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What is the net feedback from clouds?

What the science says...

Select a level... Basic Intermediate

Evidence is building that net cloud feedback is likely positive and unlikely to be strongly negative.

Climate Myth...

Clouds provide negative feedback

"Climate models used by the International Panel on Climate Change (IPCC) assume that clouds provide a large positive feedback, greatly amplifying the small warming effect of increasing CO2 content in air. Clouds have made fools of climate modelers. A detailed analysis of cloud behavior from satellite data by Dr. Roy Spencer of the University of Alabama in Huntsville shows that clouds actually provide a strong negative feedback, the opposite of that assumed by the climate modelers. The modelers confused cause and effect, thereby getting the feedback in the wrong direction." (Ken Gregory)

The effect of clouds in a warming world is complicated. One challenge is that clouds cause both warming and cooling. Low-level clouds tend to cool by reflecting sunlight. High-level clouds tend to warm by trapping heat.

clouds

As the planet warms, clouds have a cooling effect if there are more low-level clouds or less high-level clouds.  Clouds would cause more warming if the opposite is true.  To work out the overall effect, scientists need to know which types of clouds are increasing or decreasing. 

Some climate scientists, such as Richard Lindzen and Roy Spencer, are skeptical that greenhouse gas emissions will cause dangerous warming. Their skepticism is based mainly on uncertainty related to clouds.  They believe that when it warms, low-level cloud cover increases. This would mean the Earth's overall reflectiveness would increase. This causes cooling, which would cancel out some of the warming from an increased greenhouse effect. 

However, recent evidence indicates this is not the case. Two separate studies have looked at cloud changes in the tropics and subtropics using a combination of ship-based cloud observations, satellite observations and climate models. Both found that cloud feedback in this region appears to be positive, meaning more warming.

Another study used satellite measurements of cloud cover over the entire planet to measure cloud feedback.  Although a very small negative feedback (cooling) could not be ruled out, the overall short-term global cloud feedback was probably positive (warming).  It is very unlikely that the cloud feedback will cause enough cooling to offset much of human-caused global warming.

Other studies have found that the climate models that best simulate cloud changes are the ones that find it to be a positive feedback, and thus have higher climate sensitivities.  Steven Sherwood explains one such study:

While clouds remain an uncertainty, the evidence is building that clouds will probably cause the planet to warm even further, and are very unlikely to cancel out much of human-caused global warming.  It's also important to remember that there many other feedbacks besides clouds. There is a large amount of evidence that the net feedback is positive and will amplify global warming.

Basic rebuttal written by dana1981


Update July 2015:

Here is the relevant lecture-video from Denial101x - Making Sense of Climate Science Denial

Last updated on 25 July 2017 by skeptickev. View Archives

Printable Version  |  Offline PDF Version  |  Link to this page

Comments

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Comments 201 to 250 out of 256:

