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All IPCC definitions taken from Climate Change 2007: The Physical Science Basis. Working Group I Contribution to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Annex I, Glossary, pp. 941-954. Cambridge University Press.

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Comments 120451 to 120500:

  1. Skeptical Science Housekeeping: flags, printable versions, icons and links... lots of links
    I notice that of the 18 "skeptic" articles or media stories from the last month, over half (10) are from Fox News(3), Daily Telegraph(3), Daily Mail(2) and the Washington Times(2). These organisations have a well-known political tilt. Two other organisations share that tilt, the Wall Street Journal and the Australian, which published 1 "sceptic" story each. Now, can anyone tell me if these were balanced with "positive" stories about climate science? I thought so.
  2. Skeptical Science Housekeeping: flags, printable versions, icons and links... lots of links
    Looking forward to the Android app. The peer reviewed feature is great, though I notice that the classification isn't 100%. For instance, one of the 'peer reviewed pro-AGW' items is a BBC blogger sounding off about how the 'evils of Climategate' are being whitewashed. On the flags, I'd suggest translating the tooltips into the relevant languages. "View skeptic arguments in Portugese" isn't much help to someone who doesn't speak English and might not recognize the flag of Portugal, but speaks the language... like say, most of Brazil.
  3. Models are unreliable
    Riccardo Alright, thank you Riccardo. That totally cleared the things for me.
  4. Philippe Chantreau at 01:29 AM on 23 April 2010
    The significance of past climate change
    Ther has not been a D.O. event for over 20000 years. Of all the known Bond events, only a small fraction had the potential to affect climate. They seem to lead to an opposite change in the other hemisphere, a phenomenon that has been dubbed the "bipolar see-saw." All in all, the resemblance with what's happening now is so poor as to be irrelevant. All that has already been discussed and referenced on this site before.
  5. The significance of past climate change
    I'm not clever enough to spot that kind of game unless I know the participants well enough. It occurred to me that Tom was being facetious. But it's better to assume straightforwardness if you're not sure when chatting amongst unfamiliars. Wasn't going to comment about that, but seeing as you mentioned it Chris... On another note, I find the reactiveness to skeptics a bit disappointing at times. Don't get me wrong, I've been as frustrated as hell quite often and been pretty abrupt, but I've lately seen well-meaning questioners mobbed with vitriol. I also hope that erstwhile obstinate interlocutors in these climate debates might eventually modify their approach, if not their doubts, if the door remains open. I ask myself "what's my purpose here" and try to operate as if the answer is meaningful. And I'm basically sick to death of the Punch and Judy. Seems to me it achieves the opposite of what is wanted (unless slap-downs are a turn-on for you). That's Nana's lecture for the year. Now back to our feature presentation.
  6. Models are unreliable
    cloneof, the video is a sort of short version of the paper. He calculated a possible cause of error in empirical sensitivity estimates based on random variability of some internal forcing factor. Tuning the variability with just satellite tropical data he found a lower climate sensitivity than the global sensitivities obtained by various GCMs. This is all it has to do with models, Spencer compares his sort of "tropical sensitivity" with GCMs. While the effect of random variability on short term empirical estimates of the sensitivity might in principle make sense, it does not make any sense when he compares his tropical sensitivity with GCMs. This paper is on the very same track of the more recent (and wrong) Lindzen and Choi 2009 paper, similar wrong reasoning that they sell as the definitive proof.
  7. The significance of past climate change
    Tom, I meant no disrespect to BC, and I firmly believe that he gives an honest opinion. Above, I had presented the argument that there is a tendency in engineers, when you present information that only makes sense if something they have been assuming is a constant, is in fact a variable, they don't believe what you are telling them. BC, describing himself as an engineer, reported that he balked upon reading something that only made sense if the solar output was not constant, and then came to the incorrect conclusion that John was talking about changes related to earth's attitude or position. That follows very closely with the example I gave above.
