ppm of [CO2] repartitioned to the atmosphere during glacial-interglacial transitions. So whereas a 90 ppm CO2 rise is near the limit of any realistic temperature-induced enhancement of atmospheric CO2 probably during the past 100's of millions of years, it is very easy for non-temperature-dependent drivers of [CO2] to push CO2 concentrations above 1000-2000 ppm (we could easily manage to reach 1000 ppm during the next 150 years). So in the real world, [CO2] variation is, and always has been, a major effector of global temperature variation, whereas global temperature change is a rather minor effector of atmospheric [CO2] variation. One could look at specific examples. During the Medieval Warm Period, atmospheric CO2 levels seem not to have risen more than a few ppm above pre-MWP levels. Now that likley means that the MWP didn't result in very much global scale warming. The drop in atmospheric CO2 during the Little Ice Age (LIA) from ~ 280-276 ppm was seemingly also very small. That's because the atmospheric CO2 levels respond to a rather small extent to changes in global temperature. On the other hand global temperatures are responding much more significantly to the raised anthropogenic CO2 levels. One can easily be fooled by numbers. It's not the magnitudes of the numbers, as such, that are relevant, but the accessible ranges of likely variation... -
chris at 07:20 AM on 11 January 2010Why does CO2 lag temperature?
re #14 Ian, the paper by Ahn and Brook that bobo cites [*] has a very intersting overlay of CH4 levels in Greenland and Antarctic cores, together with Greenland and Antarctic temperature proxies (delta 18-O2) and Antarctic CO2 levels (see Figure 1). Several things are striking (to me)...boba might have some further insight: 1. Within the last glacial period small variations in CO2 levels follow Antarctic temperature variation pretty faithfully, but the large CO2 rise at the termination from ~17000 to ~11000 years ago lags Antarctic warming quite markedly (as described in the top article). 2. Methane levels follow Greenland temperature variation very faithfully indeed, and are non-synchronous with Antarctic temperature change until the termination. The simple explanation would be that methane levels follow high N. latitude warming (perhaps associated with methsane release from tundra melt??). 3. This is very striking. The very sharp warming/cooling pulses in the Greenland cores associated (likely) with on-off shifts in the AMOC have totally synchronous sharp rises/falls of methane levels that are observed (synchronously) in Greenland and Antarctic cores. 4. At least within glacial periods, the slow CO2 rises and falls (of around 20 ppm over several thousand years) associated with slow Antarctic temperature rise and fall, occur well in advance of the methane spikes associated with Greenland warming spikes. That would imply that the enhanced CO2 is not a result of enhanced methane release and oxidation to CO2. Even during the termination where the Antarctic temperature rose rather steadily between ~20-10,000 years ago, the Greenland warming has a cold interval (Younger Dryas) which has a synchronous coincident drop in methane (observed in Greenland and Antarctic cores). So it really does look like methane levels match events in the N. hemisphere. J. Ahn and E. J. Brook (2009) Atmospheric CO2 and Climate on Millennial Time Scales During the Last Glacial Period Science 322, 83-85 http://www.sciencemag.org/cgi/content/abstract/322/5898/83 -
chris at 06:47 AM on 11 January 2010Why does CO2 lag temperature?
re #7 Andreas As I mentioned in the post above, there are some other scenarios that involve a more direct S. hemisphere response to Milankovitch-driven insolation changes. It does seem clear that glacial termination is driven by Milankovitch cycles; however Milankovitch driven insolation variation obviously applies to the S. hemisphere as well (see below). It’s likely that the AMOC underwent quite abrupt ice melt driven cessations (and re-establishments); it’s difficult otherwise to explain the sharp temperature drops/rises in the Greenland core (and their lack of appearance in the Antarctic cores). But whether these were active/causal or passive/responsive phenomena is still an open question I believe, ‘though I find the scenario outlined by Barker/Broecker (paraphrased in my post #6) plausible. And one could substitute the enhanced Westerly-driven Southern ocean-destratification mechanism that boba describes (Anderson et al, 2009; Toggweiler 2009 cited in boba’s post) as the warming-driven proximate cause of CO2-outgassing from the Southern oceans, within the same ultimate scenario of Barker/Broecker. In this case the Arctic melt-water induced weakening/shut-down of the AMOC warmed the Southern oceans at the expense of Northern latitude warmth, and shifted the Intertropical Convergence Zone southwards, pushing the Southern westerlies closer to Antarctica and “stirring up” the deep Southern oceans to promote CO2 release. Looking at the alternative proposals, Stott et al (2007) consider that the glacial terminations might be driven by direct Southern ocean ice sheet responses to austral spring insolation variation (Milankovitch), and that the warming-induced CO2 release from the Southern oceans transmits the warming to the N. hemisphere, to give the Antarctic warming > CO2 release > Greenland warming sequence at the terminations. Their plot of the Milankovitch variation of austral spring insolation varies in synch with the N. hemisphere summer insolation