  1. No, net feedback in the climate system is not required to be negative.
  2. Bibliovermis (RE: 201), "No, net feedback in the climate system is not required to be negative." Then can you explain how the current energy balance is maintained despite such significant amount of shorter-term, local, regional, seasonal hemispheric and even sometimes globally averaged variability?
  3. 202, RW1, Can you explain how such variability could exist with a net negative feedback damping the system?
  4. Sphaerica (RE: 203), "Can you explain how such variability could exist with a net negative feedback damping the system?" It's a highly dynamic and chaotic system with large changes in incident energy flux. Changes from day to night, changes in atmospheric circulation patterns, etc., etc. It's constantly changing everywhere all the time.
  5. Sphaerica (RE: 203), Feedback, by definition, is the response to the changes in energy flux from all the chaos that results in the constant variation.
  6. 204, RW1, Yes, we all know that. It doesn't answer the question.
  7. 205, RW1, Yes, we all know that. It doesn't answer the question. Except for the "from all the chaos that results in the constant variation" part. You added that just to make it look like it fits well with your own hypothesis, but you just made it up. Feedback is the response to the inputs. Period.
  8. 204, RW1, 205, RW1, In case I'm being too subtle, what I mean by that is stop playing games and answer the question.
  9. Sphaerica, Feedback is the response to changes in energy flux. I'm not sure I understand the question. Yes, the constant change and chaos fits well with what I'm saying. That's largely my point.
  10. RW1, I must have missed your answer to my question - how do you explain palaeoclimate variations (glacial-interglacial cycles and so on) with a net negative feedback? Maybe you can provide an answer where Pielke, Spencer and Lindzen have not (to my knowledge)?
  11. The question, rephrased so that you can understand it, is: If you have a net negative feedback, why does the system succeed in fluctuating so greatly? Why does the negative feedback not keep the system stable and within very narrow confines? And separately there is no requirement that the inputs be the "constant change and chaos." Yes, I understand that it fits with what you are trying to arbitrarily impose on the system, but it is too narrow a definition. The feedback is a response to any input, whether that input is part of constant change and chaos, or a new, steady input. Any attempt to frame the definitions and system only within the narrow confines of a predetermined conclusion will confuse the issue. Please stick with proper, true definitions, rather than reframing things in order to score points or twist the argument in a certain direction.
  12. RW1, Your current question to me (#202) is effectively "How can 2 + (2 * 1.5) = 5?" In the context of your question, positive feedback is simple math.
  13. Sphaerica (RE: 211), "The question, rephrased so that you can understand it, is: If you have a net negative feedback, why does the system succeed in fluctuating so greatly? Why does the negative feedback not keep the system stable and within very narrow confines?" Because the feedbacks take time and the system is largely chaotic. Over time, the net negative feedback does keep the system tightly constrained, which is why longer-term globally averaged there is generally very little change relative to the much larger more local and regional short-term change.
  14. Sphaerica (RE: 211), "The feedback is a response to any input, whether that input is part of constant change and chaos, or a new, steady input." Yes. It's interesting that you would mention this because it leads into my next point, and that is the physical processes and feedbacks that maintain the planet's energy balance cannot be separated from those that will act on additional 'forcings', such as GHGs.
  15. Feedbacks need not be instantaneous. For instance, when wolves were shot in the early 20th century in order to increase the deer populations, herds increased immediately. However, the increase in the herds exceeded the carrying capacity of the environment, and the herds decreased over the next several years due to the lack of food supply. The herds varied widely initially, but were eventually constrained by the food feedback to a population which was not all that different from the original.
  16. 213, RW1, Your original question was:
    Then can you explain how the current energy balance is maintained despite such significant amount of shorter-term, local, regional, seasonal hemispheric and even sometimes globally averaged variability?
    My leading question was:
    If you have a net negative feedback, why does the system succeed in fluctuating so greatly? Why does the negative feedback not keep the system stable and within very narrow confines?
    Your answer for my question was:
    Because the feedbacks take time and the system is largely chaotic.
    My answer to your original question is:
    Because the feedbacks take time and the system is largely chaotic.
  17. 214, RW1,
    Yes. It's interesting that you would mention this because it leads into my next point, and that is the physical processes and feedbacks that maintain the planet's energy balance cannot be separated from those that will act on additional 'forcings', such as GHGs.
    Good for you. You are beginning to demonstrate some grasp of how the system operates. Now your questions have been answered. You need to answer some of the questions that have been posed to you, specifically: With a net negative feedback, how do you account for the broad fluctuations in climate that have been identified throughout recorded history (through proxy studies)? And With a net negative feedback, how do you account for the dramatic and historically unique warming of the past 30 years? Why has your powerful net negative feedback not succeeded in constraining temperatures for the past thirty years? If it has not done so in that time frame, how can you imagine that it will do so in the future, as we continue to raise CO2 levels to dramatic extremes?
  18. RW1 - "Then can you explain how the current energy balance is maintained despite such significant amount of shorter-term, local, regional, seasonal hemispheric and even sometimes globally averaged variability?" Conservation of energy, RW1. Internal variation produces lots of fluctuations, but such excursions up and down are limited by the incoming/outgoing energy levels, and will cycle around those energies. And of course, if the amount of energy in the climate changes due to (for example) increased GHG's, the climate will shift it's average behavior accordingly. As to feedbacks, as long as the gain < 1, the system is stable, as per the Does positive feedback necessarily mean runaway warming thread. Net positive feedback means a greater shift in climate state for input/output energy changes - not instability. And positive feedback is observed from the ratio of paleo changes in climate to reasonably well known energy changes, QED. --- RW1 - This has all been discussed with you before, in excruciating detail, on the Lindzen-Choi threads. Your continuing intransigence indicates (IMO) that your opinions and preconceptions are apparently more important to you than the facts.
  19. Sphaerica (RE: 217), I don't think you understand what net negative feedback means. It does not mean that no long-term change can occur (or even short-term change). It means the response to changes in 'forcing' or energy imbalance will be to oppose or diminish those changes rather than re-enforce or amplify them.
    Response:

    [DB] Sphaerica quite well understands both positive and negative feedbacks, including those "net" ones.

  20. RW1, I see you continue to ignore my question to you, put in #197 and #210. How do you explain palaeoclimate variations with a net negative feedback? The initial orbital forcings were much smaller than the resulting climate changes. Palaeoclimate variations, being real-world climate changes with real causes and real effects, already include the cloud feedbacks. I take your non-answer to mean that you, like Lindzen, Spencer and Pielke, do not have an answer to that question...
  21. 219, RW1, I don't think you understand what positive feedback means. It does not mean that only long-term changes can occur. It means the response to changes in 'forcing' or energy imbalance will be in the same direction or enhance those changes rather than reduce or negate them. Now that we're done with the absolute silliness, it had been left that you had your question answered quite clearly and succinctly. Indeed, I allowed you to provide the answer to the question yourself. Now you need, in order to carry the conversation forward, to answer the questions that have been asked of you, without evasion. These questions have now been asked multiple times and you have failed to provide answers. The discerning viewer will begin to come to the conclusion that you either do not have the answers, or you are chagrined at where those answers logically lead. The questions you must answer are: With a net negative feedback, how do you account for the broad fluctuations in climate that have been identified throughout recorded history (through proxy studies)? With a net negative feedback, how do you account for the dramatic and historically unique warming of the past 30 years? Why has your powerful net negative feedback not succeeded in constraining temperatures for the past thirty years? If it has not done so in that time frame, how can you imagine that it will do so in the future, as we continue to raise CO2 levels to dramatic extremes?
  22. sky#220: Not to worry; we're coming up on the one year anniversary of the net negative feedback gambit.
  23. It's like Groundhog Day...all over again.
  24. skywatcher (RE: 220), I can answer those questions, but they are off topic and not really relevant to what's being discussed at present. I'm primarily talking about the planet's current energy balance and whether or not net negative feedback is required to maintain this balance. The claim here seems to be that net negative feedback is not required, though I don't see this could be the case.
    Response:

    [DB] Actually, skywatcher's questions to you are both germane and on-topic.  You are clearly being evasive and avoiding answering questions for which you have no substantive answer.

  25. Sphaerica (RE: 221), "The questions you must answer are: With a net negative feedback, how do you account for the broad fluctuations in climate that have been identified throughout recorded history (through proxy studies)? With a net negative feedback, how do you account for the dramatic and historically unique warming of the past 30 years? Why has your powerful net negative feedback not succeeded in constraining temperatures for the past thirty years?" I'm sorry, but I still don't think you understand entirely what is meant by net negative feedback. The warming we've experienced in the last 30 years is entirely possible with net negative feedback operating on the system. I'm not sure what else to say in regards to this. As to the more 'broad fluctuations' in the climate that have occurred (whatever that means exactly), no doubt there are numerous reasons why. The main ones appear to be changes in energy distribution within the system (from Milankovitch orbital cycles) and the positive feedback effect of melting surface ice (like from glacial to interglacial) or growing surface ice (like from interglacial to glacial).
  26. 225, RW1, Clear evasion. And gibberish.
  27. RW1 - "These things appear to be strong enough to overcome the net negative feedback operating on the system and cause significantly more change than just what the change in net incident energy alone would cause." (emphasis added) You know, that's a perfectly reasonable definition - of positive feedback. You have just invalidated your last N+ posts claiming negative feedback, RW1.
    Response:

    [DB] RW1 is clearly trolling now.  His comments will be treated as such until he can offer up substantive dialogue supported by more than mere opinion and hand-waving.  This has become tiresome.