  8. The significance of past climate change
    @Berényi Péter at 22:56 PM on 22 April, 2010 #21 chris at 00:05 AM on 22 April, 2010 they [Dansgaard-Oeschger events] are not representative of global warming/cooling events Think again. PNAS online Ice-core evidence of abrupt climate changes Richard B. Alley I don't think your reference quite supports what you're intending. For example: Geographic Coverage. The ice-core record of abrupt climate changes is clearest in Greenland. No other record is available that spans the same time interval with equally high time resolution, complicating interpretations. It appears, however, that ice cores from the Canadian arctic islands, high mountains in South America, and Antarctica contain indications of the abrupt changes. Dating is secure for some of the Antarctic cores. The Canadian arctic cores show a sharp cold reversal during the deglaciation that is probably the Younger Dryas event (29). Ice cores from the high peaks of Huascaran and Sajama in the Andes also show a deglacial reversal in the ice isotopes that may be correlative with the Younger Dryas (2, 30). However, for various reasons, the exact timing and abruptness of the changes are difficult to ascertain in these records, and records of older abrupt changes are even less secure. In Antarctica the Byrd core from West Antarctica, and probably the Vostok and some other cores from East Antarctica, show events that are correlative to the larger millennial events of Greenland, including the Younger Dryas (6, 31). Byrd and Vostok also contain indications of events that may be correlative to nearly all of the Greenland events (31). However, the ice isotopes indicate an antiphase behavior, with Byrd warm during the major events when Greenland was cold; dating control is not good enough to determine the phase of the smaller events. The general impression of the Antarctic events is that they are smaller and less abrupt than those in Greenland, although fewer paleothermometers and other indicators have been brought to bear in Antarctica, reducing confidence somewhat. To further complicate the issue, the Taylor Dome core from a near-coastal site in East Antarctica appears to be in-phase with Greenland and out-of-phase with Byrd during the deglacial interval centered on the Younger Dryas (32). As reviewed in ref. 33, non-ice records from broadly distributed sites in the Northern Hemisphere indicate large, abrupt changes (near-)synchronous with those in Greenland, with generally cold, dry, and windy conditions occurring together although with some sites wet perhaps because of storm-track shifts (cf. ref. 28). Some Southern Hemisphere sites also exhibit the Greenland pattern during the deglaciation, although high-resolution (annually resolved) southern records are still lacking. However, southern sites near and downwind of the south Atlantic show an anti-Greenland pattern with millennial warming when Greenland cooled, superimposed on the slower orbital variations, which are broadly synchronous in both hemispheres. Sudden 'climate change' is probably regional. Global climate change is clearer in the long-term. The last sentence in the reference reads:
    Abrupt changes have been especially large when atmospheric carbon-dioxide concentration, insolation, and other important climatic variables were changing rapidly, with possible implications for general behavior of the climate system.
  9. Skeptical Science Housekeeping: flags, printable versions, icons and links... lots of links
    "So this allows you to check out all the skeptic peer-reviewed papers published in the last month. Or if you want to keep up with current views, check out the skeptic articles published in mainstream media over the last week." Both the links are to the same (mainstream media) list.
    Response: Oops, fixed, thanks!
  10. Skeptical Science Housekeeping: flags, printable versions, icons and links... lots of links
    Wow! I thought this site was pretty good when I first came across it. Now I am pretty much blown away by how much detail and depth of resources are here. Thank you again John for putting this all together, and thanks to those who help with the features of the site and to all those who contribute to the discussions. It has given me a much better understanding of just what is happening. Though some of the discussions are way out of my league I appreciate the effort to make this site comprehensible to all knowledge levels.
  11. Berényi Péter at 23:42 PM on 22 April 2010
    Tracking the energy from global warming
    #65 Ken Lambert at 23:04 PM on 22 April, 2010 Can you explain Of course I can. However, I think I have already explained it, just give it some thought on top of reading sentences. The two TOA curves are essentially the same. The difference is a linear trend with a slope. The reason behind it is that TOA fluxes as measured by satellites (recently CERES mission) have large sytematic errors but reasonable interannual precision. At least as long as instrumentation does not change much and intercalibration issues are resolved. On the other hand, net TOA flux should be very close to proportional to the time derivative of OHC, because there is no other heat reservoir in the climate system with comparable storage capacity. Rapid large scale (back & forth) heat exchange between the upper 700 m of oceans and the abyss has no know mechanism, turnover time being several millenia. If climate system heat content is calculated from net TOA fluxes, only the second derivative is measured by CERES with reasonable accuracy, therefore heat content history has a free additive linear term. With OHC, on the other hand, the temporal inegral itself is measured. What I did was to choose the free term for best fit. It can be done for the last six years, but not before first half of 2003. This is the same period when ARGO float deployment was still at an early stage with poor global coverage and rather few floats compared to the target of 3000. At the same time older systems were already phased out almost completely.
  12. Models are unreliable
    Riccardo I was going to write about the paper, but I actually found a good video where Spencer explains hi's paper. And at least he gives the impression that it is supposed to do something about climate models. http://www.youtube.com/watch?v=LpFk0zTW-ik
  13. Tracking the energy from global warming
    BP #60, #62, #64 I forgot to add - the NODC OHC data in your charts is only the top 700m of the oceans, Yes? If so, the hot topic is what is happening in Dr Trenberth's deeper oceans down to 2000m and beyond. With an average ocean depth of 3700m - there seems plenty of un-explored depth for more 'hidden heat' or is it 'hidden cold'.
