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johnd at 14:21 PM on 11 March 2011Interactive animation of the climate change impact on agriculture
Marcus at 13:54 PM, these rainfall trend maps illustrate how conditions, for the present generation of farmers, in this example rainfall, are closer to that experienced by their grandparents, and quite different to that experienced by their parents. As for the present day policy of the NFF, please provide some evidence. -
Marcus at 14:05 PM on 11 March 2011Interactive animation of the climate change impact on agriculture
"I will stand with real world research from fields showing that additional co2 results in higher bio mass and crop yields." ....and which field trials are you referring to? All the FACE trials I've read about suggest that the benefits of extra CO2 have been massively overstated, & usually come at significant cost (as I've highlighted above)-& are ultimately short lived anyway. Still, you go on clinging to that meme if it makes you feel better. -
Tom Curtis at 14:03 PM on 11 March 2011What would a CO2-free atmosphere look like?
From Peru @19, clouds form when water vapour condense from the atmosphere as the surrounding gas cools. With a drier atmosphere, you will also get a greater change in temperature with altitude, and hence a greater relative rate of condensation. So there is at least one solid reason to think cloud cover will not just track water vapour levels unambiguously. -
Marcus at 14:02 PM on 11 March 2011Interactive animation of the climate change impact on agriculture
What you keep forgetting Camburn, is several key things: (1) warmer weather increases the rate of senescence (aging) in plants, meaning that seed ripening tends to occur *before* they have a chance to reach maximum size. (2) most plants tend to be biased towards increasing vegetative biomass over seed biomass. (3) plants exposed to higher CO2, prior to acclimation, require much more nitrogen as they need to produce more of the enzymes needed to utilize the extra CO2 in their bio-synthetic pathways. (4) these plants also require greater energy to build & maintain the enzymes necessary to utilize the extra CO2. (5) over time, these plants become acclimatized, & actually switch off the production of the extra enzyme, meaning biomass increases from extra CO2 usually only last about 2-3 years at most-shorter if the plants lack access to sufficient quantities of nitrogen, water & trace elements-the *real* rate-limiting factors in determining long-term plant growth. (6) several plant types (rice in particular) actually reduce their take up of certain trace elements (such as Zinc) when exposed to above normal levels of CO2. -
Marcus at 13:54 PM on 11 March 2011Interactive animation of the climate change impact on agriculture
"It is interesting that some of those present day farmers whose family holdings extends beyond two generations, are finding that some of the conditions they have experienced were similar instead to what confronted their grandparents." You want to back that up with some *evidence* John? Man, your ability to keep repeating the same falsehoods as though they're indisputable facts is getting somewhat tiresome. Your claims of some magic 30-year cycle is simply not backed up by the wealth of scientific data, nor is your claim that the NFF genuinely reflects the opinions of ordinary farmers backed up by the evidence I've seen & heard with my own senses. So unless you want to start backing up your claims with something approaching *real* evidence, then I simply don't see any point in arguing the case with you. According to PIRSA, btw, the science behind AGW is supported by both the SA Farmers Federation & the National Farmers Federation-so seems like your earlier claim isn't backed by the facts either. -
Tom Curtis at 13:54 PM on 11 March 2011Christy's Unconvincing Congressional Testimony
Rovinpiper @18 & 19, I tend to agree with your political analysis, but disagree with your suggestion on tactics. Expert witnesses called in support of action on climate change should not step outside of their expertise while giving testimony. It is not their role to do so, and it is unethical for them to do so. Further, it would be tactically disadvantageous because when they make mistakes (as they inevitably will speaking outside of their area of expertise), the mistakes will be seized upon and trumpeted through out the blog-0-sphere as a means of discrediting their expertise even in those areas where they are in fact expert. Rather, the tactic that should be adopted is some actual skill in questioning by the Democrats and rational Republicans on the committee. If Christy makes comments about economics, he should be pointedly asked what his claim to expertise in economics is. Given his publication record, his expertise on climate science should be actively challenged by trolling through the example after example of egregious error. I'm sure suitable comments on using the wrong sign for how many years was it? could be judiciously used to make him look a buffoon. The deniers have been playing hard ball on this issue for years, and more rational politicians have been soft on the issue for fear of losing votes. Its about time they toughened up and started pointing out that the emperor of the deniers has no clothes. -
Camburn at 13:53 PM on 11 March 2011Interactive animation of the climate change impact on agriculture
Albatross: I would caution you to use a grain of salt on relying on articles by Dr. Reich. I will stand with real world research from fields showing that additional co2 results in higher bio mass and crop yields. Also, Dr. Reich is wrong on higher co2 effects on corn. The root structure of co2 enhanced corn in unbelievable compared to normal levels of co2. I can only suggest that if you are going to comment on articles such as this that you do a lot more reading and stay abreast of the current research being done. The resutls that you are alluding to are not the results of real world experiments. -
Chris Colose at 13:41 PM on 11 March 2011What would a CO2-free atmosphere look like?