at 65 oC… ..and Huybers and Denton, consider that it is the Milankovitch-forced variation of the duration of the S hemisphere summer (which covaries with the Milankovitch-forced variation of the intensity of the N. hemisphere summer), that is important…. If I understand your last question (different phase patterns between insolation and warming) it could be that this is a result of different response of AMOC. Since the insolation variation is extremely regular (and predictable), any non-regular/variable consquences should have their origins in less predictable responses to the regular insolation variation. If the AMOC responds to ice-melt intensity, presumably this has rather non-regular features and will impose a more stochastic pattern onto the insolation-driven changes. But more generally, if (by whatever scenario), N. hemisphere warming is ultimately driven by CO2-release from the vast S. oceans in response to S. latitude warming/reduced S-N hemisphere temperature gradients, the very slow warming, with associated very slow CO release, may, by itself, result in a phase difference between insolation patterns, and warming responses. While there are still some issues with matching the timings exactly between Greenland and Antarctic cores, it seems clear that Antarctic warming precedes Greenland warming during terminations, and even during some of the periodic warming transitions within glacial periods…again variations in the AMOC seem to be implicated in these events… -
MarkJ at 04:47 AM on 11 January 2010Sea level rise is exaggerated
Re: 1 & 2 - I can't find much on Morner other than his Wiki page which suggests his work was often cited and though now seemingly discredited he must have once been a leading authority on sea level rises or the lack of them. He certainly claimed to be the best in the world in the external links to interviews from Wiki in which he rages about the IPCC bringing in modellers rather than sea-level experts. -
RSVP at 04:39 AM on 11 January 2010Why does CO2 lag temperature?
According to the graph presented here and in a previous article: http://www.skepticalscience.com/The-correlation-between-CO2-and-temperature.html (figure 2) a 10 degree change in Earths temperature causes a change of 90 ppm CO2, while a change of 60 ppm CO2 could possibly have partially effected 1 degree of change in the Earths temperature. This data indicates that temperature drives CO2 much stronger than CO2 drivers temperature. -
Ian Forrester at 04:03 AM on 11 January 2010Why does CO2 lag temperature?
Boba, interesting comments. I've always felt that CO2 coming from warming oceans didn't seem quite right from a simple chemistry view point (it seemed to me that it was unlikely that the oceans would be saturated because of various cycles). Have you considered that the increase in CO2 during deglaciation periods could be from methane released by the retreating ice and permafrost? The methane will then be oxidized both biologically and photochemically to CO2. -
boba10960 at 03:09 AM on 11 January 2010Why does CO2 lag temperature?
First I’d like to commend John for a great blog. This is a fabulous resource and your careful, thorough, and prompt explanations of new science papers is very impressive. Thanks! Temperature’s lead over CO2 in Antarctic ice core records keeps getting mentioned as proof against human impacts on climate, so it’s good to have an objective discussion of the issue. Here I present some additional perspective from the paleoclimate community I’m sorry this comment is so long, but it’s a complex issue. John - It seems that the link to Shemesh et al., 2002 is still broken. At least I get a damaged file. Presumably this is: Shemesh, A., Hodell, D., Crosta, X., Kanfoush, S., Charles, C. and Guilderson, T., 2002. Sequence of events during the last deglaciation in Southern Ocean sediments and Antarctic ice cores. Paleoceanography, 17(4): 10.1029/2000PA000599. Turboblocke - Henry’s law absolutely applies to CO2, as it does to all gases. The CO2SYS document from the CDIAC web site doesn’t support that claim. The main difference between CO2 and other gases is that once CO2 dissolves from air into seawater it undergoes further reactions, dissociating into bicarbonate and carbonate ions. This makes the chemistry of carbon dissolved in seawater complex, but CO2 gas still obeys Henry’s Law. Dennis, Riccardo - Yes, the uncertainty in the overall age model for an ice core gets larger further back in time, as does the uncertainty in the difference between the ages of gas and of ice at any given depth. For those who aren’t familiar, at any given depth in an ice core the ice is at least a few hundred years, and sometimes a few thousand years, older than the gas. This is because gases diffuse through firn (packed snow) before it is sealed off as ice. The age offset between gas and ice increases as the accumulation rate of snow decreases. Therefore, the ice-gas age difference is much greater during ice ages, when there is less snow accumulation, than during interglacials. Uncertainty in the ice-gas age difference has been a big problem in establishing reliable lead-lag relationships between temperature and CO2. People have done statistical analyses of gas-ice age differences, but the best statistics still produce meaningless results if the age models for ice and/or gas are inaccurate. This applies to the data set cited by Ari Jokimäki. Age models for ice cores are constantly being revised. See: Bénédicte et al., Consistent dating for Antarctic and Greenland