  14. Skeptical Science Housekeeping: flags, printable versions, icons and links... lots of links
    I am assuming that the paper you are referring to was listed as a "skeptics paper" because it is one that could be used by the deniers given their tendency to re-interpret peer reviewed research to fit their preconceived notions. In the case of the above referenced paper, the deniers could reinterpret the findings along the lines - "because this paper shows that CO2 warming can not account for a significant amount of the observed warming, the models must be wrong and none of the warming is caused by increased CO2 levels."
  15. The significance of past climate change
    Chris G and barry, I believe you misunderstood BC's intent. He was helping John by giving his knee-jerk reactions, to simulate an audience's immediate reactions upon seeing the slide presentation, to help John revise his slides to keep that audience engaged and on track.
  16. The significance of past climate change
    Chemware, Barry, I believe Hansen et al cover this topic to some extent in "Target Atmospheric CO2: Where Should Humanity Aim?" http://arxiv.org/ftp/arxiv/papers/0804/0804.1126.pdf
  17. The significance of past climate change
    When the sun gets brighter - I baulked at this as my immediate reaction was that you are saying that the sun is emitting more energy. (With thought, I accept that your statement is correct because the sun gets brighter from our perspective because it's closer or the earth is differently tilted due to the Milankovic cycles) As I understand it, our sun has been getting hotter over the aeons. It's not a cyclical process.
    Even during its current life in the main sequence, the Sun is gradually becoming more luminous (about 10% every 1 billion years), and its surface temperature is slowly rising.
    http://en.wikipedia.org/wiki/Sun
    In the long term, the greatest changes in the Solar System will come from changes in the Sun itself as it ages. As the Sun burns through its supply of hydrogen fuel, it gets hotter and burns the remaining fuel even faster. As a result, the Sun is growing brighter at a rate of ten percent every 1.1 billion years.
    http://en.wikipedia.org/wiki/Formation_and_evolution_of_the_Solar_System
    The continuous fusion of hydrogen into helium will cause a build-up of helium in the core. The rate at which this process occurs depends on the initial mass of the star and ranges from millions to billions of years. Larger, hotter stars produce helium more rapidly than smaller, cooler ones. The accumulation of helium in the core causes a gradual increase in the rate of fusion and gravitational self-compression, as helium is denser than hydrogen. Higher temperatures must be attained to resist this increase in gravitational compression and to maintain a steady state. Eventually, the core exhausts its supply of hydrogen, and without the outward pressure generated by the fusion of hydrogen to counteract the force of gravity, it contracts until either electron degeneracy becomes sufficient to oppose gravity or the core becomes hot enough (around 100 megakelvins) for helium fusion to begin. Which of these happens first depends upon the star's mass.
    http://en.wikipedia.org/wiki/Stellar_evolution
  18. The significance of past climate change
    BC #63, The energy emitted by the sun is not constant. There are, and have been over the ages, real differences in its energy output that have nothing to do with any orientation or orbital phase of the earth. Sorry, but I'm going to use you as a case in point that engineers often expect things to be constant that are not.
  19. Tracking the energy from global warming
    BP #60, #62, #64 Can you explain why the 2003-2009 TOA line from your Post #60 chart does not match the TOA line for the same period from the Post #62 Chart. The values on the energy axes (E22 Joules)are vastly different and so is the shape of the TOA curve, The OHC curve seem roughly the same for both charts.
  20. Berényi Péter at 22:56 PM on 22 April 2010
    The significance of past climate change
    #21 chris at 00:05 AM on 22 April, 2010 they [Dansgaard-Oeschger events] are not representative of global warming/cooling events Think again. PNAS online Ice-core evidence of abrupt climate changes Richard B. Alley "Ice-core records show that climate changes in the past have been large, rapid, and synchronous over broad areas extending into low latitudes, with less variability over historical times." It is not "global warming" anyway, it is "climate change". And D-O events brought hell of an abrupt climate change for sure. With such an instability, current agriculture would be impossible, billions would perish of mass starvation. Even if such events can not happen in the present warm regime, it is well known at least 7 years worth of food storage is needed. Still, world economy is run on a "just on time" philosophy with less than a year food backup. Grim.