  28. 227, RW1, What "things"? How is this any different from today? Why can it appear to cause more change in those cases, but not now?
  29. KR, "You know, that's a perfectly reasonable definition - of positive feedback." I know what you're saying, but this isn't quite what I meant. What I meant is the other things are strong enough to cause more change than the net amount of change that would result from the net negative feedback alone.
  30. Daniel Bailey - Somewhere between Groundhog Day and Whack A Mole... RW1 - I strongly suggest actually doing some reading on radiative physics. You are once again demonstrating the D-K effect.
    Response: [Sph] End italics tags fixed.
  31. RW1, I second KR's suggestion. There is a wealth of information out there to be learned. Fill in the gaps in your understanding and come back with a model which is consistent with all of the facts, not just some. [We want to discuss science here, not magic.]
  32. Sphaerica (RE: 229), "What "things"? How is this any different from today? Why can it appear to cause more change in those cases, but not now?" For starters, the positive feedback effect of melting ice from that of leaving maximum ice cannot be equated to that of minimum ice where the climate is now (and is during every interglacial period). There just isn’t much ice left, and what is left would be very hard to melt, as most of it is located at high latitudes around the poles which are mostly dark 6 months out of the year with way below freezing temperatures. A lot of the ice is thousands of feet above sea level too where the air is significantly colder. Unless you wait a few 10s of millions of years for plate tectonics to move Antarctica and Greenland to lower latitudes (if they are even moving in that direction), no significant amount of ice is going to melt from just a few degrees rise in global average temperature. Furthermore, the high ‘sensitivity’ from glacial to interglacial is largely driven by the change in the orbit relative to the Sun, which changes the distribution of incident solar energy into the system quite dramatically (more energy is distributed to the higher latitudes in the NH summer, in particular). This combined with positive feedback effect of melting surface ice is enough to overcome the net negative feedback and cause the 5-6 C rise. The roughly +7 W/m^2 or so increase from the Sun is a minor contributor to the whole thing. We are also relatively close to the end of this interglacial period, so if anything the orbital component has already flipped back in the direction of glaciation and cooling.
    Response:

    [DB] Now you post gibberish.  It has become etremely evident that you are here simply to be argumentative, and that you simply do not have a background sufficient to realize that most of what you write above is, to put it delicately, "crap".

    Please make a considered effort to ensure what you write is consistent with the known physics of climate change; your persistence in forcing physics to contort to your electronics-based interpretation of things is admirable, but misguided.

    Shorter admonition:  less posting, more studying.

    A general note to the lay reader:  RW1 has a long history here of having these exact type of interactions on many previous threads.  He promulgates the same basic arguments which are promptly shown to have the same basic misunderstandings.  Not liking the answers, he has even taken the propositions to other websites like Real Climate, where he was given the same answers, to which he expressed similar reluctance in believing.  Let the reader beware.