ice cores. In Press, Quaternary Science Reviews, Available online 3 December 2009 The uncertainty between gas age and ice age can be virtually eliminated at glacial terminations (i.e., at the end of an ice age) when the initial warming is recorded by the isotopic composition of argon gas, which can then be compared directly against CO2 concentration. Since both temperature and CO2 come from the gas phase, there is no age offset in need of correction. This is how Caillon et al. 2003 (cited by John) was able to show that temperature started to rise in Antarctica before CO2 began to increase. This direct evidence is more robust in my opinion than the statistical comparison of CO2 and temperature on different age models, each with their own uncertainty. I think Caillon et al convinced paleoclimate scientists that the initial increase in temperature in Antarctica leads the initial rise in atmospheric CO2 at the end of an ice age by several hundred years. This leads to the main point that I wanted to make, namely: Why did temperature start to rise in Antarctica before concentrations of CO2 began to increase at the end of an ice age? Does this mean that CO2 does not have an impact on climate? Two hypotheses have already been described. I will summarize those and add a third. The first hypothesis invokes changes in earth’s orbit (Milankovitch) and its effect on spring insolation around Antarctica. Increasing insolation in spring is suggested to cause sea ice to melt back earlier in the year, which allows more CO2 to escape from the ocean to the atmosphere. A scenario like this was invoked by Shemesh et al. (2002) and would follow from the conclusions of Huybers and Denton (2008; cited by Chris). The general principles are described in a paper by Stephens and Keeling: (Stephens, B.B. and Keeling, R.F., 2000. The influence of Antarctic sea ice on glacial-interglacial CO2 variations. Nature, 404(6774): 171-174.). However, if you read the papers that comment on Stephens and Keeling, you will find skepticism in the paleoclimate community about whether or not sea ice can truly serve as a “lid” holding CO2 in the ocean. Second, Chris described a hypothesis that is commonly invoked for the sequence of events at the end of an ice age, namely: 1) Changes in Earth’s orbit (Milankovitch again) led to warmer summers in the Northern Hemisphere. 2) Warmer summers started melting the large northern ice sheets that built up during the ice age. 3) Freshwater from melting ice flowed into the North Atlantic. Because of its lower density, the freshwater slowed or stopped the overturning circulation that transports heat northward. 4) This had a global impact, but here some hypotheses diverge (denoted A and B below). According to the ocean bi-polar seesaw hypothesis described by Chris: A5) Reduced northward flow in the Atlantic allowed heat to build up in the Southern Hemisphere, a phenomenon known as the bipolar seesaw. A6) Warming of the Southern Ocean caused CO2 to be released from the ocean due to the lower solubility of gases in warmer water. Rising CO2 followed the initial warming of the Southern Ocean and of Antarctica, and also contributed to warming of the Earth as a positive feedback. (See Chris - Post 6, point 2c) A problem with this hypothesis is that the temperature dependence of CO2 solubility in seawater is well known, and the rise in ocean temperatures during deglaciation is not nearly large enough to have caused the observed rise in CO2. This was pointed out long ago by Broecker and others. The principle is firmly established in the scientific literature. Broecker, W.S., 1982. Glacial to interglacial changes in ocean chemistry. Progress in Oceanography, 2: 151-197. Something other than warming must have caused CO2 to be released from the oceans. This is why some people invoke the melting of sea ice to allow more CO2 to escape (see above). However, (a) as noted above, others have argued that sea ice is not sufficiently effective as a barrier to gas exchange and (b) changes in sea ice driven by orbital forcing cannot explain the tight correlation between CO2 and Antarctic temperatures on the millennial time scales that are shown in Figure 1 of: Ahn, J. and Brook, E.J., 2008. Atmospheric CO2 and climate on millennial time scales during the last glacial period. Science, 322(5898): 83-85. A third hypothesis not yet described in this thread of comments involves a reorganization of global wind systems toward conditions more favorable for mixing in the Southern Ocean that drives CO2 from the ocean to the atmosphere. The process begins as above, with changes in Earth’s orbit melting northern ice sheets and slowing Atlantic overturning circulation (Points 1 - 4). Then the emphasis switches from the ocean to the atmosphere: B5) When freshwater shuts down Atlantic overturning circulation, winter sea ice expands over the North Atlantic, causing severely cold winter conditions. B6) Cold winters cause changes in atmospheric circulation, which are well documented for the Intertropical Convergence Zone and for the Asian Monsoons (see Cheng et al., 2009, cited by Chris, and references therein). B7) Reorganization of the winds extends all the way to Antarctica, strengthening the Southern Hemisphere westerlies so that they are more effective at driving CO2 out of the ocean. According to this hypothesis, intense cooling in the northern hemisphere causes warming in the southern hemisphere by changing wind patterns. The initial warming in Antarctica is caused more by a redistribution of heat