Forcing The Ocean To Confess

Guest Post by Willis Eschenbach

According to the current climate paradigm, if the forcing (total downwelling energy) increases, a combination of two things happens. Some of the additional incoming energy (forcing) goes into heating the surface, and some goes into heating the ocean. Lately there’s been much furor about what the Levitus ocean data says about how much energy has gone into heating the ocean, from the surface down to 2000 metres depth. I discussed some of these issues in The Layers of Meaning in Levitus.

I find this furor somewhat curious, in that the trends and variations in the heat content of the global 0-2000 metre layer of the ocean are so small. The size is disguised by the use of units of 10^22 joules of energy … not an easy one to wrap my head around. So what I’ve done is I’ve looked at the annual change in heat content of the upper ocean (0-2000m). Then I’ve calculated the global forcing (in watts per square metre, written here as “W/m2”) that would be necessary to move that much heat into or out of the ocean. Figure 1 gives the results, where heat going into the ocean is shown as a positive forcing, and heat coming out as a negative forcing.

annual forcing into out of the oceanFigure 1. Annual heat into/out of the ocean, in units of watts per square metre. 

I found several things to be interesting about the energy that’s gone into or come out of the ocean on an annual basis.

The first one is how small the average value of the forcing actually is. On average, little energy is going into the ocean, only two-tenths of a watt per square metre. In a world where the 24/7 average downwelling energy is about half a kilowatt per square metre, that’s tiny, lost in the noise. Nor does it portend much heating “in the pipeline”, whatever that may mean.

The second is that neither the average forcing, nor the trend in that forcing, are significantly different from zero. It’s somewhat of a surprise.

The third is that in addition to the mean not being significantly different from zero, only a few of the individual years have a forcing  that is distinguishable from zero.

Those were a surprise because with all of the hollering about Trenberth’s missing heat and the Levitus ocean data, I’d expected to find that we could tell something from the Levitus’s numbers.

But unfortunately, there’s still way too much uncertainty to even tell if either the mean or the trend of the energy going into the ocean are different from zero … kinda limits our options when it comes to drawing conclusions.

w.

DATA: Ocean temperature figures are from NOAA, my spreadsheet is here.

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Ximinyr
June 19, 2013 8:59 pm

w: here’s an explanation more in the language you’ve used.
you’ve shown there is a small trend in the annual forcing, that isn’t statistically significant at the 2-sigma level (but is at some lower level).
but even an unchanging forcing, i.e. a constant forcing, means the ocean is warming — some number of W/m2 is going into the ocean on a constant basis. more joules every second.
that *heats* the ocean, until the forcing=0.
a zero *forcing* keeps the ocean at a constant temperature (i.e. constant OHC), not a constant forcing.
you haven’t understood what you’re really calculating. this is a wrong post all around.

Kristian
June 19, 2013 9:21 pm

Willis Eschenbach says, June 19, 2013 at 3:57 pm:
“Neither the solar flux, nor the downwelling longwave radiation (DLR) from the atmosphere, nor the upwelling longwave radiation (ULR) from the surface, is a flow of heat. They are all flows of energy. Heat, on the other hand, is a NET energy flow.”
Eh, have you even read my posts? Where do I say anything to the contrary? That’s my whole point. There is no NET flow of IR, as you call it, to the surface from the atmosphere. Hence, there is no HEAT, as I call it, going from the atmosphere to the surface. The NET radiative energy goes from the surface to the atmosphere. There is no IR from the atmosphere that can increase the internal energy of the surface, because on average more always goes the other way. The posited 390 UP and 324 DOWN fluxes are part of the same exchange and the spontaneous flow of NET energy (‘heat’) that results is going UP. That’s my whole point.
If we agree on this, which we appear to do, there is no quarrel.
The solar flux, however, is clearly a heat flux. It warms the Earth. It brings the surface a NET contribution of energy – heat. It is most important to separate between systems when looking at heat flows. There’s the ‘exchange’ between Sun and Earth’s surface. That is +168 W/m^2. Radiative HEAT coming IN (of course there is such a thing, that is the thing, that’s the thing that’s actually measured/detected, not the inferred individual fluxes). Then there’s the ‘exchange’ between Earth’s surface and atmosphere/space. That is (324-390=) -66 W/m^2. Radiative HEAT going OUT. (Of which 26 go to the atmosphere and 40 go directly to space.) Then you have that other heat loss flux from the surface which is the convective one (conduction/convection + evaporation). Convective HEAT going OUT. This is -102 W/m^2 on average. It all goes to the atmosphere.
(-66-102=) -168 W/m^2 of total HEAT escapes the surface. Balancing the incoming from the Sun.
This is the heat budget of the Earth’s surface. It is balanced. 168 in, 168 out.