  21. The significance of past climate change
    As an engineer I thought it behoved me to read and comment, so here goes. . When the sun gets brighter - I baulked at this as my immediate reaction was that you are saying that the sun is emitting more energy. (With thought, I accept that your statement is correct because the sun gets brighter from our perspective because it's closer or the earth is differently tilted due to the Milankovic cycles). When volcanoes erupt - my immediate reaction was we've had recent cases (Pinatubo, Krakatoa) where volcanoes have erupted and only caused very short term climate change. (I'm just giving you my first reaction here) So I was in a doubtful mood when I came to the second last paragraph. . the second last paragraph seems to be the key and I didn't find it convincing (Ie on a quick read. Similar to hearing it as part of a talk). It gave me the impression that there are a jumble of variables here and how would you know what's causing what and which variables are feedback. (Again with contemplation I start to realise what you are saying and how it does make sense. By the way, how can ice cores tell us temperature change and solar activity?) PS. I am not a skeptic on climate science. I live in a hot bed of activism on climate change and my daughter tells me you are giving a talk at UQ next month. I'll try and make it. PPS. I read a great comment in an IPCC article or related document about the greenhouse effect and saturation and the build up of pressure due to extra CO2 and the temperature of Venus being 400+ due to it being 98% CO2. I can't find it right now but I'd be really interested in your take on this topic as I didn't understand the build up of pressure bit and how it affects termperature.
  22. The significance of past climate change
    Arkadiusz Semczyszak at 21:50 PM on 22 April, 2010 1. You are misrepresenting Lonnie Thompson's PNAS article, which shows that current warming is likely unprecedented in the areas studied for 5000 year. Since this is an open access article, anyone wishing to know understand this can read it here Note that this work is about mountain glaciers in S. America (Peru); the analyses presented are interpreted in line with similar data from mountain glacier cores elsewhere in the world. 2. You're misrepresenting the science on the LIA. It certainly wasn't "a rapid and permanent change of temperature in about a few years of at least circa 0.8 deg C". One can assess this by inspection of published data also in open access articles. See here, for example (Fig 3). On can only get "at least circa 0.8 deg C" if one goes from the "height" of the MWP to the "depths" of the LIA, and that took around 500 years (not "in about a few years"!). If one takes the more generally accepted temperature decrease to LIA (from around 1200-1600 AD), the temperature decrease was in the range 0.3-0.5 deg C. However one looks at this your interpretation is grossly incorrect. 3. Bond events. There's not much evidence that these are truly manifest within the Holocene. In any case since the last N. hemisphere warmish period was around 1000-1100 AD and the Bond events have a supposed 1500 year periodicity, we shouldn't actually be having a Bond event now at all. In any case you'll need to provide us with some evidence for Holocene Bond events. It's simply not possible to "explain the very existence of the current changes in temperature", without massiverly enhanced anthropogenic greenhouse gas levels. Making stuff up isn't going to aid our understanding!
  23. The significance of past climate change
    Arkadiusz, another point. The little ice age didn't occur quickly. Reconstructions show a 0.8 degree fall in temperature over a period of around 600 years-a rate of -0.013 degrees per decade! By contrast, global warming since the 1970's has been at a rate of +0.16 degrees per decade-ten times faster! Also, the LIA is directly connected to both the Maunder & Dalton minimums-coupled with some volcanic activity, wheras recent warming has no solar connection.
  24. The significance of past climate change
    Arkadiusz Semczyszak-1st Bond events really would only explain climate change in the Northern Hemisphere. 2nd, almost *every* Bond Event in the Holocene has resulted in *cooling* of the Northern Hemisphere, not warming (like the Iron Age Cold Epoch of 900BC-300BC or the 4.2 KYr event thought responsible for the collapse of the Egyptian Old Kingdom). 3rd, these cooling events have been relatively slow compared to recent warming. So one wonders how you think GLOBAL WARMING is in anyway consistent with Bond Events, when past Bond events-like the 30-year decline in solar activity-suggest that we should be moving into a modest global *cooling* event, if anything-not warming. The fact remains that the only thing consistent with the rapid rise in temperature the last 30-50 years is the equally large rise in CO2 & methane during that same time period.
  25. The significance of past climate change
    John, according to my reading, pre-Quaternary global temperatures were frequently around 22 degrees C, around 6-8 degrees warmer than at any other point since. The only exception was a very brief period at the end of the Ordovician Era and again at the end of the Carboniferous Era-where temperatures fell to those closer to modern averages. Both climate change events were preceded by significant drops in atmospheric CO2 (from 7,000ppm to 4,000ppm between the Cambrian & Ordovician Eras & from 4,000 down to less than 1,000 over the course of the Devonian & Carboniferous Eras). What's important, though, is that even though the sun was around 10% cooler than the modern era, the planet's temperature was significantly warmer than today-& the only real explanation is the very high levels of CO2 in the atmosphere-CO2 that we're now re-releasing back into our atmosphere. Yet still some people would have us believe that this massive release can have *no* impact on our global climate.