from north to south than by a global rise in temperature. The winds then drive CO2 out of the ocean so that the observed rise in CO2 lags slightly the initial warming detected in Antarctic ice cores. It takes a few thousand years to melt the northern ice sheets. During this time when meltwater is being dumped onto the North Atlantic, the winds are shifted and CO2 is being driven out of the Southern Ocean. These conditions can experience brief reversals, as happened 14,500 years ago during the Bolling period. After the Bolling warm period, the conditions resumed during the Younger Dryas period. Increased atmospheric CO2 together with reduced albedo following the meltback of the northern hemisphere ice sheets provided the feedbacks to Milankovitch forcing that brought the earth out of the last ice age into a warmer interglacial period. The principles underlying the forcing of CO2 by shifting winds over the Southern Ocean are described by Toggweiler (2006). Evidence to support the principles, but modifying the timing, are described by Anderson (2009). See also comment by Toggweiler (2009). Toggweiler, J.R., Russell, J.L. and Carson, S.R., 2006. Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages. Paleoceanography, 21(2): doi10.1029/2005PA001154. Anderson, R.F., Ali, S., Bradtmiller, L.I., Nielsen, S.H.H., Fleisher, M.Q., Anderson, B.E. and Burckle, L.H., 2009. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2. Science, 323(5920): 1443-1448. Toggweiler, J.R., 2009. Shifting Westerlies. Science, 323(5920): 1434-1435. These hypotheses all need to be investigated further. Each has strengths and weaknesses. Given the complexity of Earth’s climate system and its connection to the global carbon cycle, the correct answer is likely to be “all of the above”. -
Paz at 00:43 AM on 11 January 2010What happened to the evidence for man-made global warming?
- Satellites measure less infrared radiation escaping out to space at the wavelengths that CO2 absorb energy (Harries 2001, Griggs 2004, Chen 2007) - Surface measurements find more infrared radiation returning back to the Earth's surface (Philipona 2004), specifically at the wavelengths that CO2 absorb energy (Evans 2006) I think these two arguments are very strong. What would be the clincher, however, is if the radiation loss going outward and radiation increase going back onto the surface where mathematically equivalent to the energy increase in the athmosphere. Are you aware of any such calculation? The argument would be problematic if, for instance, the increased radiation back would be much less than the increase in temperature. -
Alexandre at 22:40 PM on 10 January 2010Can you make a hockey stick without tree rings?
The only link that worked for me here was Oerlemans'. Is it just me or have the links indeed been moved? Another question: why does the Mann graph show a 0.8+ degree warming after de mid-century pause? Shouldn't it be some 0.5ºC? -
MarkJ at 22:14 PM on 10 January 2010What ended the Little Ice Age?
Thank you for an excellent post Chris. John your site is a wonderful model of how knowledgeable lay people and scientists should interact with ordinary inquisitive folk such as myself whose initial approach to the subject is skeptical. -
Ari Jokimäki at 20:07 PM on 10 January 2010Why does CO2 lag temperature?
Dennis, you are correct that there is large uncertainty in measurements, and there is additionally the fact that datapoints for carbon dioxide are typically separated by thousands of years which adds to the measurement uncertainty. This leads to the situation where you can't usually say on individual moments for sure that there's temperature leading. However, the lead/lag situation has been determined statistically from the whole datasets, not from individual events. So, I would say that the temperature leading is real phenomenon but we can't rule out that there might be some individual events where CO2 leads. Here's an example data for carbon dioxide (from Vostok ice core) where you can get the feel of the thing yourself: http://cdiac.ornl.gov/ftp/trends/co2/vostok.icecore.co2 -
Marcus at 17:50 PM on 10 January 2010Hockey sticks, 'unprecedented warming' and past climate change
I have a few relevant points to add here. On my reading of Jared Diamond's book "Collapse" (highly recommended read I might add), there are 3 civilizations whose collapse is consistent with a warming period between the 7th & 14th C AD. The Khmer Empire, the Mayans & the Anasazi all declined/collapsed around the same time, & all the Paleo-climatic data from the respective areas (especially sediment cores from lake beds & coastal regions) show that there was definitely a warming event which triggered/accelerated the decline of these civilizations. So we do have fairly reasonable evidence of warming-induced collapses of civilizations from the low N. Hemisphere & Tropical S. Hemisphere. What is interesting, though, is this-the warming events are believed to have been on the order of +0.5 to +0.8 degrees, but occurred over a period of almost *seven hundred years*. Secondly, solar activity proxies for that time period (Be-10 & C-14) suggest a surge in solar activity not unlike what we saw during the 19th & early 20th centuries. So this again leaves us with the fact that the current warming period is *faster* than any other in the last 2000 years (at least), & is the only one not underpinned by changes in the heliosphere. -
Doug Bostrom at 15:34 PM on 10 January 2010Is the airborne fraction of anthropogenic CO2 emissions increasing?
