Sense and Sensitivity

Guest Post by Willis Eschenbach

This is an extension of the ideas I laid out as the Thunderstorm Thermostat Hypothesis on WUWT. For those who have not read it, I’ll wait here while you go there and read it … (dum de dum de dum) … (makes himself a cup of coffee) … OK, welcome back. Onwards.

The hypothesis in that paper is that clouds and thunderstorms, particularly in the tropics, control the earth’s temperature. In that paper, I showed that a falsifiable prediction of greater increase in clouds in the Eastern Pacific was supported by the satellite data. I got to thinking a couple of days ago about what other kinds of falsifiable predictions would flow from that hypothesis. I realized that one thing that should be true if my hypothesis were correct is that the climate sensitivity should be very low in the tropics.

I also figured out how I could calculate that sensitivity, by using the change in incoming solar energy (insolation) between summer and winter. The daily average top of atmosphere (TOA) insolation is shown in Figure 1.

Figure 1. Daily TOA insolation by latitude and day of the year. Phi (Φ) is the Latitude, and theta (Θ) is the day of the year expressed as an angle from zero to 360. Insolation is expressed in watts per square metre. SOURCE.

(As a side note, one thing that is not generally recognized is that the poles during summer get the highest daily average insolation of anywhere on earth. This is because, although they don’t get a lot of insolation even during the summer, they are getting it for 24 hours a day. This makes their daily average insolation much higher than other areas. But I digress …)

Now, the “climate sensitivity” is the relationship between an increase in what is called the “forcing” (the energy that heats the earth, in watts per square metre of earth surface) and the temperature of the earth in degrees Celsius. This is generally expressed as the amount of heating that would result from the forcing increase due to a doubling of CO2. A doubling of CO2 is estimated by the IPCC to increase the TOA forcing by 3.7 watts per metre squared (W/m2). The IPCC claims that the climate sensitivity is on the order of 3°C per doubling of CO2, with an error band from 2°C to 4.5°C.

My insight was that I could compare the winter insolation with the summer insolation. From that I could calculate how much the solar forcing increased from winter to summer. Then I could compare that with the change in temperature from winter to summer, and that would give me the climate sensitivity for each latitude band.

My new falsifiable predictions from my Thunderstorm Thermostat Hypothesis were as follows:

1 The climate sensitivity would be less near the equator than near the poles. This is because the almost-daily afternoon emergence of cumulus and thunderstorms is primarily a tropical phenomenon (although it also occurs in some temperate regions).

2 The sensitivity would be less in latitude bands which are mostly ocean. This is for three reasons. The first is because the ocean warms more slowly than the land, so a change in forcing will heat the land more. The second reason is that the presence of water reduces the effect of increasing forcing, due to energy going into evaporation rather than temperature change. Finally, where there is surface water more clouds and thunderstorms can form more easily.

3 Due to the temperature damping effect of the thunderstorms as explained in my Thunderstorm Thermostat Hypothesis, as well as the increase in cloud albedo from increasing temperatures, the climate sensitivity would be much, much lower than the canonical IPCC climate sensitivity of 3°C from a doubling of CO2.

4 Given the stability of the earth’s climate, the sensitivity would be quite small, with a global average not far from zero.

So those were my predictions. Figure 2 shows my results:

Figure 2. Climate sensitivity by latitude, in 20° bands. Blue bars show the sensitivity in each band. Yellow lines show the standard error in the measurement.

Note that all of my predictions based on my hypothesis have been confirmed. The sensitivity is greatest at the poles. The areas with the most ocean have lower sensitivity than the areas with lots of land. The sensitivity is much smaller than the IPCC value. And finally, the global average is not far from zero.

DISCUSSION

While my results are far below the canonical IPCC values, they are not without precedent in the scientific literature. In CO2-induced global warming: a skeptic’s view of potential climate change,  Sherwood Idso gives the results of eight “natural experiments”. These are measurements of changes in temperature and corresponding forcing in various areas of the earth’s surface. The results of his experiments was a sensitivity of 0.3°C per doubling. This is still larger than my result of 0.05°C per doubling, but is much smaller than the IPCC results.

Kerr et al. argued that Idso’s results were incorrect because they failed to allow for the time that it takes the ocean to warm, viz:

A major failing, they say, is the omission of the ocean from Idso’s natural experiments, as he calls them. Those experiments extend over only a few months, while the surface layer of the ocean requires 6 to 8 years to respond significantly to a change in radiation.

I have always found this argument to be specious, for several reasons:

1 The only part of the ocean that is interacting with the atmosphere is the surface skin layer. The temperature of the lower layers is immaterial, as the evaporation, conduction and radiation from the ocean to the atmosphere are solely dependent on the skin layer.