David Riser
June 19, 2013 9:34 pm

Well Ximinyr,
I am pretty sure that if the ocean heat content has an average effect of increasing the averaged temperature of the ocean by less than a .1 degree C over the course of 60+ years; for most of that time we were taking a very small number of measurements; and those measurements were taken had a greater uncertainty than .1 degree C than this is logically not significant.
If you have to take a measurement such as the oceans temperature and turn it into energy and then graph it so it looks huge and significant your not doing anyone any favors. Particularly if the data it is based on is not statistically significant.

Ximinyr
June 19, 2013 9:43 pm

David Riser: i am told that ARGO sensors can measure temperature to ~0.01 C.
it does not matter if you are talking about heat gain or temperature — they are proportional. the oceans have a huge volume, so a small temperature change means a lot of heat change.
what do you think is the change in avg ocean temperature from a glacial to interglacial period?

Manfred
June 19, 2013 10:16 pm

The variation in figure 1 is again totally implausible.
There is a mean of 0.2 W/m2 representing the oceans heat uptake due to total forcing of about 1.6 W/m2 since 1955
(IPCC at about 2.4 today, about 0.8 in 1950).
http://i81.photobucket.com/albums/j237/hausfath/ScreenShot2012-12-13at43419PM_zps4a925dbf.png
Every upside variation has to be associated with a reduction in cloud cover.
The effect of a 3% decrease in cloud cover is believed to represent a forcing of 1-1.5 Wm-2 (Rossow and Cairns, 1995, Svensmark has similar numbers).
Observed cloud cover changes amount to only a few percent over a year. Therefore cloud reduction forcing has at maximum been about the size of the total forcing.
Any yearly variation in figure 1 exceeding about 0.2 W/m2 is then not plausible.
Larger variation must then be a measurement error. Such errors may level out during long term measurements similar to very noisy sea level data.
But this does not apply to the largest error in 2003-2005 due to equipment change to ARGO. This false step increase in ocean heat content will not be corrected by future ARGO data.

phlogiston
June 19, 2013 10:22 pm

The AGW paradigm of the ocean is ludicrously simplistic. It treats the oceans as a passive puddle. Only external “forcing” (what a deeply ignorant word) can change its temperature and heat content. However the oceans own internal dynamics with oscillations on century and millenial scales drive heat and temperature changes in the upper ocean, bearing in mind the overwhelming majority of climatic heat content being in the ocean. Measured temperature trends in the upper ocean allow very little if anything to be concluded about in-out heat budget.

June 19, 2013 10:23 pm

I love this graph. It is easy to understand, and it shows how little change there really has been.

Manfred
June 19, 2013 10:24 pm

Ximinyr says:
June 19, 2013 at 7:04 pm
you are calculating the trend of d(OHC)/dt, not the trend of OHC
—————————
Yes, because Willis was talking about d(OHC)/dt, What is your point ???
The trend in OHC is approx. equal to the mean, also given in figure 1. Its all there…

David Riser
June 19, 2013 10:51 pm

Ximinyr says
David Riser: i am told that ARGO sensors can measure temperature to ~0.01 C.
Actually ARGO sensors are not that accurate nor are they the same type or design of sensor across the fleet. Nor is the accuracy of other ocean temperature sampling methods prior to ARGO that accurate. for a interesting read on the issue:
http://earthobservatory.nasa.gov/Features/OceanCooling/page1.php
To go from Cooling to Heating based on the accuracy of your measurements is precisely what Willis is talking about.