Peru, Keep in mind that clouds make up an extremely small amount of water in the actual atmosphere. From Trenberth and Smith (2005), there's generally about 250 times more water vapor (in mass per unit area) than liquid or ice in the air. I don't know how realistic the cloud feedbacks are in the Lacis paper (that would be a good question to ask the people in the study), but there's a lot of wiggle room to change the water vapor without changing clouds much. It's not the total water in the atmosphere that matters, but how you reach saturation, and lowering the temperature makes condensation easier. As for the albedo effect, the reason clouds are such a problem in the modern atmosphere is because they have two big terms (a longwave and a shortwave term) and constraining climate sensitivity amounts to figuring out the the very small difference between the two competing effects. In the snowball case though, the albedo effect of clouds isn't very important over bright surfaces, so they have an unambiguous warming effect on the snowball climate (as noted in Pierrehumbert 2002, as well as the coming review article). So your argument wouldn't really hold in this case. -
Rovinpiper at 13:29 PM on 11 March 2011Christy's Unconvincing Congressional Testimony
Notice also that other scientists were unwilling to go outside of their expertise but Christy didn't mind jumping right into economics. Trying to take the high road and stay within your expertise will win you no points in this sort of exercise. -
Rovinpiper at 13:28 PM on 11 March 2011Christy's Unconvincing Congressional Testimony
This was a win for the Republicans. All they need to show is controversy about the science and negative economic consequences of regulation. No one challenged Christy on his statements about day vs. night-time temperatures. No one pushed him to explain changes in outgoing and downward IR or stratospheric cooling. No one contested statements by Republican representatives or the skeptics about the negative impacts of regulation. They presented predictions of negative impacts from an increase in the price of energy. This is introductory level economics. People need to be reminded that economics is a model. We all now that model predictions should be validated against empirical data. We have some data now because of carbon emissions controls in the European Union and in part of the Northeast United States of America in the Regional Greenhouse Gas Initiative. These programs have not made those states into third world areas as Rep. Griffith assumes GHG regulation would do to the United States. -
Phila at 13:12 PM on 11 March 2011Examining Hansen's prediction about the West Side Highway
As a PS, Tom Curtis @54 has done a much better job than I of clarifying the difference between legitimate scrutiny and ideologically motivated ankle-biting. -
From Peru at 13:09 PM on 11 March 2011What would a CO2-free atmosphere look like?
In the Lacis et al (2010) paper "Atmospheric CO2: Principal Control Knob Governing Earth’s Temperature" it is shown (figure 1 in this post) that cloud cover remains roughly the same while the Earth cools (it even grows a bit at first before stabilizing at a constant value). How could this be possible, while the water vapor content of the atmosphere drops by 90%? Since clouds are formed by condensed water vapor, should not cloud cover decrease proportionally to the moisture decrease in the air, because there is less water vapor to make clouds? This is a very important point, because if the cloud cover drops while the sea ice cover grow, it is not clear if the total albedo of the planet would grow (due to more ice) or drop (due to less clouds). A cloud-induced drop in albedo would be a negative feedback that may prevent the Earth into entering a snowball state, if it is strong enough to compensate the loss of the greenhouse effect. -
Phila at 13:03 PM on 11 March 2011Examining Hansen's prediction about the West Side Highway
HR: There is nothing I can do if you feel the climate science establishment shouldn't be held to scutiny. This is yet another strawman. I didn't say or imply this, and I don't believe it. Frankly, I don't think you're helping your credibility with this comment. Two other points come to mind. First, AGW has been under incredible scrutiny, as you know perfectly well. I've been following this issue pretty carefully since 1990 or so, so I know that there are few major claims from the consensus side that haven't been challenged, questioned, parsed, anatomized, checked and rechecked repeatedly. That process continues today -- despite efforts to defund or slander the relevant agencies -- and I'm pretty confident that when important adjustments are made to AGW, or its predicted outcomes, they'll come from competent scientists, rather than a flock of willfully ignorant ideologues. Second, "scrutiny" of a scientific theory is valuable laregly to the extent that it comes from informed, intelligent, honest people who are not simply parroting frivolous criticisms they heard on a site like WUWT. We probably don't agree on much, but I hope we can agree on that. -
Tom Curtis at 12:44 PM on 11 March 2011Christy's Unconvincing Congressional Testimony
johnd @16, I find the suggestion that piers would dam the river more than mangroves (the natural river bank vegetation in Brisbane) interesting, but hardly credible. However, the suggestion that changes in geography between 1893 and 2011 rather than, say the 300 mm's (370 at Savages Crossing) rain in three hours dumped onto an already flooded river system are the major oontributor to Brisbane's flood is simply laughable. Below are the rainfall intensity graphs for Helidon (in the Lockyer Valley) and Lowood (just below the Wivenhoe dam wall) to give you some idea of the intensity of the rain involved. The primary flooding in Helidon is associated with the flash flooding in the Lockyer Valley on Monday 10th (google Grantham if you are unfamiliar with it); the peak at Lowood is associated with the second peak that fell mostly on the dam and surrounds. At the same time, Savage's Crossing (just east) received 370 mm in three hours. Note that the white dashed line on the graphs represents the expected intensity of a 1 in 2000 year event. The Helidon peak is associated with the first peak of inflows into Wivenhoe dam (dark blue line), the one at Lowood with the second peak. The dark red line indicates the peak flow at that location in 1974. Note, some areas of the catchment did not experience so intense rainfall, so that overall the intensity of the event over the period is about 1 in 200, but it is the peak falls over the Lockyer on the 10th that destroyed the Lockyer valley, and caused most of the flooding; and directly onto the dam and surrounds on the 11th, that necessitated the massive releases from the dam. And those events had probabilities of significantly less than 1 in 2000 per annum. -
Chris Colose at 12:43 PM on 11 March 2011What would a CO2-free atmosphere look like?