  33. 233, RW1, Nice try, but no. It has been very clearly calculated that the insolation and albedo changes alone are insufficient to produce the temperature swings seen between glacials and interglacials. CO2 changes are measured, and in fact are computed to account quite well for the difference when other positive feedbacks (water vapor, etc.) are added in. This would not be the case if there were a net negative cloud feedback. Goodness, you really, really want CO2 to be a non-factor, don't you? But even if your scenario were true -- why doesn't your strong net-negative cloud feedback counter the changes in insolation and ice albedo? If cloud feedbacks are driven by temperature changes, and temperatures rise, shouldn't there be more clouds, and a higher albedo -- keeping the earth covered in ice?
  34. RW1, you really are talking gibberish now. And my question was not off-topic in relation to the feedback from clouds, as palaeoclimatic variations include feedback from clouds (as I said in #221), thus constraining their magnitude. Is the total feedback demonstrated by palaeoclimate positive or negative? And remember we live on an Earth with some hefty ice sheets, sea ice and winter snowcover right now. All ready and willing to chip in on positive albedo feedback, right now. A large portion of the Greenland Ice Sheet lies below the glacier equilibrium line. Its mass balance is presently negative and accelerating negative. Do you think that all that ice is going to remain safe at high altitude under these conditions? Speaking of altitude, what was the average altitude of the Laurentide, Scandinavian or British ice sheets? Did altitude help them survive, too? I like your definition of positive feedback in #227. With a very slight alteration in wording I might use it myself... It really does totally invalidate your argument though! If your last sentence in #233 is correct, where's the cooling? #222 mc - I see, the D-K is strong with this one.
  35. Sphaerica (RE: 234), Now you're at least asking some good questions. It's late though and I need to call it night. I'll respond tomorrow.
    Response:

    [DB] "Now you're at least asking some good questions."

    Actually, all parties have presented you with good questions.  If you are going to participate in the dialogue here, it is incumbent upon you to formulate good answers to those questions.

  36. Dear all, I wanted to make another observation regarding water-vapour feedback that might not have already been discussed. If the amount of water vapour increases in the troposhere so will the specific heat capacity of the air. The change in temperature of the air as a function of altitude is governed by the adiabatic lapse rate. For dry air this turns out to be about -9.8 Kelvin per kilometre. For air of "average moisture content" (I forget what value this is) the lapse rate turns out be be around -7 Kelvin per kilometre. So I expect this value to decrease. Now, the minimum temperature found in the lower atmosphere occurs at the tropopause. This minimum temperature is a kind of compromise between heating at the Stratospheric ozone layer and the troposheric lapse rate. Any change in the latter will imply that the tropopause occurs at a higher altitude and at a greater (minimum) temperature. This will affect the amount of radiation that can be emitted from the Tropopause in a positive way. A second influence will be that, if a greater rate of condensation occurs due to increased water vapour content this will also increase the temperature of the upper troposphere, thus further enhancing the emission rate there. These effects may not have already been considered in the models. On a different matter: sometimes it is not useful to talk about radiation as though this is the main mechanism of energy exchange within the troposphere. The only radiation that is essentially transferred in the atmosphere is incoming solar radiation and up to 40 W m-2 emitted directly from the near the Earth's to clouds and back again. All other energy is transferred by thermal conduction enhanced by convection (or just convection in the case of vaporization/condensation). This does not make any difference to most of the arguments presented but one can get a clear picture of the situation.
    Response:

    [DB] Welcome to Skeptical Science!  There is an immense amount of reference material discussed here and it can be a bit difficult at first to find an answer to your questions.  That's why we recommend that Newcomers, Start Here and then learn The Big Picture.

    I also recommend watching this video on why CO2 is the biggest climate control knob in Earth's history.

    Further general questions can usually be be answered by first using the Search function in the upper left of every Skeptical Science page to see if there is already a post on it (odds are, there is).  If you still have questions, use the Search function located in the upper left of every page here at Skeptical Science and post your question on the most pertinent thread.

    All pages are live at SkS; many may be currently inactive, however.  Posting a question or comment on any will not be missed as regulars here follow the Recent Comments threads, which allows them to see every new comment that gets posted here.

    Comments primarily dealing with ideologies are frowned upon here.  SkS is on online climate science Forum in which participants can freely discuss the science of climate change and the myths promulgated by those seeking to dissemble.  All science is presented in context with links to primary sources so that the active, engaging mind can review any claims made.

    Remember to frame your questions in compliance with the Comments Policy and lastly, to use the Preview function below the comment box to ensure that any html tags you're using work properly.

    "These effects may not have already been considered in the models."