I'm not sure if I'm witnessing the conception of a new misconception or just a "rebunking" (hat tip to Hank Roberts) but ralphiegm's constant repetition of problems with C02 measurements sure sounds like a launch to me. ralphiegm, all of the measurement sites you worry over show a steady increase in C02 content. How would the poor mixing you imagine comport with that? Is each site measuring a hermetic local atmospheric cell with its own C02 sources? For instance, what about the grandpa site, Mauna Loa? Is Hawaii stuck in a persistent gyre, with the atmosphere isolated from the rest of the world? Does the C02 measured at that site originate just within Hawaii? Or does the imaginary bubble extend to Midway? Japan? San Francisco? Where does the C02 in the contrail of a jet flying to Hawaii make the transition from one magical domain to another? Is there a mysterious atmospheric atomic and molecular sieve at play here, unknown until now but identified via proxy only by you? Remember Chernoybl? Remember how it was detected outside of the Ukraine? How about those radionuclides, hmm? Did the the sieve remove Ukrainian C02 prior to crossing the border? Speaking of isotopes, how about the C02 isotope distribution? Does each mysterious atmospheric bubble include a special synchronizing system so that even while mixing does not take place, isotope ratios are kept at the proper proportion across domains? Wait a minute. Maybe it's more reasonable to accept that the atmosphere is mixed. I dunno. What do you think? -
Marcus at 14:59 PM on 10 January 2010Is the airborne fraction of anthropogenic CO2 emissions increasing?
I concur Ned. Ralph's comments about CO2 varying by +/- 200ppm sound very reminiscent of the results of the Beck "paper". Ralph's coyness about his knowledge of Beck actually *confirms* that this is his primary source (methinks he doth protest too much). Beck's collection of historical CO2 samplings ignores the poor quality of both the sampling sites, the measurement methods & the sensitivity of the measurement tools-all of which are suspect. For a very good analysis of Beck's data-I suggest going here: http://www.realclimate.org/index.php/archives/2007/05/beck-to-the-future/ Oh, & before Ralph accuses me of merely trying to "squeeze out skeptics"-that claim is simply *not true*. I just want to squeeze out BAD SCIENCE! That's as true of Beck as it is of Manne (he of the awful Hockey-stick. I mean, seriously, what kind of *scientist* uses a single, dubious source of paleo-climatic information & builds a paper round it?) By contrast, though it has still to be independently verified, Lindzen's hypothesis regarding "The Iris Effect" is based on quite sound scientific principles (yes, I have read the paper, & understand enough of it to make this judgment)-even though Lindzen is a noted Skeptic. -
Riccardo at 10:12 AM on 10 January 2010Why does CO2 lag temperature?
Dennis, the uncertainty on lag of CO2 is of the order of some centuries, not thousands of years. The precision in the absolute dating of the air bubles depends on many factors, including accumulation rate and temperature, so it strongly depends on the geographic location of the ice core. Whenever possible the dating of the ice core (or part of it) is calibrated using known and well defined events. -
Turboblocke at 09:38 AM on 10 January 2010Why does CO2 lag temperature?
Henry's Law is not appropriate for the solubility of CO2 in sea water. See here for more details: http://cdiac.ornl.gov/oceans/co2rprt.html -
Dennis at 08:34 AM on 10 January 2010Why does CO2 lag temperature?
Non-scientist asking a scientific question here. The chart showing CO2 and temperature changes for the past 400,000 years shows CO2 lagging. I would assume that the level of uncertainty in our measurement of the number of years increases as we increase the number of years we go back in time. For example, we can confidently compare data that's measured decades back, but I would suspect that thousands of years back (as we see above) have a much greater margin of error. This would suggest to me that CO2 may not lag temperature and may even be a driver in the increase. What data disproves that and why can we be confident with that? My thinking is that, e.g., while we may say that a particular ice core sample used to measure CO2 is 400,000 years old -- perhaps that plus or minus 10,000 years? -
stevecarsonr at 07:04 AM on 10 January 2010Why does CO2 lag temperature?
One of the papers in the link above to papers on Milankovitch cycles (link at end of article) argues that the relationship between ice ages and the Milankovitch cycles is very weak and doesn't really explain anything. "Quantitative estimate of the Milankovitch forced contribution to observed Quaternary climate change", Wunsch 2004 -
Andreas at 06:20 AM on 10 January 2010Why does CO2 lag temperature?