HumanityRules, I largely agree with you, but non-linearity in sensitivity is rather small over the ranges of climate of interest to us right now (e.g. http://www.nonlin-processes-geophys.net/18/125/2011/npg-18-125-2011.pdf ). Certainly you don't want to compare snowball Earths to say, the PETM directly, but I haven't seen anything suggesting it's a big deal for evaluating modern global warming. The effect isn't absolutely zero. Colman and McAvaney (2009) did this type of experiment from 1/16th to 32x modern CO2 and found a weaker sensitivity in the warm climate than in the cold cases, but it's not a large effect over a few degrees about the modern climate, so you don't really lose much by using the past as a guide to the future. The albedo feedback does get weaker in the warm simulations, but the water vapor grows in strength in warmer climates as well. The Colman and McAvaney paper have the lapse rate feedback increasing in strength too, essentially offsetting the water vapor feedback over most of the range (So the WV+LR feedback is positive the whole time, but not acceleratingly so), but I'm pretty skeptical of that. Eventually the water vapor feedback makes the sensitivity much higher, eventually getting you to a point where a runaway greenhouse is possible if your solar insolation is high enough. There's some other papers on this (e.g., Crucifix 2006, looking at the LGM vs. present) but the non-linearity is pretty small. -
michael sweet at 12:17 PM on 11 March 2011Examining Hansen's prediction about the West Side Highway
Tomurray: Do you hold Lindzen and Spencer to the same standard you hold Hansen? Remember that in 1988 Lindzen was predicting it would get colder in the next decade. Why are you still listening to him? -
Albatross at 12:12 PM on 11 March 2011What would a CO2-free atmosphere look like?
Well done Chris, you have got Lindzen there. That is just one of several misleading and/or false statements he made that day. -
bibasir at 12:03 PM on 11 March 2011What would a CO2-free atmosphere look like?
Really good article and discussion. It is a shame that someone did not answer Lindzens "guess" with some facts. Now the republicans and deniers go away thinking that CO2 is no big deal up or down. -
johnd at 11:39 AM on 11 March 2011Christy's Unconvincing Congressional Testimony
Tom Curtis at 11:27 AM, there is one dam that is being left out, and that is the city itself, and all the other infrastructure and changes that have occurred in the various water courses that artificially confines the natural flow paths. It is a common change that has happened on every water course where human occupation occurs. Geography has as much influence as the weather on all outcomes except for the timing of the events. -
Chris Colose at 11:39 AM on 11 March 2011What would a CO2-free atmosphere look like?
Bern, It's a good question. Impacts as well as internal heating source can certainly leave you very hot early in history, and in some cases can even push you over a threshold for the runaway greenhouse (tidal interaction with the Moon might have been a major heating source for Earth’s climate too in the first few millions of years). The bombardment period is relatively short though, and certainly the sun was a lot less luminous for a large deal of time when impacts were no longer critical. There's a lot to explore about this super-early stuff though in the context of habitability studies. The other thing is that not all stars evolve like our sun. M-type stars which constitute some 75% of all the stars out there are much more stable over geologic time (the lifetime on the main sequence for a star is inversely related to its mass, usually to a third or fourth power). M-stars are smaller and have a low effective temperature (only a few thousand degrees, in contrast to our own sun which is 6,000 K when it becomes optically thin enough for photons to escape) and so potential habitable planets need to be a lot closer to M-types. But with weak (and stable) luminosity, getting them out of a snowball state once they're in can be very tough. The volcanic outgassing of CO2 that helped Earth recover from snowballs in the past might be less meaningful, since a lot of these planets are so close to the sun that they are tide-locked (always having the same face to the sun) or at least close to it, so on the cold night side CO2 could condense out of the atmosphere faster than it is replenished by outgassing. -
scaddenp at 11:36 AM on 11 March 2011What would a CO2-free atmosphere look like?