2 The skin layer of the ocean, as well as the top ten metres or so of the ocean, responds quite quickly to increased forcing. It is much warmer in the summer than in the winter. More significantly, it is much warmer in the day than in the night, and in the afternoon than in the morning. It can heat and cool quite rapidly.

3 Heat does not mix downwards in the ocean very well. Warmer water rises to the surface, and cooler water sinks into the depths until it reaches a layer of equal temperature. As a result, waiting a while will not increase the warmth in the lower levels by much.

As a result, I would say that the difference between a year-long experiment such as the one I have done, and a six-year experiment, would be small. Perhaps it might as much as double my climate sensitivity values for the areas that are mostly ocean, or even triple them … but that makes no difference. Even tripled, the average global climate sensitivity would still be only on the order of 0.15°C per CO2 doubling, which is very, very small.

So, those are my results. I hold that they are derivable from my hypothesis that clouds and thunderstorms keep the earth’s temperature within a very narrow level. And I say that these results strongly support my hypothesis. Clouds, thunderstorms, and likely other as-yet unrecognized mechanisms hold the climate sensitivity to a value very near zero. And a corollary of that is that a doubling of CO2 would make a change in global temperature that is so small as to be unmeasurable.

In the Northern Hemisphere, for example, the hemispheric average temperature change winter to summer is about 5°C. This five degree change in temperature results from a winter to summer forcing change of no less than 155 watts/metre squared … and we’re supposed to worry about a forcing change of 3.7 W/m2 from a doubling of CO2???

The Southern Hemisphere shows the IPCC claim to be even more ridiculous. There, a winter to summer change in forcing of 182 W/m2 leads to a 2°C change in temperature … and we’re supposed to believe that a 3.7 W/m2 change in forcing will cause a 3° change in temperature? Even if my results were off by a factor of three, that’s still a cruel joke.

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lgl
March 4, 2010 6:23 am

Willis Eschenbach (01:57:20) :
Here’s a paper on energy transport: http://www.cgd.ucar.edu/cas/Trenberth/trenberth.papers/i1520-0442-21-10-2313.pdf
I think fig.1 a) contradicts your claim “that the albedo is highest in the Southern Hemisphere in February”. True for the tropics, but the opposite at higher latitudes.
And why are you trying to convince people that 10 meters is a representative mixed layer depth?
“We’re interested in about the top ten metres or so, that’s where the action of the sunlight is greatest. When diving there is often a pronounced thermocline around that depth”
This isn’t science. It doesn’t matter where the action of the sunlight is greatest when the heat is mixed tens or hundreds of meters down (or what your close to shore diving is telling you).

TLM
March 4, 2010 8:14 am

I think what you are doing here is setting up the proverbial “straw man”, that is countering an argument that hasn’t been made. Nobody is saying that positive feedbacks work within a single year!
Many of the positive feedbacks hypothesised gradually build up over a number of years, not from season to season.
The main ones are:
1. warming releases CO2 from the oceans which reinforces the anthropogenic release of CO2. The warming of the oceans in response to increased back-radiation from CO2 in the atmosphere would likely take decades, not a single season.
2. a decline in Arctic summer sea ice reduces the albedo of the oceans at high latitudes during the period of greatest insolation at that time of year leading to greater absorption of the back-radiation. Again, warming of the oceans is a long-term phenomenon – not a Winter/Summer one.
3. warming increases the anaerobic breakdown of vegetation currently locked up in permafrost which releases methane. Again a multi-year effect.
4. warming of the oceans may prompt the release of methane clathrates. This would definitely take several decades.
All of these have counter arguments but your paper sets out to address why positive feedback does not occur when it gets warmer in Summer. What is the point?

Steve Koch
March 4, 2010 10:54 am

TLM,
In 2005, Hansen predicted that ocean heat content (ohc) would rise significantly in the next few years. He was very specific in his prediction (IIRC it was something like 10^22 joules increase in ohc/year).
That did not happen, as ohc instead levelled off and recently is declining. The question is why was Hansen’s model falsified? Maybe increased cloud cover has something to do with it.

Grizzled Wrenchbender
March 4, 2010 2:57 pm

To take the dynamic effects out of the model, perhaps you can compare the insolation anomalies to the temperature anomalies _at the extremes of temperature_ (which lag the sun by about six weeks). The off-peak sun at peak (average daily) temp should give a reasonable approximation to dT/dF for the earth as a whole.