    Please use the search function to find a page on models.  Likely any question you may have on climate science has already been addressed on one of the 4,700+ pages here.  Thus, the search function is your friend; use it and the coppers of your pocket [your questions]...and it will line your mind with gold.

  37. SC1 @236, what you are describing is the Lapse Rate Feedback, a well known negative feedback. Because it is a product of increased specific humidity, it tends to correspond inversely to the Water Vapour feedback, which is positive. That is, if there is a strong water vapour feedback, then the lapse rate feedback is also expected to be strong. Correspondingly, if there is a weak water vapour feedback, the lapse rate feedback is correspondingly weak. As can be seen below, the Water Vapour feedback is stronger than the Lapse Rate feedback, so that the net effect is a positive feedback. Please note that though the tropopause does increase in altitude with a warming atmosphere, this is not due to the change in lapse rate. Water vapour, unlike CO2, is not well mixed so that it is largely confined to the lower half of the troposphere. As such, the lapse rate feedback is negligible, or even slightly positive at higher altitudes (see first link, to the IPCC AR4, for discussion).
  38. Dear All, it would be very informative if Dessler (2010) identified the mechanism by which fewer low-lying clouds would be generated if the water vapour content of the air (plus air temperature) increases. Is anyone aware of such a mechanism being mentioned in a peer-reviewed pulblication?
  39. Dear Tom, thanks very much for your quick and informative answer. Indeed I hadn't been aware that lapse-rate forcing had been treated already.
  40. SC1 @238, there are multiple ways in which clouds can interact to produce feedbacks, both positive and negative. For example, the strength of incoming Short Wave radiation varies in (approximate) proportion to the cosine of latitude. Meanwhile the greenhouse effect of clouds varies in proportion to the surface temperature. Because surface temperature declines only slightly (about 15%-20%) from equator to Arctic, while the cosine of latitude varies from 1 to 0, clouds have a net positive effect in polar regions. Because greenhouse gases reduce the temperature range from equator to pole, that increases the strength of polar cloud greenhouse effect relative to cloud albedo effect, and hence acts as a positive feedback if all else remains equal. The point here is not that this is a major effect (it probably is not), but that the interaction between clouds and radiation is subtle. Another effect, significant in the tropics is the increase in strength of convection cells, resulting in more anvil head clouds. It is not the height of the cloud base, but the cloud tops which determines the greenhouse effect of clouds, so stronger convection in the Inter Tropical Convergence Zone would probably result in a positive cloud feedback. Further, if temperature increases in a region and/or altitude faster than water vapour so that relative humidity falls, the result will be reduced cloud in that region and/or altitude. This effect can result in more high cloud and less low cloud (or the reverse) which depending on the distribution of these phenomena can result in a positive or negative net cloud feedback. Other physical mechanisms exist. So, the problem in answering your question does not lie in deducing physical mechanisms. It lies, firstly in the fact that models do not agree on the properties of clouds, so we cannot look at the models to deduce exactly which physical mechanisms will dominate with regards to clouds. Further, observations are limited in number so that it is difficult to distinguish signal from noise in this instance. While substantial mystery remains about the behaviour of clouds in a warming environment, what can be said is that both the balance of models (see graph in 237), and the balance of physical evidence (see main article) suggest a net positive feedback. That means that summed over a variety of possible cloud reactions, more possible combinations of cloud responses result in warming (models), and physical evidence suggests the actual response is a positive feedback.
  41. I'm a bit late on this. We all agree that clouds both cool by reflecting the Sun's energy and warm by 'blocking' or delaying the exit of surface emitted energy, but this is rather trival to the fundamental question of the net cloud feedback, is it not? The biggest problem is in the current climate, the net effect of clouds globally averaged is to cool by about 20 W/m^2, as is even acknowledged in papers claiming to show net positive cloud feedback (i.e. Dessler 2010), and is consistent with net negative feedback from clouds. This discrepancy would have to be explained in the context of strong net positive feedback from clouds on incremental warming, would it not? Not only is this not explained either by Dessler or anyone else to my knowledge, but without knowing physically why the net effect of clouds is to cool by 20 W/m^2 in the current climate, there is no way to know if the assessments of net positive feedback on incremental warming are accurate, let alone even physically possible. Ultimately, the fact that no one purporting evidence of net positive cloud feedback can explain this or even tries to explain it in light of the conclusions of their work, is rather telling to me how weak and unsubstantiated the case for net positive cloud feedback actually is. And while globally averaged, the water vapor concentration and