"I was hoping you could help with understand something. I've started to think that climate sensitivity (CS) is not a constant figure through the history of the earth." A good question and one I would like to know answer to as well. It certainly seems to me that a planet of mostly ice would have a much higher sensitivity than one that is warm and ice-free. (change in albedo feedback - and change in water vapour feedback). PETM features are difficult to explain with sensitivity of around 3 (Zeebe, Zachos and Dicken 2009) - either its higher then or atmosphere has more methane. -
Tom Curtis at 11:27 AM on 11 March 2011Christy's Unconvincing Congressional Testimony
johnd @10, no! I make it seem, as it is, inappropriate, indeed dishonest, to compare flood levels from different periods without noting the effects of dams built on the river. If you want to defend that practice, please say so. I also rebut the casual repetition of false claims about the flood. Again, if you want to defend those false claims, speak up. Finally, I point out that the events of 2011 are extraordinary by any measure. But, if you had read my linked blog, you would have seen that those of 1893 were even more extraordinary by many measures. Wild weather and floods are a part of Brisbane's history. The only thing that is changing in that regard is that now mere thunderstorms are bringing floods comparable with those brought by cyclones in the past. All I can say is God help us when a cyclone next hits Brisbane in a La Nina year. -
What would a CO2-free atmosphere look like?
Chris Colose - Thank you! This is an excellent and thought-provoking thread. As a further investigation into this, for all concerned - looking at the historic (ice core) temperature record, it appears that temperatures rise (in the Earth system) much faster than they fall. Is this due to differences between the sequestration rates and release rates (clathrates, vegetation rot, vs. weathering, ocean release/uptake) upon phase change initiation? -
Chris Colose at 11:17 AM on 11 March 2011What would a CO2-free atmosphere look like?
On the interpretation of the bifurcation graph, a thing to note is that for very low or very high CO2 levels, the equilibrium states correspond to snowball or ice-free states, respectively. In between however, there are three solutions (indicated by the circles on the diagram). The intermediate solution (white circle) is an unstable one which separates the attractor basin of the upper warm solution with the colder ice-covered solution. It is here that nudging the climate into a warmer or colder direction will make it head to that new state rather than tending to bounce back to where it was. For further clarification, I'm putting a supplementary hysteresis loop (also in the Pierrehumbert paper) below: Here's an example situation to help read this. Suppose we start off in the warm climate state on the upper branch labeled W1. Now suppose you gradually lower the CO2 a bit. In this case you will get just a bit colder, say evolving toward W2, or decreasing the CO2 a bit more, to W3. This is a steady cooling you expect from lowering CO2, but it isn't an irreversible jump, and if CO2 returns to initial conditions you can return back to W1. However, suppose we decrease CO2 a lot, such that we reach W4 along the upper branch. This is a rather unstable case (like a ball on the top of a sharply peaked hill just getting ready to be nudged), and further tendency to cool will cause an abrupt jump to the S1 state. Physically, this is where an ice line starts to advance and the albedo feedback becomes very powerful. Also note that the water vapor feedback becomes negligible once you get tropical temperatures near freezing. Now if you return CO2 levels back to W2 likes conditions, you don't actually get to the W2 temperature. Now, you only warm a tiny bit to S2. In other words, because of the ice-albedo effect, you have multiple temperature solutions for a fixed solar irradiance and CO2 levels, and what state you're in also depends on the history to get there. Just how "left" and "right" the boundaries are of the hysteresis loop in the diagram in my post is ultimately critical in understanding how to get in and out of the snowball state. The Pierrehumbert diagram doesn't come from a full-blown GCM, and uses some simple parametrization (for example, what threshold global temperature is appropriate for ice-free conditions? He uses 290 K, but that's an assumption too. Also, how "dirty" is the ice, etc) so I wouldn't try to look an individual numbers too close with a magnifying glass, the point is the concept. -
Bern at 11:17 AM on 11 March 2011What would a CO2-free atmosphere look like?
Great article Chris, I quite enjoyed reading it. Regarding this bit: "This is a big problem in planetary habitability studies, especially if a planet succumbs to a snowball fate early in its history when the sun is faint. Once you begin to melt ice however, the temperature jumps rapidly to a very hot solution." Do these studies include the effects of asteroid impacts? As I understand it, the impact rate was substantially higher early in the Earth's history. Small impacts would result it localised heating, but larger ones can provide quite substantial 'kicks', both in terms of heating from the kinetic energy, and in terms of very rapid increases in CO2 levels. There's also the debris that would be spread globally, which would significantly affect albedo, and these combined effects could lead to substantial warming after the initial aerosol cooling subsided. -
Alexandre at 11:14 AM on 11 March 2011What would a CO2-free atmosphere look like?