  26. Skeptical Science Housekeeping: flags, printable versions, icons and links... lots of links
    The 'skeptical papers' bit is a little weird. 'Is the basin-wide warming in the North Atlantic Ocean related to atmospheric carbon dioxide and global warming?' is hardly 'skeptical', unless you think that 'skeptical' means 'doesn't think EVERYTHING is CO2 related'! They conclude that CO2 warming contributes ~half of Atlantic warming - I don't see how this makes them a 'skeptical' paper, they're simply adding to a body of evidence on AMO & climate...
  27. Arkadiusz Semczyszak at 21:50 PM on 22 April 2010
    The significance of past climate change
    "The past geological record indicates that changes on a global scale are invariably very slow. We're talking tens of thousands, to hundreds of thousands and even millions of years in the vast majority of cases." "The fact that virtually *every* natural climate change event in the past (with the exception of those caused by extremely massive natural disasters) has occurred at a rate of between 1/2 to 1/10th [???] of the rate of recent change is simply further proof that nature is not the cause of the most recent climate change event." ... This is a representation of knowledge - science, with a few years. At least. Repeatedly (here) I proposed-presented, a graph: http://www.pnas.org/content/103/28/10536/F4.large.jpg. Why? 1st L. G. Thompson is a definitely not a skeptic. 2nd Certainly his work only for Africa but (as one of the few) dates back to 2003. Please look at the changes in the eighteenth century. It is difficult to explain only the increase in volcanic activity in the LIA. LIA began, moreover, a rapid and permanent change of temperature in about a few years of at least circa 0.8 deg C. Chris - why? After all, there were no significant changes in ice surface ... Certainly the current change is unprecedented, but certainly no more violent than the old change! For example, according to v. Storch once looked like this: http://www.korthweb.de/PhZT/Temperatur_Intcal2.gif Moreover, the current temperature change fits neatly into the sequence of Bond Events (not to be confused with D-O). CO2 is not needed to explain the very existence of the current changes in temperature ...
  28. Berényi Péter at 20:54 PM on 22 April 2010
    Tracking the energy from global warming
    #63 kdkd at 19:43 PM on 22 April, 2010 Is a csv file of the raw data available anywhere? I could not collect proper data files, so re-digitized both NODC OHC & CERES FLASHFlux (pp. 21) graphs. You can find the csv here. The dimension is 1022 J for both columns, offsets arbitrary, slope of TOA radiation imbalance as well (being the temporal integral of a function with offset unknown). Time resolution is three months.
  29. Tracking the energy from global warming
    BP #62 Thanks. What's the cause of the difference between the TOA line in the first graph compared to the second graph? Is a csv file of the raw data available anywhere? I wouldn't mind doing some crude resampling stats on the time series.
  30. Jacob Bock Axelsen at 18:40 PM on 22 April 2010
    Are we too stupid?
    gallopingcamel We are in the middle of the holocene extinction event due to the lack of intelligent self-interest. The policy of laissez-faire is so appealing, and control so disgusting, that it is only now we might realize that we need control. Instead of putting trust into the "invisible hand" then let us intelligently devise a real visible hand to point the direction of best self-interest. Indirect reciprocity will take care of Joe and his friends as they are not islands entire of themselves. I have never heard of non-perishable foods. That seems to me to be the actual reason for inventing money. Natural trees are not good sequesters with respect to excess CO2 in the atmosphere. Even the Freeman Dyson knows that. A "year without a summer" would be an emergency independently of any plan to mitigate global warming. The prospect of disaster is still not a good justification for creating mountains of rotting food for no use most of the time. I am in favor of a new clean generation of nuclear power, but that may take long and they are very expensive to build. Geothermal is a low-hanging fruit in comparison. I hope this was useful to you.
  31. The significance of past climate change
    There's the ice age CO2/temp graph at wiki, too, a bit down the page on the right, though it's only a straightforward comparison. http://en.wikipedia.org/wiki/Ice_age#Origin_of_ice_age_theory
  32. Glenn Tamblyn at 18:10 PM on 22 April 2010
    The significance of past climate change
    John If you are talking to Engineers, admitedly a very specific audience, try following the energy trail. Radiation Budget, Joules of heat in the ocean etc. Get them onside by doing the 'laymen may focus on temps but we know its about the energy trail'.