chris: Thank you, that was interesting. So that will imply a local negative feedback mechanism related to warming in the NH, but which on the global scale just rearranges heat so that the SH warms even more. I have heard elsewhere about the see-saw NH/SH pattern, the explanation you provide seems quite plausible. What you are arguing, I take it, is that the insolation at 65N is the most interesting in order to predict milankovitch-related warming even at the SH, due to circulatory mechanisms such as the AMOC. That is also what I after some doubt assumed in my post, so I do appreciate that argument. (although I'm not sure how the milankovitch-related insolation varies depending on latitude, or if it does it in a way that is at all significant on the timescales in question here. This might even be a non-issue?). However, do you suggest that differences in how the AMOC responds to insolation changes may explain why we see different phase patterns (between insolation and warming) at the different warming periods present in the vostok ice core data? Or are we still clueless on that account? -
Riccardo at 05:19 AM on 10 January 2010It's cooling
selti, i'm afraid you didn't even bother to look at how a cycle is define and identified from the links i gave you. Indeed, statistics is no joke, just looking at a couple of up and downs does not define a cycle. It looks like you are following a pre-defined idea and do not care of contrast it with science. Do you have any physical _and_ statistical reason to claim that there is a cycle, other than looking at a couple of up and downs? -
selti at 05:19 AM on 10 January 2010It's cooling
#21 Tom Dayton. Sooner than later, it will be established that CO2 driven global warming is the greatest scientific stuff up of all times. The stuff up is caused by assuming the temperature rise from 1970 to 2000 was unprecedented. Actually, as shown in this oscillating anomaly, this rise in temperature is similar to those at the end of 1880s and 1940s. Once the oscillating anomaly reaches its maximum it reverses and the cooling phase starts. -
chris at 03:48 AM on 10 January 2010Why does CO2 lag temperature?
Andreas, the answers to your good questions haven’t been worked out yet, but recent research provides some very plausible (in my opinion!) scenarios. One of the most powerful hypotheses for providing insight into climate variation on centennial, millennial, and the longer timescales relevant to Milankovitch cycles is the variations in the Atlantic Meridonial Overturning Circulation (AMOC), the most well know aspect of which being the Gulf Stream, that transports heat from the equator to the high Northern latitudes. There is evidence that changes in the intensity of the AMOC made contributions to the Little Ice Age and the Medieval Warm period, both episodes (especially the MWP) having indications of a “focus” in the high N. latitudes. It’s easy to see that if the AMOC is strengthened (weakened), heat transfer to the high N latitudes in enhanced (reduced). The evidence indicates that variations in the AMOC may have been very dramatic in the past, and recent studies support a role for this in ice age terminations and the anomalous differences in the N and S hemisphere responses to Milankovitch insolation variations that you refer to in your post. The idea is as follows: 1. The AMOC [*] can (in principle) be completely “switched off” by large scale melt of Arctic ice, which dilutes the cooling dense high salinity portion of the current as it sinks in the high Atlantic regions between ~ Greenland-Iceland - after having left some of its heat to the grateful occupants of the Western European fringes! [*]http://en.wikipedia.org/wiki/Thermohaline_circulation Weakening, or cessation of the AMOC results in cooling of the high Northern latitudes, but warming of the S. hemisphere, since less heat is transferred northwards – it remains in the S hemisphere and low latitudes. This is a likely explanation for a large amount of data that supports a northern, southern hemisphere bipolar “see-saw”, where evidence from ice cores, for example, shows an asynchronicity in temperature variations between Greenland and Antarctica. Likewise, temperature reconstructions from ice cores, shows (in Greenland cores) some extremely abrupt large scale temperature rises and falls (due likely to switching on and off of the AMOC), which are barely visible or highly damped in Antarctic cores. 2. The “see-saw” is apparent in glacial terminations, and a detailed examination was recently published in Nature [**] (a good commentary accompanies the article [***]). The progression of events is proposed to be: a. The gradual Milankovitch-induced change in summer insolation at 65 oN resulted in retreat of the N. ice sheets, lowered albedo and enhanced high NH warming, which is observed in Greenland (but not really in Antarctic) cores between around 21000-19000 years ago. b.The meltwater from this ice sheet retreat is proposed to have switched off the AMOC (as in 1. above) about 18000 years ago, switching the bipolar “see-saw” to its “warm-south” mode, resulting in significant Antarctic and Southern ocean warming (observed in Antarctic cores). c. The warming of the Southern oceans resulted in a lagged release of CO2, which produced slow warming on a global scale, which promoted N. hemisphere ice retreat, the melt-water from which kept the AMOC in its “warm-south” mode, increasing CO2 further, and driving the termination towards completion. d. It’s thought that the AMOC switched on again around 14700 years ago where there is an abrupt rise in temperatures in the Greenland cores, and a slower cooling in the Antarctic cores, and the termination was effectively brought