Accuracy, Precision, and One Watt per Square Metre

Guest Post by Willis Eschenbach

I’ve been investigating one of my favorite datasets in the last few days, the CERES satellite-based top-of-atmosphere (TOA) radiation dataset. In particular, I’ve taken month-by-month global and hemispheric averages of the data. The dataset consists of observations of three variables—downwelling solar radiation, upwelling longwave (infrared) radiation, and upwelling shortwave radiation (reflected sunlight). From these I derive a further dataset. This is the top-of-atmosphere (TOA) imbalance. It is calculated as downwelling solar minus upwelling (reflected) solar minus upwelling longwave. That gives a fascinating look at the overall radiation picture.

I got to thinking about this because of a curious claim in a recent paper published in Nature Climate Change entitled Model-based evidence of deep-ocean heat uptake during surface-temperature hiatus periods (paywalled). I did love the whole concept of “model-based evidence”, but that wasn’t what caught my eye. It was this statement (emphasis mine):

There have been decades, such as 2000–2009, when the observed globally averaged surface-temperature time series shows little increase or even a slightly negative trend (a hiatus period). However, the observed energy imbalance at the top-of-atmosphere for this recent decade indicates that a net energy flux into the climate system of about 1 W m−2 (refs 2, 3) should be producing warming somewhere in the system (refs 4, 5). Here we analyse twenty-first-century climate-model simulations that maintain a consistent radiative imbalance at the top-of-atmosphere of about 1 W m−2 as observed for the past decade. [References are listed at the bottom of this post.]

Anyhow, here’s some news regarding that claim of a consistent TOA imbalance, from the CERES satellite dataset:

global top-of-atmosphere radiation

Figure 1. CERES satellite-measured top-of-atmosphere (TOA) radiation levels, starting in January 2001. Numbers on the horizontal axis are months. Shown are the solar energy entering the system (red line), solar energy leaving the system (dark blue line) and longwave (infrared) energy leaving the system (light blue line). The overall monthly imbalance at the TOA is shown at the bottom in purple. The 12-month running average for each variable is shown as a thin line. Curiously, the variations in upwelling longwave are about 6 months out of phase with the downwelling radiation. All radiation values are positive. TOA Imbalance is solar less reflected solar less outgoing longwave, i.e. inflow less outflow. Twelve-month averages vary too little for the changes to be visible at this scale. 

Now, there are a number of things of interest in this chart. The first is the fact that while the seasonal variations are fairly large, tens of watts per square metre, the annual variations are so small. At this scale we can hardly see them. So let’s expand the scale, and take a more close-up look at just the variations in the overall TOA energy imbalance (purple line at bottom of Figure 1). Figure 2 shows that result.

toa imbalance ceres datasetFigure 2. Closeup of the overall energy imbalance. Horizontal scale is months. Narrow line shows running centered 12-month averages of the TOA imbalance data. All radiation values are positive. TOA Imbalance is solar less reflected solar less outgoing longwave, i.e. inflow less outflow.

Here, we can begin to see the small variations in the 12-month running average. However, the average itself is around five watts per square metre … not good. That much out of balance is not credible.

This shows the difference between precision and accuracy. You see that the measurements are obviously quite precise—the 12-month running average only varies by about three-quarters of a degree over the whole period.

However, in absolute terms they’re not that accurate, we know that because they don’t balance … and it’s very doubtful that the earth is out of balance by five watts per square metre. That’s a very large amount, it would be noticed.

Now, I’ve previously discussed how James Hansen deals with this problem. He says:

The precision achieved by the most advanced generation of radiation budget satellites is indicated by the planetary energy imbalance measured by the ongoing CERES (Clouds and the Earth’s Radiant Energy System) instrument (Loeb et al., 2009), which finds a measured 5-year-mean imbalance of 6.5 W/m2 (Loeb et al., 2009). Because this result is implausible, instrumentation calibration factors were introduced to reduce the imbalance to the imbalance suggested by climate models, 0.85 W/m2 (Loeb et al., 2009).

As a result, Hansen used the Levitus data rather than the CERES data to support the claims of a ~ one watt per square metre radiation imbalance. However, all is not lost. The precision of the CERES data very good. In Figure 2 we can see, for example, how one year’s TOA radiation imbalance  is different from another. So let’s expand the scale once again, and take an even closer look at just the 12-month running averages, for all four of the radiation measurements shown in Figure 1.

anomalies 12 month averages ceres datasetFigure 3. An even closer look, this time at just the tiny variations in the 12-month running averages of the CERES data as shown in Figure 1. All radiation values are positive. TOA Imbalance is solar less reflected solar less outgoing longwave.