HumanityRules #9 Good question. I often wondered if the persistent uncertainty range of CS, particularly the long tail at that longer geological study, could be due to such differences you mentioned. -
johnd at 11:08 AM on 11 March 2011Interactive animation of the climate change impact on agriculture
Marcus at 09:11 AM, who the NFF represents comes both directly, and indirectly through the various state bodies, and in turn the various industry bodies that do closely represent individual farmers. It would be interesting to find out if ordinary farmers consider that the Federal Government or the IPCC more closely represents their views. With regards to your mention of multi-generational family farms, because of the post WW2 soldier settlement scheme, in many areas of Australia, multi-generational means that a large number of family farms are only second generation. When they compare the conditions the present generation are facing, with that their parents faced, then obviously they are confined to a 50 -60 year period, but more importantly a period that their parents enjoyed that was not the normal when compared to what is known about Australia's longer term variable climate. It is interesting that some of those present day farmers whose family holdings extends beyond two generations, are finding that some of the conditions they have experienced were similar instead to what confronted their grandparents. With regards to the 30 year period you mentioned, which is generally taken to be the length of time that will represent a climate cycle rather than weather cycles. I think it is about time that this is re-evaluated as to whether it is still appropriate or not. When it was adopted about 100 years ago, the knowledge of weather and climate, both of then and past, was somewhat limited compared to today, as was the ability to measure and quantify all the relevant parameters. Like the concept of a flat earth, it came about reflecting the level of scientific understanding of the day. Obviously our understanding of both has progressed somewhat since those early days, and perhaps we should look to adopting a more appropriate time frame to define climate. -
muoncounter at 11:07 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
Tom, When you don't have substance, go with the rhetorical shortcuts. Here's a more recent discussion of the same work, including a more detailed map of lower Manhattan: A Columbia University study concluded that as sea levels rise, large parts of Lower Manhattan including Battery Park City, part of the World Trade Center site, and the Seaport will experience 10-foot floods after large storms. 1988? Yup, that's what it says up top. For Watt$ to be combing over this is a joke. -
dana1981 at 11:06 AM on 11 March 2011Christy's Unconvincing Congressional Testimony
Ian #13 - thanks for the link. Very good point from Santer about the (mis)use of the debunked Douglass et al. paper. I got hung up on the (worse, IMO) mistake of calling the 'hot spot' anthropogenic, and glossed over that error. Just goes to show what a horrendous Gish Gallop Christy's testimony was. We couldn't even catch all the errors therein in this long rebuttal! -
HumanityRules at 11:04 AM on 11 March 2011What would a CO2-free atmosphere look like?
Chris, I was hoping you could help with understand something. I've started to think that climate sensitivity (CS) is not a constant figure through the history of the earth. The impact of forcings in the form of feedbacks can be markedly different given the prevailling situation especially in the more extreme situations you describe in the final paragraph (snowballs, the PETM, glacial-interglacial cycles). For example the cryospheres in these periods will be very different with very different ice albedo feedback, another issue might be land cover and the biosphere, maybe you can think of more situations. I'm concerned that when scientist attempt to make CS estimates are they making estimates for the version of earth that was prevailing at the time and that this is different to the version we are living through now. Can you help with were I'm going right or wrong and describe how scientists deal with that problem (if it exists)? -
Riduna at 11:02 AM on 11 March 2011The Earth's Sixth Mass Extinction May Be Underway