to completion by as combination of high insolation, high CO2, reduced albedo and the resumption of massive heat transfer to the high N. latitudes by the resumption of the AMOC. That scenario (there are other possible explanations [****]) provides an explanation of how Milankovitch insolation changes manifest largely in the high Northern latitudes can result in glacial terminations that seem to be led by events in the Southern hemisphere. [**] Barker S et al. (2009) Interhemispheric Atlantic seesaw response during the last deglaciation Nature 457, 1097-0111 http://www.nature.com/nature/journal/v457/n7233/abs/nature07770.html [***] Severinghaus, JP (2009) Southern hemisphere see-saw Nature 457, 1092-1094 [****] Stott et al. (2007) Southern hemisphere and deep-sea warming led deglacial atmospheric CO2 rise and tropical warming Science 318, 435-438 linked in John Cook’s top article [****] e.g. H. Cheng et al. (2009) Ice Age Terminations Science 326, 248 – 252 http://www.sciencemag.org/cgi/content/abstract/326/5950/248 P. Huybers & G. Denton (2008) Antarctic temperature at orbital timescales controlled by local summer duration Nature Geoscience 1, 787 – 792 http://www.nature.com/ngeo/journal/v1/n11/abs/ngeo311.html E. W. Wolff et al. (2009) Glacial terminations as southern warmings without northern control Nature Geoscience 2, 206 – 209 http://www.nature.com/ngeo/journal/v2/n3/abs/ngeo442.html -
Tom Dayton at 03:40 AM on 10 January 2010It's cooling
selti: Look at the forest, not the individual trees. -
selti at 02:34 AM on 10 January 2010It's cooling
#18 Tom Dayton What I am comparing is the data after 2005. For all the data points after 2005, the actual anomaly measured observations are BELOW the anomaly projections with CO2 restricted at the 2000 level:Year Measured (deg C) Projections (deg C) 2005 0.47 0.45 2006 0.42 0.47 2007 0.40 0.48 2008 0.33 0.52 -
selti at 02:23 AM on 10 January 2010It's cooling
#18 Tom Dayton What I am comparing is the data after 2005. For all the data points after 2005, the actual anomaly measured observations are BELOW the anomaly projections with CO2 restricted at the 2000 level: Year Measured (deg C) Projections (deg C) 2005 0.47 0.45 2006 0.42 0.47 2007 0.40 0.48 2008 0.33 0.52 As a result, the IPCC projections are utterly wrong. -
Tom Dayton at 01:42 AM on 10 January 2010It's cooling
selti, your link "The IPCC projections are deadly wrong" is to an IPCC chart whose ranges of model runs (the shaded areas) and the observed data (the black dots and line) go up only to 2005. The black line for HADCRUT3 observed temperatures smoothed has been extended beyond that not by the IPCC, but by someone who modified (doctored, faked, falsified, as in Elvis with Bigfoot) the graph but adding an unsmoothed line! Perhaps the added black dots after 2005 really are the observed anomalies, but the line's extension is not smoothed across the dots! The resulting and false impression is that the smoothed line dove after 2005. The actual smoothed line makes a much shallower dip after 2005, especially if you add 2009 data. If you want to look at smoothed data then you must smooth it all the way from 1990 through 2008. If you want to look at unsmoothed data then you must look at unsmoothed data across all years, by ignoring the black line and just looking at all the black dots starting in 1990 and going up through 2008. If you want to draw a line from dot to dot you must do so for all the dots starting in 1990, not just starting in 2006. You must also look at either the line or the dots within the range of projections (the shaded areas) beyond 2005. That is shown on RealClimate in the post Updates to Model-Data Comparisons. Guess what? Observations are within the bounds of the projections! -
Andreas at 01:10 AM on 10 January 2010Why does CO2 lag temperature?
Is it possible to know in detail how the Milankovitch cycle affected temperature in the past? Analogously to comparing the phases of the temperature and CO2 cycles, it should be possible to do the same involving the milankovitch cycles. This picture from wikipedia show the milankovitch-related insolation at 65 deg north superpositioned on proxy temperaures from the vostok (Antarctica) ice core: http://en.wikipedia.org/wiki/File:Vostok_420ky_4curves_insolation.jpg 65 deg north is far from Antarctica, but assuming that it is globaly relevant (lowest-albedo latitude?) I tried a comparision of the cycles based on the picture. In the picture we see four major temperature/CO2 peaks, at roughly 320k, 230k, 120k and 1k years from now. Looking on the lowest temperature dips before these peaks (the points where the respective warmings starts) I read that two oldest dips (at -340k and -245k years) actually coincides with peaks in insolation, each followed by a period where the insolation (at 65N) declines but the temperature (in the antarctic) rises. In these cases the temperature trends does not start to decline until we have reached the insolation's next local minimum. This would possibly indicate that the milankovitch cycle can only explain the onset of the warming, leaving the rest to be explained by CO2 only. However, this does only hold for two of four warming periods that we can see in the core (the others being more in phase with the milankovitch cycles), Antarctica is not near the 65N latitude, and I do not know how the milankovitch-related insolation varies globally (apart from 65N). Are there better models on how the fluctuations in insolation due to the milankovitch cycles affects the southern hemisphere, and antarctica in particular, more specifically? In that case such models would be a better starting point. -
chris at 01:05 AM on 10 January 2010What ended the Little Ice Age?