Now we’re getting somewhere.

The first thing I noticed is the precision of the measurements of the downwelling solar radiation (red line). As you might expect, the sun is quite stable, it doesn’t vary much compared to the variations in reflected solar and upwelling longwave radiation. And the observations reflect that faithfully. So it seems clear that their instruments for measuring  radiation are quite precise.

Next, I noticed that the change in the imbalance (purple) is more related to the change in reflected solar (dark blue) than to the variations in upwelling longwave. I’ve highlighted the reflected solar (dark blue) in the graph above. This is confirmed by the correlation. The R^2 between TOA imbalance and reflected solar is 0.67; but between TOA imbalance and upwelling longwave, R^2 is only 0.07.

This seems like an important finding, that the imbalance is mostly albedo related, and that because of variation in the albedo, the variations in the reflected solar energy were on the order of ± three tenths of a watt within a few years.

Finally, I am once again surprised by the overall stability of the system. Twelve-month averages of all three of the variables (the TOA balance, reflected solar, and upwelling longwave) are all stable to within about ± 0.3 watts per square metre. Out of a total of 340 watts per square metre going each way, that’s plus or minus a tenth of one percent … I call that extremely stable. Yes, with a longer sample size we’d likely see greater swings, but still, that’s very stable.

And that brings me back to the quotation from the paper where I started this post. They say that there is

a consistent radiative imbalance at the top-of-atmosphere of about 1Wm−2 as observed for the past decade …

Now, according to their references [2] and [3], this claim is based on the idea that the excess energy is being soaked up by the ocean. And this claim has been repeated widely. I’ve discussed these claims here. The claims are all based on the Levitus ocean temperature data, which shows increasing heat in the ocean. Here’s my graph of the annual forcing needed to give the changes shown by Levitus in ocean heat content:

annual forcing into out of the oceanFigure 4. Annual forcing in watts per square metre needed to account for the energy going into or coming out of the ocean in the Levitus data. Data is for the top 2,000 metres of water. Note that despite average values being used, both by Hansen and also in the study under discussion, neither the mean nor the trend are statistically significant. Further discussion here.

For current purposes, let me point out that Figure 4 shows that in order for the ocean to gain or lose the energy that is shown in the Levitus data, it requires a very large year to year change in the amount of energy entering the ocean. That energy has to come from somewhere, and it has to go to somewhere when it leaves the ocean. Since the solar input is about constant over the period, that energy has to be coming from a change in either the upwelling longwave or the reflected solar … and we have precise (although perhaps inaccurate) data from CERES on those. Fortunately, the lack of accuracy doesn’t matter in this case, because we’re interested in the year to year changes. For that all we need is precision, and the CERES data is very precise.

So … let me compare the forcing shown by the Levitus ocean heat content in Figure 4, with the CERES data. Figure 5 shows the difference.

anomalies levitus 12 month averages ceres datasetFigure 5. Forcing given by the Levitus ocean heat content data, compared to the CERES data shown in Figure 3.

As you can see, they have a couple of big problems with their claims of a consistent 1 W/m2 imbalance over the last decade.

First, it is contradicted by the very data that they claim establishes it. There is nothing “consistent” about what is shown by the Levitus data, unless you take a long-term average.

The second problem is with the Levitus data itself … where is the energy coming from or going to? While the CERES TOA imbalance is not accurate, it is very precise, and it would certainly show a fluctuation of the magnitude shown in the Levitus data. If that much energy were actually entering or leaving the ocean, the CERES satellite would surely have picked it up … so where is it?

I’ve discussed what I see as unrealistic error bars in the Levitus data here. My current comparison of Levitus with the CERES data does nothing to change my previous conclusion—the precision of the Levitus data is greatly overestimated.

Finally, the idea that we have sufficiently accurate, precise, and complete observations to determine the TOA imbalance to be e.g. 0.85 watts per square meter is … well, I’ll call it premature and mathematically optimistic. We simply do not have the data to determine the Earth’s energy balance to an accuracy of ± one watt per square metre, either from the ocean or from the satellites.

Best regards to all,

w.

MY OTHER POSTS ON THE CERES DATA:

Observations on CERES TOA forcing versus temperature

Time Lags In The Climate System

A Demonstration of Negative Climate Sensitivity

DATA:

CERES data: Unfortunately, when I go to verify it’s still available, I get:

The Atmospheric Science Data Center recently completed a site wide redesign.  

