John--Not at all. It is not at all linear.
Mike
Hi John--I don't really understand your thinking on this. CO2 forcing is logarithmic in concentration. IR radiation is proportional to the fourth power of temperature. If you are saying things are sort of linear with small change, okay, but you were going back to the Earth with no GHGs and that is not linear. In addition, the calculation of 33 C is based on a planetary average, daily average calculation rather that considering the day-night cycle, latitudinal effects or not. Without any GHGs, the Earth would be like the Moon--get heated in sunlight and go to very cold temperatures at night. the oceans would largely be frozen and there would be no clouds so the albedo would be very different--lower if no water and clouds at all, higher if there were water and frozen. And you seem to be mixing up climate sensitivity with equilibrium temperature.
I just don't think this discussion is on a useful track at all.
Mike
Hi Mike,
It should be linear to a first approximation. A doubling of GHG forcing should move the equilibrium temperature about twice as far from where it would have been without any GHG forcing. There must be another explanation if 16C equilibrium temperature is way out. I'd hoped you'd come out with it.
BTW, who's equilibrium temperature do you support, since there are many around? David Wasdell has the highest I've seen, but nowhere near 16C. Some seem to be as low as 3C - my foot.
Cheers, John
On Sun, Mar 1, 2026 at 1:47 AM Michael MacCracken <mmac...@comcast.net> wrote:
John--Not at all. It is not at all linear.
Mike
On 2/28/26 5:04 PM, John Nissen wrote:
Hi Mike,
Without GHGs the planet would be 33C cooler at equilibrium. Water vapour provides about half the GHG effect [1]; let's say 17C, leaving 16C from CO2, methane, etc. The doubling of CO2e should add another 16C to the planet's equilibrium temperature, assuming water vapour hasn't changed (which it has, upward) and assuming albedo hasn't changed (which it has, downward). Does this mean that the equilibrium temperature for CO2e doubling (which we've very nearly reached) must be in the region of 16C above the pre-industrial times when the ES was in equilibrium. This is far from the 1.5C that we have reached.
The implication is that temperature rise is proportional to the GHG level to a first approximation. If net zero is reached in 2050, by which time CO2e will certainly have doubled, the planet will continue to warm towards the equilibrium temperature which will be far higher. The idea that the temperature will "stabilise" at net zero is fundamentally flawed. To lower the global temperature, cooling intervention is required with a cooling power greater than the heating power from excess GHGs - and from increased H2O and lost albedo to boot. This could amount to over 4 W/m2 or 2 petawatt couldn't it?
Cheers, John
Water vapor is Earth’s most abundant greenhouse gas. It’s responsible for about half of Earth’s greenhouse effect — the process that occurs when gases in Earth’s atmosphere trap the Sun’s heat. Greenhouse gases keep our planet livable. Without them, Earth’s surface temperature would be about 59 degrees Fahrenheit (33 degrees Celsius) colder.
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Hi John--The temperature of 255 K for the world with no atmosphere is just solving the Stefan-Boltzmann equation for the temperature assuming a 30% albedo for the amount of energy going in and out. The mid-20th century average of observed temperature around the world was about 15 C (or about 288K), and the difference is 33 C. So nothing detailed at all. The surface temperature depends on both water vapor and CO2 GH effects. I don't think you can divide them as you are thinking and I don't think that they are linear, and each develops feedbacks and those will depend on the temperature at any given point. It is just not possible to linearize based on the 33 C difference.
If you want to get a natural estimate of climate sensitivity, seek to get it from Earth's climatic history. Soviet scientists did this and got 3 C for the sensitivity given the climatic state we are in now. Hoffert and Covey in a paper in Nature 30 some years ago did an analysis and got about the same central value that gives about the same range as IPCC is using. In my view, if the sensitivity is well higher than this, it is hard to see how the temperature through the Holocene could have been as nearly stable as it was. And then also, if it is significantly smaller that 3 C, it is hard to understand how we could have had such a large range between glacial and interglacial conditions.
It is also not clear that the sensitivity is the same for all types of forcings. As I mentioned, using the IPCC approach to evaluation, orbital parameter changes have virtually no global and annual average effect, but drove the quite large glacial-interglacial changes in climate just by redistributing solar energy by season and latitude. Exerting a change in radiative forcing in the atmosphere versus at the surface (i.e., above or below the water vapor GH effect) can have an effect (see past modeling studies by Govindasamy. Bala). Changing baseline amounts of sea ice, etc., can have an effect on the sensitivity, and the timescales of some feedbacks can change how fast one sees a response (e.g., consider times for subsidence and rebound to occur).