  33. The significance of past climate change
    Chemware - is this the kind of thing you're looking for? http://residualanalysis.blogspot.com/2008/06/anthropogenic-global-warming-is.html http://residualanalysis.blogspot.com/2009/12/statistical-proof-of-anthropogenic.html http://moregrumbinescience.blogspot.com/2009/03/does-co2-correlate-with-temperature.html http://bp3.blogger.com/__6PO0G1BcJM/SHjWm0gCguI/AAAAAAAAACk/BsbMNnwz0Go/s1600-h/figure2b.JPG
  34. The significance of past climate change
    #39 Momerath "Being engineers I’m sure at least one asked to see a graph of atmospheric CO2 concentration verses temperature for our planet. Since such a graph does not exist ..." That bugged me too, about a year ago. No amount of googling could find such a graph. So I downloaded the Vostok ice core data, graphed it over the last 100 kYears. You can see the results here: http://home.exetel.com.au/chemware/Paleoclimate.htm I also grabbed some sea-level data by Bard et al., and interpolated that to construct a similar graph for sea levels. Both plots are remarkably linear. They also have alarmingly large slopes.
  35. The significance of past climate change
    I have a pet hypothesis that is in the same vein as Barry's. Another, layman speculation here; so, keep that in mind. I somewhat think that there are plateaus in global temperatures, and the within a plateau, a certain amount of change in forcings has less effect that near the edge of one. I'm imagining a few mechanisms for this, but I'll just try to explain just one. Let's consider the Greenland ice sheet and the albedo of the surface area it occupies. Let's say there is an ice sheet, and the mean temperature over it is -6 C. (Yeah, I know it'll be warmer in the south and colder in the north, on average, and the actual degrees are just for illustrating a point. Humor me; I like to keep things simple.) About 90% of the energy received is reflected. Let's say you have a change in some forcing that raises this area's mean temperature by 4 C to -2 C. The ice sheet remains, and the change in climate is more or less linear (or probably a log) of the forcing. Let's say there is some additional forcing that, by itself, would push the mean temp to +2 C, and the ice cap melts. The albedo changes, the temperature raises some additional factor, and whatever relationship between forcing and effect that existed when the temp was between -6 and -2 C is not the same relationship that you will find between -2 and +2(+x). Same effect on the way down, in reverse. So, if it likely to be the case that there is not a consistent relationship between the amount of forcing and the amount of climate change, it is going to be difficult to anticipate where the current change in forcing will take us. Will we stay within this plateau, or will we be leapfrogged to some other? I believe Hansen has written along these lines better than I can. The point is, engineers are used to thinking in terms of coefficients that relate x to y, but they aren't always prepared to deal with coefficients that are not constant. If some engineer isn't prepared to deal with a variable coefficient, and they detect that it wasn't the same in scenario A as it was under scenario B, you'll loose them. When they learn that the coefficient isn't constant, but don't have a grasp of the larger forces in the equation, they can also come to some erroneous conclusions. In my own experience, I remember aerospace students, when they learned that the coefficient of drag of a sphere decreased with an increase in velocity, jumped to the erroneous conclusion that the drag itself reduced. No, the drag (subsonic) is still proportional to the square of the velocity, and the square of the velocity goes up a lot faster than the coefficient goes down. If there are questions about runaway feedbacks, you can always point out that the energy radiated by a body is proportional to the fourth power of the absolute temperature, and no other part of the equation has that large an exponent. Engineers will get that. I get the same feeling as I did with the decreased drag arguments when I hear arguments that the negative feedbacks, like increased cloud cover, will prevent warming. a) What, water molecules are going to anticipate a warming and leap up to form clouds to prevent it? No, they evaporate more than they had been because they are warmer than they had been. It's not like they weren't evaporating and forming clouds before at some equilibrium level. Clouds might mitigate a warming, but they can not prevent it. Nevermind that water vapor is itself a GHG. b) The changes in the past are a strong counterpoint to the idea that the climate is inherently stabilized by negative feedback mechanisms. Maybe that is my second point. It may be too much of a stretch to jump in saying that changes in the past support that we are changing climate now; it might be better to say that changes in the past establish that a change in forcings can very well change the climate. From there, those that are with you up to that point will naturally start to ask how much forcing are we doing now as compared to some other forcing at some other time. I haven't seen your talk; so, I'll just hazard a guess that some were still eating the first course when you yanked it and presented desert. Well, it's late, I've let myself get long winded, and I'm a choirboy preaching to the preacher. Good night and good luck.