It is possible that the page you are looking for is being transitioned.  Please try back later.

If the page you have requested is still not available, it may have been renamed or deleted.

It is recommended that you use the Search interface on the ASDC Web Site to find the information you were looking for.

Since I got there via the aforementioned “Search interface on the ASDC Web Site”, I fear we’re temporarily out of luck.

[UPDATED TO ADD] I’ve collated the global and hemispheric monthly averages from R into a “.csv” (comma separated values) Excel file available here.

Levitus data

REFERENCES FOR THE NATURE CLIMATE CHANGE ARTICLE:

2. Hansen, J. et al. Earth’s energy imbalance: Confirmation and implications.

Science 308, 14311435 (2005).

3. Trenberth, K. E., Fasullo, J. T. & Kiehl, J. Earth’s global energy budget.

Bull. Am. Meteorol. Soc. 90, 311323 (2009).

4. Trenberth, K. E. An imperative for climate change planning: Tracking Earth’s

global energy. Curr. Opin. Environ. Sustain. 1, 1927 (2009).

5. Trenberth, K. E. & Fasullo, J. T. Tracking Earth’s energy. Science 328,

316317 (2010).

 

0 0 votes
Article Rating

Discover more from Watts Up With That?

Subscribe to get the latest posts sent to your email.

158 Comments
Inline Feedbacks
View all comments
Gail Combs
August 30, 2013 11:26 am

steveta_uk says: August 30, 2013 at 10:24 am
Even if the CERES hardware is extremely accurate, how much confidence is there that it is capturing all energies at all wavelenghts? For example, if it was missing part of the UV spectrum the reflective figures could be low by about the 4-5 W/m2 mark.
>>>>>>>>>>>>>>>>>>
FWIW:

EVE: Measuring the Sun’s Hidden Variability
…explains Tom Woods, a solar physicist at the University of Colorado in Boulder. “If you want to get a good look at solar activity, you need to look in the EUV.”…..
When the sun is active, solar EUV emissions can rise and fall by factors of hundreds to thousands in just a matter of minutes. These surges heat Earth’s upper atmosphere, puffing it up and increasing the air friction, or “drag,” on satellites. EUV photons also break apart atoms and molecules, creating a layer of ions in the upper atmosphere that can severely disturb radio signals.
To monitor these energetic photons, NASA is going to launch a sensor named “EVE,” short for EUV Variability Experiment, onboard the Solar Dynamics Observatory this winter.
“EVE gives us the highest time resolution and the highest spectral resolution that we’ve ever had for measuring the sun, and we’ll have it 24/7,” says Woods, the lead scientist for EVE. “This is a huge improvement over past missions.”
…..

MORE:

Quick Facts: Solar Dynamics Observatory/EUV Variability Experiment (SDO/EVE)
Launch date: February 11, 2010
LASP Instrument
The EVE instrument is designed to measure the solar extreme ultraviolet (EUV) irradiance. The EUV radiation includes the 0.1-105 nm range, which provides the majority of the energy for heating Earth’s thermosphere and creating Earth’s ionosphere (charged plasma). This wide spectral range requires the use of multiple channels. Some key requirements for EVE are to measure the solar EUV irradiance spectrum with 0.1 nm spectral resolution and with 20 sec cadence. These drive the EVE design to include grating spectrographs with array detectors so that all EUV wavelengths can be measured simultaneously. Another key requirement for EVE is to measure the EUV radiation with an accuracy of 25% or better, thus on-board calibration channels are included to go with underflight calibration experiments to be conducted during the SDO mission.
The primary objectives of the EVE instrument are to:
* Specify the solar EUV spectral irradiance and its variability on multiple time scales
* Advance current understanding of how and why the solar EUV spectral irradiance varies
* Improve the capability to predict the EUV spectral irradiance variability
* Understand the response of the geospace environment to variations in the solar EUV spectral irradiance and the impact on human endeavors

Clouds and Earth’s Radiant Energy System (CERES)
The CERES experiment is one of the highest priority scientific satellite instruments developed for NASA’s Earth Observing System (EOS). The first CERES instrument was launched in December of 1997 aboard NASA’s Tropical Rainfall Measurement Mission (TRMM), CERES instruments are now collecting observations on three separate satellite missions, including the EOS Terra and Aqua observatories and now also on the NPOESS Preparatory Project (NPP) observatory.
CERES products include both solar-reflected and Earth-emitted radiation from the top of the atmosphere to the Earth’s surface. Cloud properties are determined using simultaneous measurements by other EOS and NPP instruments such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Visible and Infrared Sounder (VIRS)…..