As far as we know, there have been 5 events causing mass extinction of biota. Those events all have at least 5 things in common. 1. Their effect was global 2. All caused atmospheric changes 3. In geological terms they occurred rapidly 4. All resulted in loss of >50% of plant and animal species 5. All were characterised by destruction of habitat. The most serious of these events was the Permian Extinction which resulted in the loss of >90% of plant and animal species. So severe was this event that rebound of life-forms took 15 million years. In this and other extinction events, deep ocean warming, possibly caused by warming of the earths mantle, resulted in the melting of clathrates. This resulted in triggering of the so called “Methane Gun”, the release of massive amounts of methane from the ocean bed over a prolonged period, though possibly only a few centuries. As this methane percolated from the ocean bed to the surface, it oxidized to form CO2 and in the process deoxygenated ocean waters, causing the death of marine flora and fauna on a massive scale. Both gases may have become atmospheric pollutants, though possibly not as serious as the release of aerosols from volcanism or asteroid collision. Atmospheric pollution would have prevented or at the very least limited photosynthesis and produced rapid cooling, at some stage countered by diminution of aerosols and increase of CO2 and other greenhouse gases. The most vulnerable to extinction events are plants and animals unable to rapidly adapt to increasing atmospheric pollution, those with small populations or large body size and those dependent on limited diet. It is not clear that we are now at the start of an Extinction Event but we may well be, though on this occasion one triggered by the human species rather than “natural” volcanism. What is clear is that if unchecked in the very short term, greenhouse gas pollution will cause relatively rapid global warming having the same effects as those characterising earlier extinction events. Shakhova (2010) has already reported that warming of the ocean and seabed off the Siberian coast is already beginning to melt methane clathates. The result is that atmospheric concentration of methane in the Arctic has already reached the highest levels known in 400,000 years. No less concerning is her estimate that destabilisation of offshore permafrost could result in accelerated melting of clathates with an estimated capacity to release 70 billion tones of methane into the ocean. In addition, melting of Siberian marshland permafrost has potential to increase this total. Significant quantities of methane from shallow offshore waters are likely to reach the atmosphere without oxidizing. The bulk, from deeper water, would oxidize before reaching the surface, reducing oxygen in the Arctic Ocean. Both would add to the level of CO2 in the atmosphere further accelerating global warming, placing the environment of biota under increasing stress. It is possible that we may not be approaching the next Extinction event but the signs are ominous and the past provides a stark warning of what lies ahead unless we act promptly to curb greenhouse gas emissions. -
Albatross at 11:02 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
Not to be pedantic Muoncounter, but this is about what was said in 1988, not 1998. But I agree with your point, it is absurd, and pathetic that people are having to debunk this nonsense being spread by WUWT and others. Hopefully concrete in cheap post 2050 to increase the height of the the sea walls-- hmm, but making concrete is CO2 intensive.....oh dear, another positive feedback loop. -
Tom Curtis at 10:54 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
Muoncounter @55, interesting, but Hansen still consistently predicts greater sea level rises than the consensus position. It is, therefore, certainly justified to examine his independent predictions, so long as you actually do so rigorously (see 54). Of course, the deniers are simply taking rhetorical short cuts rather than actually examining Hansen's predictions. -
muoncounter at 10:50 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
This is getting more and more absurd. In a normal scientific review process, the 1998 interview would be long forgotten, as it was superseded by this more recent research brief. The two models suggest that ocean waters in this area could rise another 18 cm to 60 cm by mid-century, as the planet warms. By the 2080s, sea level could climb by 24 cm to nearly 110 cm ... As sea level rises, flood levels produced by the 100-year storm could reach 3 to 3.8 meters by the 2050s, and between 3.2 to 4.2 meters by the 2080s. --emphasis added So its not sea level rise alone, its the combination of sea level rise and the 100 year storm that floods the West Side. -- Figure 2 ... the current 100-year flood return period would shorten dramatically. By the 2080s, the likelihood of a flood engulfing the area in blue (Figure 2) would be once in 50 years, given present rates of sea level rise, and as often as once every 4 years, in the worst-case scenario. Given the huge percentage of NYC's infrastructure that is underground, this should be a serious concern, because there is no 3 meter sea wall around lower Manhattan. Instead its become a denialist playground. Go figure. -
HumanityRules at 10:49 AM on 11 March 2011What would a CO2-free atmosphere look like?