water vapor feedback in response can further increase temperatures in a warmer world, it cannot be separated or isolated from the cloud feedback, as the two are constantly interacting together to maintain the current energy balance. This gets back to my point about the water vapor and cloud feedbacks already operating in a very dynamic manner in the current climate's globally averaged state from the forcing of the Sun. From this, let's look at the fundamental question of climate sensitivity, net feedback, etc. from the basic constraints dictated by conservation of energy. If the surface of the Earth is the warm by 3C, it must emit 406.6 W/m^2 from S-B (assuming an emissivity of 1 or very close to 1), which is +16.6 W/m^2 from the current global average of 390 W/m^2. Conservation of Energy dictates this +16.6 W/m^2 flux has to be entering the surface from the atmosphere on global average if it is to warm by 3C. There are really only two possible sources for this required energy flux into the surface, and that is either from the Sun via a reduced albedo or from increased atomspheric absorption (like from water vapor). If the current averaged state of the atmosphere is only going to provide +6 W/m^2 (+1.1C) from 2xCO2 (3.7 W/m^2 directly from the CO2 'forcing' and the remaining 2.3 W/m^2 from the current average opacity of the atmosphere; 3.7 W/m^2 x 0.62 = 2.3 W/m^2), where is the additional 10.6 W/m^2 needed for the 3C rise coming from? Can anyone explain and quantify the actual physics of how about a 1 C rise in temperature will change the atmosphere in a way that will further cause an additional 10.6 W/m^2 flux into the surface? If you think it will come primarily from increased water vapor, are you claiming that the water vapor absorption will increase by 10.6 W/m^2 from a 1 C rise in temperature (actually more than 10.6 W/m^2 because half of what's absorbed by the atmosphere escapes to space as part of the flux leaving at the TOA), and if so based on what data or physics? Or if you think the combined cloud feedback will cause a large portion of it, in what specific physical way? If by letting in more sunlight, how does increasing water vapor cause decreasing clouds or more transparent clouds? If by causing increased atmospheric absorption through more clouds, how is this specifically more than the incremental power reflected from the additional or thicker clouds? How is this rectified with the fact the net effect of clouds is to cool by about 20 W/m^2 in the current climate? In general there seems to be a lot of hand waving in regards to this fundamental question and answers to it tend to only be vague, generalized statements like "it comes from the all the feedbacks" or "from downward LW", etc. This kind of sloppy and incomplete scientific reasoning is not good enough. The required energy entering the surface for a 3C rise has to be coming from somewhere specific and from some specific physical process or combined processes that can be corroborated by some real, observable, quantifiable physics and data. I see mosly heuristic assumptions and more or less wild guessing dressed up as some kind of quasi 'best estimate' or 'educated guess'.
  42. Well, many people have tried to educate on the physics without success, but as to this one: "There are really only two possible sources for this required energy flux into the surface, and that is either from the Sun via a reduced albedo or from increased atomspheric absorption (like from water vapor)." That additional flux on the surface comes from increase in backradiation due to increased GHGs. It is that simple. This is not sloppy; it directly calculated from the RTEs.
  43. scaddenp, "That additional flux on the surface comes from increase in backradiation due to increased GHGs. It is that simple. This is not sloppy; it directly calculated from the RTEs." You disappoint me with your answer.
  44. Well that is the physics whether you can understand it or not.
  45. RW1 - I have responded to your post on the far more appropriate Climate Sensitivity thread. Moderators - Might I suggest that discussions of total climate sensitivity are (while related) off-topic in a thread on the specific subject of cloud feedback?
  46. ABC (Aussie) has a summary of Roger Davies (et al.) work on cloud height decrease over the last decade. From the summary: "Experts from the University of Auckland suggest the change in cloud altitude could be the Earth's way of dealing with global warming." Earth's way of dealing with global warming. We don't need mitigation; Earth's got our backs. Earth's a smart cookie. It likes us. Wants to protect us. That Pluto . . . dumb as a rock . . . living way out there at the edge . . . freezing! Isn't even smart enough to grow a coat.
  47. DSL - Strange how the Earth still got very hot in the past eh? The most likely explanation is that the lowering of cloud height is related to the ENSO trend, and the consequent top-of-the-atmosphere radiation flux over the last decade. The decade started off with weak La Nina and El Nino and finished off with strong ones, and the end of the decade was La Nina-dominant. A colder, drier atmosphere (relative to the beginning of the decade) should see less cloud formation and a lowering of cloud height. Nothing makes sense in mainstream media land, because they don't even make the effort to understand what's happening. Sad really. I'm writing up a post/rebuttal of Davies & Molloy (2012). Their findings have predictably been mangled - although a sentence in the study doesn't help.
  48. If clouds feedback were positive, we would expect:

    Infinite warming, until oceans become dry.

    It never has occurred in the past, even with a warmer earth.

    IPCC's Climatologists should say:

    We don't know everything about clouds. We need study a lot to understand the entire process. When we are sure, we are explaining step by step, showing with controlled laboratorial experiments, and calculation memory. When we can explain in details how to trigger an ice age, and an interglaciation era, we are ready to define positive or negative feedback for clouds. By now, we are closing our mouth about global warming or cooling.

  49. Licorj - See Does positive feedback necessarily mean runaway warming. That would only be true with a feedback gain >1, which means that any increase would have an infinite effect. In reality, the law of diminshing returns means that feedbacks of a physical scale are of gain <1, with the total change in temperature being:

    Total T = ΔT / (1-g)

    and with the positive feedbacks providing a limited scale of amplification for any temperature change. For the current sensitivity estimate of ~3C per doubling of CO2, with an initial ΔT of ~1.1C, the gain 'g' is about 0.63. 

    Now as to clouds, if you have actually read the opening post (I suspect you have not), clouds are estimated to have a small positive (amplifying) contribution to the total sensitivity. 

  50. Dear KR,

    First, thank you by attention, even after long time past from publication of this post. I just have realized it, after my post was sent.

    I have read the post, and a lot of very interesting comments. "Clouds are estimated be small positive feedback". Ok. Estimated to be, but could be estimated to not to be... It is a game.

    Excuse me by error on "INFINITE WARMING". It is clear that is not possible, otherwise, we would have free energy generation.

    Backing to the clouds: I believe, of course, with less scientific based knowledge than you, that the choice on small positive feedback for cloud, taken by climate scientists was just a choice, with high level of uncertainty. So high, that choice would be NEUTRAL, or small negative feedback. In order to get the true cloud feedback, it would be need a lot of measures taken around the world, on entire troposphere, entire world, during long time. Of course it is very expensive and hard to do, maybe impossible.

    Even assuming my mistake on INIFINITE WARMING, I still believe that oceans would be expected to dry, because of positive feedback, in any level.

    Other expected result from feedbacks for, aerossols, cloud, water vapor, CO2, CH4, etc, would be the accuracy of models on recreating paste climates. They are all wrong, on this task. Somethings are very wron with them, and nedd to be fixed, before can tell us how will be the climate after 100 years from present day.

    Why we see tomorrow's weather forecasts, and believe on it ?

    Because they are correct on vaste majority of times. It is not the same case for climate models, at least, untill now.

    But, this is off-topic.

    Response:

    [JH] Since you have provided absolutely no specific evidence to substantiate your sweeping assertions about global climate models, your assertions are merely your opinion - which carries virtually no weight on this site.

    If you post similar comments in the future, they will be summarily dismissed for violating the SkS Comments Policy re sloganeering.  

    Please read the SkS Comments Policy and adhere to it. 

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