  36. Where is global warming going?
    suibhne has been peddling the same ad hominem nonsense about people misusing the word "heat" (and therefore they are supposedly wrong about global warming) at http://scienceblogs.com/deltoid/2009/03/gerlich_and_tscheuschner_oh_my.php where he has repeatedly been refuted but has refused to address any of the substantive criticisms.
  37. Berényi Péter at 16:28 PM on 22 April 2010
    Tracking the energy from global warming
    #61 kdkd at 12:48 PM on 22 April, 2010 Is this possible, or is that data not available? CERES FLASHFlux only goes back to 2000. If I take all ten years and apply the same procedure it looks like this: The fit is awful because of the huge step-like change of OHC in early 2003 and also the high noise level before. I guess these features are measurement errors due to changing coverage & instrumentation.
  38. Greenland's ice mass loss has spread to the northwest
    It has happened to Greenland in the past when ALL the ice melted. The people had a prosperous time for many years and they enjoyed it.
    Response: There is no recorded history of the last time ALL the Greenland ice melted - the Greenland ice sheet is at least 400,000 to 800,000 years old.
  39. Models are unreliable
    Riccardo As I have just a few minutes let me first just apologize for not giving the refrence. It was almost ill responsible to brag about a paper that I didn't even give the refrence to. I will give you an response later today.
  40. Berényi Péter at 15:41 PM on 22 April 2010
    Where is global warming going?
    #39 chris at 00:18 AM on 22 April, 2010 so what Peter? Have a look and compare coverage.
  41. The significance of past climate change
    So if someone asked about CO2 being much higher in the past (noone did bring that up at the talk), I would say that the sun has been getting steadily brighter over Earth's history. I go a bit further - but as I'm a layman I would like to check with you. I put it that the configuration of the biosphere was also very different, notably a big difference in where land masses are situated. Albedo has a strong influence, so if there is more or less land on our near the poles, this can strongly impact the radiation budget. Directly comparing the biosphere now with that of millions and millions of years ago, in terms of CO2 influence, is a bit of an apples to oranges thing. Is this a fair comment or have I been getting it wrong? Also, would different ocean/atmosphere heat transport dynamics in the distant past have an impact on the total radiation budget, or does it even out for the global total? (Hope that made sense)
  42. Tracking the energy from global warming
    BP #60 That's interesting. But I want to see it on a more appropriate time scale. 30 years is a good minimum for looking at climatic effects (rather than weather effects). Is this possible, or is that data not available?
  43. gallopingcamel at 12:43 PM on 22 April 2010
    Are we too stupid?
    Jacob Bock Axelsen (#106) "Now, enough of what I know. What are your solutions to mitigate climate change?" Two things I could support: 1. Reducing Carbon Emissions As long as this is done via a rapid build up of innovative nuclear power plants (Generation IV) until the cost of electricity is low enough to convince “Joe Six-pack” to trade in his 4X4 for an electric vehicle. No government mandates; just let intelligent self interest persuade the masses. I love my electric car because it is fun to drive rather than its ability to reduce my “Carbon Footprint”! 2. Major Carbon Sequestration Programs Carbon should be sequestered along the lines pioneered by Hammurabi (Babylonian empire). Farmers should be encouraged to overproduce non-perishable foods and timber. The EEC was on the right track with its “Butter Mountains” and “Wine Lakes” although these products were too perishable. Have you ever wondered what would happen to our wonderful high tech civilisation if the recent Icelandic volcano had been a Mount Tambora? How well would we handle another 1816, the “Year without a summer”?
  44. Glenn Tamblyn at 12:39 PM on 22 April 2010
    The significance of past climate change
    #30 unrecovered "Another aspect, I have found difficult for engineers and many other scientists to grasp is: How a system where all feedbacks sum up to a net "positive" does not constitute a run-away system. This is not and easy thing to explain and typically requires too much time in a short talk. But may constitute a stumbling block for engineers in particular. " Perhaps the key point to get across is that the feedbacks are positive, but they also finite or decline with the increase. Methane runs out when the sources are drained, CO2's impact is logarithmic with concentration, when the ice sheets are melting away the albedo change tapers off. And some feedbacks such as Milankovitch Cycles actually cycle between positive & negative.