Alexander Harvey
March 4, 2010 4:22 pm

Willis,
You need to determine the admittance into space, whereas you seem to have determined the total admittance of the system Y = F/T and viewed the two as equivalent
You need to subtract out the other admittances to obtain the admittance into space but you have not. Nor do you seem to have quantifiied them in any detail. You do express an opinion about only the top ten metres being significant but do not seem to have quantified the effect of that.
The Surface Mixed Layer, also know as the Well Mixed Layer, is on average substantial and varies by season and latitude, you may find various figures quoted, but the greater range seems to be from 10-500 metres. It tends to be low at the equator and greatest in midlatitudes. I gave admittance values for 50m and 100m well mixed layers. But it does not end there. Once you have settled on a depth estimate for a well mixed layer, you have to connect it to the ocean below. This is another susceptance which on average may be equivalent in effect to a another 20m well mixed layer for a 12 month cycle ~ 15W/K plus a conductance of ~15W/K due to diffusion down into the lower levels.
Based on those figures the total oceanic admittance for a 50m well mixed layer would be ~45W/K and for a 100m layer ~85W/K. These are significant values that I simply do not think can be ignored.
I equated your CS value for midlatitudes ~25W/K (for land and ocean) in my last above. I do not know what figures you get for land and ocean seperately. But if you get figures in or below the range 45-85W/K over the ocean then they could be due to oceanic admittance alone.
Finally, if the admittance into space over the oceans were say 25W/K and that only the top ten metres of the ocean is significant (8W/K of susceptance).
You have 25W/K of conductance and only about 8W/K of susceptance which leads to a phase angle of about 18 degrees of arc which is much the same as 18 days which is considerably less than the couple of months plus that typically occurs.
(If the figure you get for the conductive admittance into space over the oceans is greater than 25W/K, the phase angle would be even smaller.)
On the other hand a system with just an ocean comprising of a well mixed 50m and a diffusive lower ocean would have a phase angle of around 70 degrees (or days), which is more in the ballpark.
Over the land, 25W/K of conductance would imply only about one week of phase lag in landlocked areas (assuming an admittance due to the atmosphere of around 3W/K) not the ~3 weeks that actually occurs.
Now I do not know what figures you have for land and ocean seperately. But I expect that you get a smaller admitance than 25W/K over the land, making the resultant phase angle more reasonable, but an admittance greater than 25W/K over the ocean implying an even smaller phase angle for the case where only the top 10 metres of the ocean were worth considering.
I do not know what figures you would get for these phase angles so I can not comment further.
I think my views are quite clearly that: the problem is ill-conditioned (see my previous), that the oceanic admittances are poorly quantified and vary with latitude, that you have taken a view that the effects of the admittances of the land, atmosphere, and oceans are insignificant and have hence failed to make any allowances for them.
I doubt that I can be of more assistance other than advise you to produce a range of results based on a plausible range of oceanic, atmospheric, and land admittances, and see where that leads you. I rest on that final thought.
Alex

Boris
March 5, 2010 7:11 am

Richard,
Your post is once again nonsense. I see a lot of hand waving about climate states. But the state that we are in, if correctly described by Willis, suggests an enormous amount of energy is necessary to move us to a glaciation. If you disagree, then what positive feedback amplifies the cooling? And why would this positive feedback not amplify the warming?

slow to follow
March 5, 2010 3:32 pm

Willis – this is a quick observation on the fly having just seen the dialogue above with DeWitt Payne re: albedo.
How is the graphic you show in comment Willis Eschenbach (01:57:20) generated? One obvious thing that strikes me is the image seems to show stronger reflection off land which is more perpendicular to the suns rays with the Sahara and the Andes appearing “seasonally constant”. Is that what you mean by albedo being a response to the forcing?
Re: the graphic – Has this image been generated by a timelapse composite? Does it have any calibration? How is cloud cover treated?
From a very rough counting squares approach I get the land area between the tropics to be about 1/5 of the Earth’s surface. Hence land’s seasonal impact on the albedo is going to be factored accordingly as one would expect sea water to have an albedo which is constact with angle of incident light. My understanding is that the tropics account for the vast majority of received insolation and that the oceans are the major recipients and distributors of solar energy in this zone.
I had a quick look at the graphic 1a) that Igl references and it shows the monthly albedo anomaly from the annual average. The -20deg to +20deg latitude bands seem consistent with your graphic.
Apologies if all this is either covered above, irrelevant or plain wrong; it’s an “on the fly” observation in case any of it is relevant/helpful – I haven’t read all the comments or your “Thermostat” article but I like your use of daily and seasonal insolation variation to get another view on sensitivity values.

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