Chris Colose, I'd agree with you the Lindzen picked a number off the top of his head but the wider issue of CO2 as a GHG is not disputed by Lindzen (video 26-27mins). -
Tom Curtis at 10:48 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
HR @51, we absolutely believe the scientific community should be held up to scientific scrutiny. The first step in that process is to examine the predictions made in scientific articles or conference proceedings rather than equivalent predictions made of the cuff in interviews. It is very clear that the former will be more precise, and will more accurately reflect the considered views of the scientist. (If the of the cuff remarks widely differ from the considered views, that raises a separate issue, but no one has suggested that to be the case.) The second step is, where there is any ambiguity as to what was meant (which is certainly the case in this example) is to clarify with the author the actual intended meaning. Did Hansen mean 40 years regardless of CO2 levels? Did he mean 40 years, provided that CO2 levels had doubled? Or did he mean 40 years after CO2 levels had doubled? The exact interpretation makes a very large difference as to whether or not the prediction has been (or will be) falsified in 2018. Neither WUWT nor you have taken either of these steps. The notion that you are trying to hold Hansen up to scrutiny is therefore nonsense. In fact, what WUWT appears to be doing is to raise a straw man of Hansen's views in order to make him the subject of ridicule. Finally, if you want to subject Hansen's views to genuine scientific scrutiny, you need to remember that any prediction is based on multiple claims. Because the purpose of scientific scrutiny is to test those claims, where some of those claims are already modified, the prediction needs to be altered accordingly. Let's assume (contrary to what I believe is the most natural interpretation), that Hansen predicted that: "If CO2 levels double by 2028, the West Side Highway in New York will be under water." The theory underlying that prediction is based on Hansen's model work of that period. So it includes the sub-beliefs that: a) CO2 levels can plausibly to double by 2028; b) Climate sensitivity is 4.2 degrees C per doubling of CO2; and c) A 4.2 degree C rise of global temperatures above preindustrial levels will raise sea levels sufficiently to flood the West Side Highway. For scientific scrutiny, (b) is now irrelevant. The evidence, partly published by Hansen himself, shows the climate sensitivity is more probably 3 degrees C. Now, should we test Hansen's predictions without substituting for (b), (b') that climate sensitivity is 3 degrees C, and altering the prediction accordingly, then all we test in the prediction is the conjunction of (a), (b), and (c); which is boring because we already know (b) is probably false. In other words, if in fact the West Side Highway is not under water in 2028, all we learn is that either CO2 has not doubled, or climate sensitivity is lower than 4.2, or sea rise at 4.2 degrees C is not sufficient to flood the West Side Highway. As we are already fairly certain about the second of those possible conclusions, we learn virtually nothing. So, if you really want to examine Hansen's position: 1) Find, if possible, an equivalent prediction from the period in his primary literature; 2) Clarify any ambiguity if any; and 3) Adjust the prediction to allow for recent advances in knowledge. And if you are not prepared to do that, you are not holding Hansen up to scientific scrutiny - you are indulging a rather tawdry rhetorical ploy. Just don't expect us to be deluded by it. -
scaddenp at 10:23 AM on 11 March 2011Dispelling two myths about the tropospheric hot spot
Well the Douglass et al paper ignored radiosonde biases despite the authors apparently being aware them. See Santer et al to see why that paper disappeared. The other two I am unaware of. Got a link to them? Cant find either in easily in google scholar. -
GFW at 10:20 AM on 11 March 2011What would a CO2-free atmosphere look like?
Ranyl, I think the dashed lines are not "real" states. What really happens, if if you're on one of the lower solid lines and you increase CO2 so much that you run out of solid line, then the temperature rapidly increases until you reach the upper solid line at the same CO2 level. If CO2 now drops (because all that melted ice has exposed rock that can weather) you slide down the upper solid line. If it drops enough, you "fall" from the upper solid line to the lower solid line (for the right ice albedo). -
Ian Forrester at 10:18 AM on 11 March 2011Christy's Unconvincing Congressional Testimony
Michael Tobis has some scathing comments from Ben Santer on Christy's testimony. -
RickG at 10:12 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
HR: It's 17 years until Hansens speculation, but more generally the satellite data is still failling to show anything but a linear rise. Come on HR, you have been shown time and time again that Hansen did not put a time frame on the sea level rise. The reference was a doubling of CO2. There's not a single scientist on the planet speculating that a CO2 will double by 2028. What does it take for you to understand that? -
Tom Curtis at 10:10 AM on 11 March 2011What would a CO2-free atmosphere look like?
Chris, I enjoyed the article, and hope it is to be the first of many on this site. Can you confirm that the sections of the bifurcation graph with dashed lines are transition states? That is, once the CO2 level reaches high enough a level to start melting ice in a snowball earth scenario, the temperature will continue warming until it reaches that of the equivalent for the equivalent CO2 level in the ice free state; and if CO2 levels drop below the minimum to maintain the upper solution, the earth would cool to a snowball state at the appropriate temperature for that CO2 level? Are they also unstable state? Ie, if the glaciation and CO2 levels where those at the white dot on the graph, could an equilibrium be maintained, or would it inevitably transition to one of the grey dots due to changes in albedo? Finally, I notice that in the non-snowball Earth case, at 666 ppm the model clearly indicates the Earth to be ice free. As the model was using less than current insolation, doesn't this mean the model is predicting an eventually ice free Earth for doubling of CO2 from current levels? -
Albatross at 09:54 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
HR @49, "If your data is correct then New York should be one of the spots on the earth were accelerating SLR should be showing up earliest." First off, they are not "my" data. Second, that is your interpretation of the paper which is talking about future GSL. Nice try though. That said, this satellite-derived map of GSL, does show a hot-spot for GSL rise (> 5 mm/yr) off the northeast coast of Canada for the period 1993-2009. [Source here] -
