Some of the Missing Energy

Guest Post by Willis Eschenbach

The canonical equation describing the energy balance of the earth looks like this:

∆Q (energy added) = ∆U (energy lost) + ∆Ocean (energy moving in/out of the ocean)                                                          (Equation 1)

This has been modified in the current climate paradigm (e.g. see Kiehl) by substituting in the following:

∆U (energy lost) = [∆T (change in surface temperature) / S (climate sensitivity)]                                                           (Equation 2)

which gives us

∆Q (energy added) = [∆T (change in surface temperature) / S (climate sensitivity)] + ∆Ocean (energy moving in/out of the ocean) (Equation 3)

As I detailed in “Where Did I Put That Energy“, the problem is that the data doesn’t bear out the substitution. In the real world, ∆U is very different from ∆T/S. There’s a whole lot of energy missing. I think that some of it is here:

Figure 1. Tracing the path of a tiny bit of energy through a simplified climate system.

Why does this count as some of the missing energy?

Note that all of the energy goes into evaporating the molecule of water. As a result, there is no net change in the surface temperature. Since the definition of the climate sensitivity is ∆T/∆Q, and ∆T is zero, that means that for this entire transaction the climate sensitivity is zero.

It is important to remember that Equation 1 is still true, and this situation complies with Equation 1. The amount of energy entering the system equals the amount leaving plus ocean storage (zero in Fig. 1). However, it does not comply with equation 2 or 3.

This certainly qualifies as a possible mechanism for the missing energy. Response time is fast, and it can move huge amounts of energy from the surface to the condensation level and eventually to space. Also, it is outside the ambit of the the climate sensitivity calculation, since the climate sensitivity for this transaction is zero.

Is this all of the missing energy? Can’t be. The missing energy is moving in huge amounts in both directions, both into and out of the system. However, the mechanism above is one-way. It can remove energy from the system, but not add energy. I say the extra energy added in the other direction comes from clouds clearing out when the temperature drops. But that is another story for another post.

My conclusion? Climate sensitivity is not a constant, it is a function of temperature. Note for example that the warmer the water, the larger a percentage of the incoming energy takes the path illustrated in Fig. 1. The formation of the clouds and thunderstorms is also temperature dependent. All of which makes the climate sensitivity strongly temperature dependent.

As always, questions, corrections, and suggestions are more than welcome.

w.

PS – Please don’t say “but you left out the greenhouse gases”. Yes, I did, but in this case they have almost no effect. The transport of the heat to the upper troposphere takes place in the thunderstorm, so it is protected from thermal exchange with the troposphere. At the top of the troposphere, where it leaves the thunderstorm, there is little atmosphere of any kind. From there it is free to radiate to space with little interference.

And in any case, GHGs will only modify rather than rule the effect. Sure, we might end up with a bit of surface warming rather than zero as in the above analysis. But the essence of the transaction is that surface temperature is not directly coupled to radiation. This means that the substitution done to get Equation 3 is not correct.

PPS — In fact, the system above does more than have zero effect on the surface temperature. When the thunderstorm starts, albedo goes up, storm winds increase evaporation, cold wind and rain from aloft chill the surface, and other cooling mechanisms kick into gear. As a result, the surface ends up cooler than when the thunderstorm started, giving negative climate sensitivity. But that is another story for another post as well.

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December 27, 2010 9:01 pm

Jim,
I don’t know the answer. I don’t even know whether your question is soundly based.
Pamela,
Very interesting and curious. I await developments.

Spector
December 28, 2010 2:07 pm

I think it is rather interesting that the top of the troposphere is literally the point where the atmosphere runs out of ‘steam’ or ‘water vapor’ as a result of condensation.
Whenever two water molecules join to form an H2O–H2O pair, the pair will initially have as much energy as if it were about 100 degrees C warmer then the individual molecules did before. I suspect that photon radiation from energetic condensing water vapor plumes may be an overlooked heat export mechanism. Note that an H2O–H2O pair actually has less mass than one single CO2 molecule.

David Socrates
January 13, 2011 11:20 am

Pamela Gray says:
December 25, 2010 at 5:40 am
I also find Stephen Wildes blog responses rather confusing but still gid value. If you are going to haul him over the coals for not being a good enough professional scientist to distinguish a hypothesis from a theory then I shal haul you over the coals for constantly confusing the words “affect” and “effect”.
So there!

Brian H
January 13, 2011 5:22 pm

DS;
A very effective rebuke! I can vicariously feel the sting from here. 😉

January 13, 2011 7:12 pm

Thanks for the support, chaps but I’ve had to put up with worse than what Pamela said and she did back off later in the thread when she seemed to start seeing my point.
Equations and words are just different means of expression. Words are best for a general overview with equations best for detailed application.
In climate issues we don’t have the general overview right yet so in my opinion words are more helpful to a lay reader and more effective to get across the general concepts than equations.
Intellectual snobbery is ill advised since those who are best with equations are often the worst with words and vice versa.

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