My feeling is that the LIA and its ending are more straightforward. Some points: 1. Meehl et al don’t really address the end of the LIA. They address attributions to global warming since the mid-19th century, and the evidence indicates that the LIA had pretty much ended by then (see 5). 2. In relation to Meehl et al., since their paper was submitted, there’s been a pretty substantial re-evaluation of the solar contribution to temperature variation of the last several hundred years. The scientists that study solar outputs and its proxies (Lean, Foukal, Solanki), indicate that the contribution of enhanced solar output since the Maunder Minimum (MM; bottom of the LIA) to the mid-20th century is around 1-1.4 W/m2, equivalent to a warming at equilibrium of up to 0.2 oC [*]. This is a bit more than the Svalgaard estimated that DeNihilist refers to in post #3 above, but I find it hard to believe that a pretty well established surface warming/cooling contribution of ~ 0.1 oC through the solar cycle, doesn’t indicate that the complete absence of sunspot activity through a few cycles at the time of the MM wouldn’t have been associated with a cooling effect of at least 0.1 oC. 3. Referring to Meehl et al again, a more recent attribution study of natural and anthropogenic contributions to global temperature since the mid 19th century, indicates that all natural contributions (solar included) have produced essentially zero nett contribution since the mid-19th century. This study (Ammann et al. (2007) [**], is very similar to Meehl et al in its methodologies, but uses the more up to date solar parameterizations. 4. If one examines CO2 levels through this period [***], the atmospheric CO2 levels rose from around 276 ppm at the bottom of the LIA to 300 ppm by 1900 to 310 ppm by 1940. It’s likely that the small reduction of CO2 from the pre-LIA values near 280 ppm to 276 ppm was the atmospheric response to reduced temperatures (as discussed on the “Why does CO2 lag temperature” current thread). But the 280-310 ppm rise is anthropogenic and should give a global equilibrium temperature rise of 0.3 oC by 1900 and 0.45 at 1940 values (assuming the medium value of the climate sensitivity of around 3 oC of surface warming per doubling of atmospheric [CO2]. Since this occurred over a long time, we’d expect quite a lot of this to have been “realized” by the mid 20th century (say 0.35 oC). 5. So what ended the LIA? If you look at the most variable temperature reconstruction (Moberg et al, 2005 [****]; a N. hemisphere one, remember), the temperature anomaly was around -0.4 oC (relative to mid 20th century values) for several hundred years before the Medieval Warm Period (MWP), rose to around 0.0 oC at the height of the MWP, and then dropped to near -0.7 oC between around 1100 AD and 1600 AD at the bottom of the LIA. So recovery from the LIA really constitutes recovery from an anomaly of -0.7 oC back to the pre-industrial -0.4 oC (it helps to look at Moberg’s reconstruction!). This was largely a recovery of the solar irradiance (say 0.2 oC, and from the enhanced volcanic activity that likely made a small contribution to LIA cooling – say 0.1 oC). 6. So there are really two questions: What caused the recovery from the LIA? …. and What has caused the marked warming during the last 150 years. Considering the total (NH) temperature rise from the bottom of the LIA to the mid 20th century (~ 0.7 oC, and to now (~ 1.2 oC), I’d say the evidence is consistent with around 0.3-0.4 oC of natural “recovery” which was largely realised by the mid 19th century, and ~0.3-0.4 oC of anthropogenic contribution up to the mid 20th century, and more like 0.7-0.9 oC anthropogenic contribution to the present, with some of the natural and anthropogenic contribution “offset” by anthropogenic aerosols. [*] Y.-M. Wang, J. L. Lean and N. R. Sheeley, Jr. (2005) Modeling the Sun's Magnetic Field and Irradiance since 1713 Astrophysical J. 625 522-538 P. Foukal, G. North, Tom Wigley (2004) A Stellar View on Solar Variations and Climate Science 306, 68-69 Lean, J. L., and D. H. Rind (2008), How natural and anthropogenic influences alter global and regional surface temperatures: 1889 to 2006 Geophys. Res. Lett., 35, L18701 http://www.atmosp.physics.utoronto.ca/~jclub/journalclub_files/LeanGRL2008.pdf [**] C. M. Ammann et al. (2007) Solar influence on climate during the past millennium: Results from transient simulations with the NCAR Climate System Model Proc. Natl. Acad. Sci. USA 104, 3713-3718 http://www.pnas.org/content/104/10/3713.abstract (open access – so should be downloadable from this link) [***][ D. M. Etheridge et al (1996) "Natural and anthropogenic changes in atmospheric CO2 over the last 1000 years from air in Antarctic ice and firn J. Geophys Res. 101, 4115 -4128 [****] A. Moberg et al. (2005) Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data Nature 433, 613-617 coast.gkss.de/staff/storch/pdf/moberg.nature.0502.pdf
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