HumanityRules at 09:50 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
45 Phila There is nothing I can do if you feel the climate science establishment shouldn't be held to scutiny. There is nowhere for our discussion to go from here. Again your appeal is that you want the discussion to be limited to what you think is relevant, you don't seem to be able to see that. There is plenty I disagree with on this site but I never(I think!) try to limit the scope of the discussion. Finally the title of the article is "Examining Hansen's prediction about the West Side Highway". That's what I'm trying to do, you seem to think the title is "Bash WUWT". Look if John wants to post an article with that title I'd be happy to join the conversation there if I thought I was going to get something from it. -
Tom Curtis at 09:40 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
tomurray @43, I have read the original post at WUWT. I noticed, for example how they carefully showed the windows of the offices of not only Hansen, but also Schmidt (who was totally unconnected to the article), two men known to have received death threats. (I also read their very weak defense of that action in the comments.) I also noticed how they are taking an ambiguous prediction from a casual interview rather than the equivalent prediction from Hansen's scientific work (which would be precise, and not in need of interpretation) as the basis of their commentary. Finally, I also notice that you have set up a standard whereby if what Hansen has predicted for the 2090's is not fulfilled by the 2010, then his work (all of it, apparently) can be dismissed. Finding pretexts to dismiss evidence may be preferable (for some) to actually understanding the evidence. However, it does not impress. -
HumanityRules at 09:37 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
25 Albatross Albatross all that modelling work is fine but did you look at the data presented by Charlie A in #20. If your data is correct then New York should be one of the spots on the earth were accelerating SLR should be showing up earliest. I don't see it in the on the ground data, it looks pretty much linear. When are we going to start to see this exponential growth? It's 17 years until Hansens speculation, but more generally the satellite data is still failling to show anything but a linear rise. -
Albatross at 09:35 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
Tomurray, "He needs to be right all of the time." No, that is a fallacy. Applying your logic we should not be funding the National Weather Service in the USA to issue warnings for severe weather because they are not correct 100% of the time. Yet, there is immense value in their warnings. Same goes for medical doctors-- and they get payed much, much more than does Hansen. You are being unrealistic and are not grounded in reality. I hope you now realize the folly of your reasoning. I strongly suspect that you are placing unrealistic expectations to set someone up for a fall, just so it can reinforce your skewed perception of reality and dismiss their inconvenient findings. I do agree that Hansen should be held to a high standard, and he is, pretty much every word he says is scrutinized. What would be disappointing (and telling) is if you did not apply your critique or skepticism equally, that is what a true skeptic would do. So I find it odd that you do not concede that Watts is misrepresenting what Hansen actually intended to communicate. And let us not be naive, Watts is embarking on an orchestrated misinformation campaign and relishes in defaming climate scientists. -
Gordon1368 at 09:23 AM on 11 March 2011Examining Hansen's prediction about the West Side Highway
@46 tomurray In fact, he does defend all of his positions within the scientific community. There is no error in his statement. If CO2 doubles, whenever it doubles, sea levels will rise a meter. No one doubts that. You are grasping at straws, which only shows how weak your position is. -
ranyl at 09:21 AM on 11 March 2011What would a CO2-free atmosphere look like?
Interesting post Chris. This graph is fascinating, if you raise CO2 in the partially ice covered state and follow the dashed lines a rising CO2 results in a global cooling which is none mechanistic. Therefore presuming a rising temperature with a rising CO2, could the increase go vertically so to speak? Could a rising temperature due to radiative forcing (like the changig alebdo effect)in the partially ice covered earth cause jumps in temperature? Can temerpatures of the top line be reached before the ice melts followed by the melt? Antarctica is going to take a long time to melt even if the world rose several degrees c. What does this sort of graph mean for climate sensitivity? Interesting graph, when is the Pierrehumbert et al., 2011, accepted paper being published?Moderator Response: [mc] Use width=500 or smaller within img tags. -
Marcus at 09:11 AM on 11 March 2011Interactive animation of the climate change impact on agriculture
John D "I have no doubt that you associate and talk to others who share similar views as yourself. Whether or not they are representative or not is another matter. Are you also sure they are not concerned more about short term weather events such as droughts?" First of all, my work doesn't allow me to *choose* who I associate or talk to-any more than it does my colleagues-yet still the majority of the farmers we come in contact with express a deep level of concern about global warming-not short term weather effects, as you suggest, but explicit mention of global warming (though they do mention its impacts on things like droughts, which most of them have noticed getting worse over the last 30 years). Second of all, do you *honestly* think that an organization like the NFF genuinely represents the view of the majority of ordinary farmers? That's like saying the ACTU represents the view of the majority of blue-collar workers. Indeed, the view I get from the farmers themselves is that the NFF really only represents the views of the so-called "agri-businesses", or "factory farms", not the views of multi-generational family farms. -
muoncounter at 08:56 AM on 11 March 2011A Scientific Guide to the 'Skeptics Handbook'
KR, I second your props to John. Regular contributors to this site: See the Organizational Nominees at George Mason University's 2011 climate change communicator award. Vote early, vote often!
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