David Riser
June 19, 2013 11:22 pm

Well actually I should say ARGO are typically calibrated to .001C however none of the manufacturers will say exactly how accurate they are in the operating environment of an ARGO float for a wide variety of reasons. ARGO claims .005C yet they have to quality check the data and there are frequently issues with them. The Ocean Cooling page goes into a lot of detail on some issues they have had but really the record before ARGO was so bad that when ARGO came online it showed cooling…. So they had to correct the record…..So they do Quality changes to their data….. So I am saying that there accuracy leaves a lot to be desired…

ironargonaut
June 19, 2013 11:52 pm

Why bother to entertain the change in subject? The climate scientists said temperature was going up and would continue to rise. Hockey stick anyone. They did not say heat content would rise like a hockey stick. Temperature and heat are two different things. If they want to discuss ocean heat then say fine first lets discuss land and atmosphere heat rise from 1900. Anthony’s graph show no rapid rise in land heat content.

Matthew R Marler
June 20, 2013 12:06 am

Willis,
Another good post, and good responses to other commenters. Many thanks.

Manfred
June 20, 2013 12:34 am

Willis Eschenbach says:
June 19, 2013 at 11:54 pm
…Mmmm … I’ve grown careful about words like “every” and “all”. There’s at least three ways to increase the amount of heat in the ocean.
1. Increase the energy input.
2. Decrease the losses.
3. Increase the residence time.
Again, mmm … and again, there are more ways to increase the energy input than to decrease the cloud cover. One main one, which functions as a major thermal control mechanism in the tropics where most of the energy enters, is to vary not the amount of clouds but their timing. A one-hour delay in the average onset time of the tropical clouds leads to about 60 W/m2 of additional incoming energy. On a 24/7 basis, that comes down 2.5 W/m2 increase in forcing.
No, larger variations can easily be due to rearrangements of the clouds, and alterations in their time of onset and disappearance.
Part of the problem is that you are looking at the average effects of clouds. But take a typical tropical day. Clouds during the day have a strong cooling effect, hundreds of watts per square metre.
Clouds in the night have a weaker effect, which is in the opposite direction, a warming effect.
So if we have twelve hours of clouds, the average cloud cover is the same whether the clouds are there in the day or the night. But the thermal effect is totally different, by hundreds of watts/m2. My point is that although the average cloud cover doesn’t vary much … that doesn’t mean much.
—————————————————–
Agree, there are such rearrangements and timing chances etc, but to what extent for a whole year and globally ?
And even if, the peaks are too large to be explained by any such mechanism:
4% reduced cloud cover corresponds approximately to the IPCC average 1955-today forcing and this correponds to a heat uptake of 0.2 W/m2
But there are yearly heat uptake values of 2.3 W/m2 in the dataset. Subtract 0.2 due to “global warming” and 2.1 W/m2 remain to be explained !
2.1 W/m2 heat uptake not forcing..This would then correspond to a cloud cover reduction of 42% (or an alternative rearrangement) globally and for a whole year.

Kristian
June 20, 2013 1:11 am

Willis Eschenbach says, June 19, 2013 at 10:08 pm:
Yes, always the same old bluster without substance when entering this subject: “You don’t know physics! Your ideas are deeply flawed! Go read a textbook and learn something! All physicists disagree with you!” And so on and so forth.
And that’s that.
Could you rather than rambling please address what I asked from Bart upthread?
“What is ‘heat’ to you? Does it fly around in every direction? Show me how my definition of ‘heat’ goes against the agreed upon physical definition. Show me how the atmosphere is a source of heat for the surface, how it transfers heat downwards.”
I have no problem admitting when I’m wrong, Willis. I am not wrong on this one.
I will however concede one point. I shouldn’t have quoted that whole paragraph of yours when claiming my argument didn’t oppose it. I was actually referring only to the last line: “Heat, on the other hand, is a NET energy flow.”
How does what I’ve written above go against this notion?
You mix up individual and opposing energy fluxes in an exchange between two systems and the ‘net’ flux between them, the heat transfer. Only heat transfer transfers … heat (increase in internal energy for the cool system, decrease in internal energy for the warm system).
There is nothing novel in my definition of heat, Willis. Heat is energy transferred from a hot to a cold system. This transfer (the ‘net’ flow of energy) only goes one way. Pertaining to the radiative interaction between Earth’s surface and Earth’s atmosphere, the transfer goes UP and only up.
You can look this up anywhere. This is not a warped idea om mine.
What happens when you introduce the upwelling and downwelling IR fluxes between surface and atmosphere in the energy budget diagrams, is that you confuse people’s perception of what is actually physically going on. You give the impression that the atmospheric flux is equivalent to the solar flux. It is not. The inferred 324 flux is not an independent, extra flux of energy coming down to the surface, like the solar flux. The 324 W/m^2 down could not increase the internal energy of the surface, and therefore could not heat it, because on average it would always be opposed by a larger flux going up (the equally inferred 390 W/m^2 flux). The 324 is the LESSER PART of an assumed continuous IR exchange between the two systems, the result of which is an upward radiative heat flux of 66 W/m^2. (Well, since you’re seemingly so against the term ‘heat flux’, then use the term ‘net energy flux’ instead.) You cannot include the one and exclude the other. They are two sides of the same coin (exchange process).
In what way is this wrong, Willis?