So, the simple attempt at reckoning you are attempting is fraught with problems. What Jim Hansen is doing is looking at various processes and feedbacks, so much more intimately at how the models are working, and looking at consistencies and inconsistencies with observations and responses and suggesting the most general sensitivity may be toward the upper limit of the typical uncertainty spread. Interesting to be doing, but making sure you are quantitatively consistent across all possible hidden feedbacks and relationships is really hard to be sure of--and is why the range suggested in the IPCC assessments has not narrowed much at all. We've got enough of a likelihood of global catastrophe in terms of impacts if the climate sensitivity is only 2 or 2.5 C given the consequences that can be seen in Earth history of a warming (e.g., during Eemian interglacial about 120-125 ka, global average temperature was maybe 1 C over preindustrial and sea level was 10 to 20 meters higher than at present). My recommendation is to just stick to the agreed sensitivity, and if the resulting impacts aren't viewed as serious enough to cause alarm and action, then we are likely doomed, so we need to keep working to educate people about impacts--we are at 1.5 and Arctic region is being seriously disrupted and we are not yet at equilibrium, especially for the cryosphere. Turning the climate ship from its present course will take time and waiting until it gets fully turned is too late to change things--as the UNFCCC states, the appropriate decision framework to use is the Precautionary Principle--doing so certainly instead of using the scientific tradition of mainly focusing on changes in the likely central value given that it is likely that it is the fairly unlikely extremes that will be wreaking havoc.
Best, Mike
Hi John--Most of the items that make you suspicious are short-term--looking over longer scales, atmospheric composition and continental drift (e.g., mountain building, altering of ocean currents) are major factors.
On the albedo issue and 33 C, indeed choosing 30% is arbitrary--but that is what was done, along with it being a zero dimensional calculation.
On your comment about 1940 to 1970 cooling, in my view, the peak in warming during WWII is an artifact--a bias created by various issues regarding ocean conditions (change in measurement methods, mix of ships, and more) that does not really show up over land. Put your finger over the WWII time period and you get a different perspective on what was going on. Also, of course, the cleaning up of air pollution by lofting pollution through tall stacks instead of emissions at ground level that blackened cities di increase the likely sulfate loading a lot, as surface emitted SO2 has a lifetime of a day or two so little contribution to tropospheric haze whereas lofted emissions likely have a lifetime of a week or two and so are the real creators of the tropospheric haze. I do agree that reduced marine SO2 emissions have likely reduced the planetary albedo, which is why I've supported the idea of widely dispersed injection of SO2 into the mid- to upper troposphere, especially over low albedo remote ocean areas as a possible cooling intervention. In my view, doing this would be more spread out and efficient than just stepping down the marine emission standard out over the ocean.
And I agree with you on benefits of refreezing the Arctic and am working on some thoughts about this (first have to convince myself about it).
Best, Mike
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Dear Paul--
Over the Amazon, where it is wet, it will be lower temperature because it takes energy to evaporate water vapor. As water vapor builds us and is trapping IR, the region warms and the air starts to rise. As it rises, it can hold less water vapor, so water vapor condenses and gives up energy to the atmosphere, warming it and causing the air to rise more and rain out more, etc. So, yes, that there is water there does hold down peak temperature, but the air is saturated and so heat index can be way up.
For the Sahara, with air going up elsewhere, air is coming down over the desert from an altitude where most moisture has been rained out when the air rose. So, as it comes down and is compressed, it warms up. With no water vapor, there will be no clouds. So, during the day most of the incoming sunlight reaches the surface and heats things up. There being no water vapor to evaporate, temperatures can get very warm during mid-day, but also, with virtually no water vapor in the atmosphere, so no greenhouse effect and the temperatures can drop at night to quite cool temperatures (even down to the dew point of the boundary layer air below the inversion that was created by the downwelling air. Relative dry air, even if hot, is generally not as uncomfortable--just go in the shade and it is better-- to endure as hot, saturated air. So, yes, temperature is different but would be better if the enthalpy, I think it is, were the comparative measure so it includes the thermal and latent energy content.
Mike MacCracken
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