  45. The significance of past climate change
    Petroleum reservoir engineers construct numerical models to forecast the production from an oil or gas field. They calibrate their models against recorded production rates in a process they refer to as a "history match". See, for example, this abstract which would, I guess, look familiar in many methodological aspects to climate modellers. So, if you were presenting to a bunch of petroleum engineers, you wouldn't have much problem explaining why palaeoclimate was important in calibrating forecast models. I think a major problem with people's misinterpreting the significance of palaeoclimate is the naturalistic fallacy: what's natural is good for us, or the Nietzschean corollary (recently popularized by the Koch brothers in the Smithsonian exhibit)that what doesn't kill us makes us stronger. What the general public doesn't usually understand is the extremely rapid rate of current changes compared to past changes, as well as the fact that the most extreme palaeoclimates would not permit the survival of our current civilization. There's also the logical fallacy that bverheggen noted (about past and present causes) that seems so elementary (to me) I'm amazed that people keep making it. Nevertheless, I've lost count of the number of times that I've used the forest fires/arson metaphor.
  46. The significance of past climate change
    John, this mechanical engineer had no problem understanding either your previous explanation, or the new simplified one. As you've mentioned, though, perhaps the issue is that you got bogged down in the details. A different order of presentation may be required, where you present a simplified overview, then explore a few areas in more depth, perhaps having some of those detailed explanations in reserve to answer questions. Also, from personal experience - if you were presenting to a bunch of students, then the 'blank looks' & shortage of questions aren't that uncommon while people are digesting the information just presented. Explaining AGW in terms of radiative heat transfer, though, is something any fourth-year engineering students should understand (heat transfer was 3rd year subject when I studied at UQ, but that was nearly 20 years ago...)
  47. The significance of past climate change
    Oh, and about understanding thermodynamics: I had a VERY long argument in Topix with somebody who clearly had an engineering background, yet believed that EVERY climate scientist claiming AGW was relying on violations of the First Law of Thermodynamics (occasionally he claimed 2nd too) in their understanding of the energy balance. He even claimed to find this flaw in Trenberth's famous diagram. But when I turned to the diagram (and Trenberth's original paper, whose title I forget), what I saw was something very different: I could not find evidence of any such violation (of course), but I DID find evidence of some very disappointing mistakes in presentation that made it difficult to verify that the First Law is satisfied by his numbers. So what is the implication of all this for this article? I would say two things 1) do NOT assume a deep understanding of Thermodynamics, not even from engineers 2) make sure that quantities, variables, scales etc. are CLEARLY marked in the diagrams, and that simple questions like which way how much heat/energy flux flows are easily visible on the diagram. Diagrams like the one in post#27 in this thread are damn near useless.
  48. Where is global warming going?
    Thanks HR. Looks like a good review.
  49. The significance of past climate change
    Everything in the "dumbed down" talk sounds good and true, but it seems to miss the point. The skeptics, for example, could immediately make it all SOUND meaningless by pointint out that in the past (was it Late Triassic? I forget), we had MUCH higher CO2 levels, but rather small climate change due to it. This would APPEAR to overrule the presentation's observations that 1) climate changes took place in the past due to forcings and 2) CO2 is a forcing. What is the right approach to this? My understanding (I would certainly welcome Cook's corrections) is that the degree to which the climate is sensitive to forcings has itself also been highly variable. Specifically, that with the Late Triassic configuration of continents and corresponding ocean currents, even a rather large CO2 forcing had a surprisingly small effect; but with modern ocean currents, it is well-expected to have a MUCH larger effect. So if that understanding is correct, then it certainly should be included in the presentation for engineers.
    Response: Funnily enough, this was one of the questions I was asked at the presentation - "are you saying climate sensitivity was lower in the past?"

    On the contrary, climate sensitivity has been surprisingly consistent in the past, even going back millions of years. So if someone asked about CO2 being much higher in the past (noone did bring that up at the talk), I would say that the sun has been getting steadily brighter over Earth's history. Millions of years ago when CO2 was much higher, solar output was lower. The combined effect of sun and CO2 show good correlation with climate. For more details, see CO2 was higher in the past.

    In fact, it's because the sun was cooler in the past that CO2 was so much higher. CO2 acts as a natural thermostat for our climate, regulated by rock weather which is the process of removing CO2 from the atmosphere by chemical reactions. When it's cooler, rock weathering activity slows so there's less removal of CO2 from the air. This means CO2 builds up, warms up the planet. Then as it gets warmer, rock weathering activity increases which removes CO2 out of the atmosphere.

    This process is a natural way of keeping our climate within a certain temperature range. It means that if the sun was cooler, temperatures get cooler so rock weathering slows down, increasing CO2 levels. This is a fascinating process but of course, I didn't go into that much detail at the talk - I just mentioned that climate sensitivity has been consistent in the past.
  50. The significance of past climate change
    CO2 science has something of history in misrepresentation of science papers by selective quoting. I think you can get a list of other examples by putting "CO2science misrepresent" into google and follow links sounding like annoyed authors.

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