Kristian
June 20, 2013 2:16 am

Willis Eschenbach says, June 20, 2013 at 2:03 am:
“Heat is the net energy flow. It is unidirectional, and always goes from hot to cold.”
Thanks. That’s all I’m saying. Still you seem to be arguing that the inferred downward atmospheric radiative flux is somehow capable of heating the surface/ocean (like the solar flux) to a higher temperature than what the Sun could manage on its own. Even if we appear to agree that the ‘net’ radiative flux (the heat) between surface and atmosphere always on average goes up, the surface/the ocean radiatively loses ‘net energy’ (heat) to the atmosphere. Go figure.
How does heat loss make warmer?

Eric H.
June 20, 2013 2:19 am

Willis Eschenbach says:
June 19, 2013 at 10:57 am
Eric H. says:
June 19, 2013 at 6:38 am
Thanks Willis,
Some of my own ponderings: 1) If it cannot be shown that CO2 is heating the ocean then CAGW is done as a theory. 2) LWIR is only capable of penetrating water at a depth of millimeters and the amount of heat transfer rate change from an increase in CO2s LWIR is dwarfed by the amount of LWIR from clouds. 3) SWR can penetrate the ocean to a depth of 30 meters (if my memory serves) and changes in cloudiness and/or solar activity would have a much greater impact to OHC than LWIR from all sources. Is this correct?
Not really, or at least that’s not all there is to it. Once it strikes the ocean, long-wave infra-red (LWIR) is converted from radiant energy to thermal energy, so it adds energy to the ocean. See my post Radiating The Ocean for a “full and frank” discussion of the issues.
w.
Thanks Willis and Ian for your responses but I am not trying to argue that LWIR cannot heat the ocean my question is one of effectiveness which I apologize if this was lost in my post. The point I was trying to make is that changes in solar output and/or cloudiness are better explanations for an increase in OHC than CO2 due to a greater ability of solar and clouds to raise ocean temperatures. If clouds and solar cannot be ruled out then CO2 cannot logically be the cause. If CO2 can’t be shown to be the cause of increased OHC then CO2 cannot be the driver of climate change…
What I appear to have wrong was my thought that SWR was a greater forcing than LWIR which I incorrectly thought was due to penetration:
“So if the DLR isn’t heating the ocean, with heat gains of only the solar 170 w/m2 and losses of 390 w/m2 … then why isn’t the ocean an ice-cube?”
Again, thanks for the info, Eric

kadaka (KD Knoebel)
June 20, 2013 2:19 am

From Kristian on June 20, 2013 at 1:11 am:

There is nothing novel in my definition of heat, Willis. Heat is energy transferred from a hot to a cold system.

An object can be heated to where the wavelength distribution peak for the energy emitted is strongly in the ultraviolet, the predominant emissions amounts are UV. Significant UV emissions come from the Sun, but also arc welding, and the rarefied gas inside a fluorescent tube yields little but UV.
The UV travels and strikes a fluorescing surface, resulting in the production of visible light. The UV wavelength energy transferred from the hotter object to the cooler object (surface) that is transformed to visible light, is heat?

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