I do not think CERES is actually looking at EUV, that is for the EVE instrument (2010).

Mark Bofill
August 30, 2013 11:30 am

I’m throwing an idea out there that just occurred to me without doing the math (big mistake I know). Is the net balance of the number of living organisms on the planet increasing? I’d expect them to store energy while alive, and mostly I’d think that energy would have ultimately come from the Sun.
How many insects are there? Microbes? Other things I’m not thinking of? are populations increasing? How much energy per lifetime do they store, how much do they release as heat, how much stays organized for awhile on death? There are probably clever ways to get upper and lower bounds on this that I’m not aware of.
This said, I certainly don’t think it comes out to 5 Wm-2, but it has to be ~something~, right?

Mark Bofill
August 30, 2013 11:32 am

Ah, I see Lester had the same idea.

bkindseth
August 30, 2013 11:37 am

Willis, you discussed accuracy and precision. The one thing that has bothered me is that measuring incoming short wave radiation from basically a point source and measuring outgoing long wave diffused radiation and reflected radiation is like comparing apples and oranges. Do you feel that the difference between these relatively large numbers can be determined to a fraction of a percent?

August 30, 2013 11:40 am

Mark Bofill says:
August 30, 2013 at 11:30 am
More CO2 does lead to greater total biomass, up to some point. What the long-term effect on equilibrium CO2 more transient (at least) biomass may be is presently not known & may not be precisely or accurately calculable.
Science really doesn’t know what the depth, so to speak, of all the carbon sinks on the planet might be.

Skiphil
August 30, 2013 11:42 am

Great piece, but I’m still stuck on the Hansen quotation about re- “calibrating” CERES data with a climate model. So they have (what I’m sure are amazing) satellites providing data of around 6+ W m-2, which does not seem credible, so the figure is “adjusted” to 0.85 W m-2 based on a model….. how exactly does anyone ***know*** what the correct figure should be? This seems like arrant guesswork and ad hoc-ery.

August 30, 2013 11:43 am

It occurs to me that the diurnal thermal stresses caused by the heat expansion of land surfaces daily followed by night-time cooling and contraction – must consume significant amounts of energy. Rocks expand and crack. Likewise solar tides ebb and flow in the ocean. Perhaps not all of this energy can end up as thermal energy to radiate to space – some of it must end up in gravitational potential energy.
Maybe it is 5 watts/m2

Mark Bofill
August 30, 2013 11:46 am

milodonharlani says:
August 30, 2013 at 11:40 am
————-
No, I was talking energy, not CO2. Chemical energy specifically.

Gail Combs
August 30, 2013 11:46 am

Another point. According to the NASA articles I linked to, CERES instruments are on three satellites so I would think they are sampling not measuring the whole earth. That should introduce a whole heck of a lot more error.

Mark Bofill
August 30, 2013 11:51 am

milidonharlani,
My idea goes more like this – a leaf on a living tree is illuminated by X W/m-2. Perhaps (0.01)*X W/m-2 is consumed in photosynthesis. This energy is chemically stored, who knows how much for how long, depends on the fate of the leaf and the tree I guess. But if the number of living things is increasing, there’s an energy imbalance there that has to be satisfied.

August 30, 2013 11:51 am

Greg Goodman says:
August 30, 2013 at 10:42 am

“Since I got there via the aforementioned “Search interface on the ASDC Web Site”, I fear we’re temporarily out of luck.”

Damn. Since you have a copy, maybe you could make it available somewhere (WUWT for example).

Done. I’ve collated it from R into an Excel spreadsheet, available here as a .csv (comma separated values) file, and updated the head post.
-w

eco-geek
August 30, 2013 11:56 am

Five Watts per square meter Imbalance for five years is the equivalent of 25 Watts per square meter in a single year which seems to be about 7% of downwelling. Yes, it does seem unlikely all that additional heat energy is still hanging around. If it was we would be suffering from lots of global warming. Of couirse it has been getting colder since 2005 so an opposite imbalance should show from 2005 onwards.
It is interesting to note that the Global Average Temperature Records from what ever source show much much greater short term variation than does the imbalance and therefore we can conclude that the former are not caused by the latter. Are the long term average trends in temperature related to the trends in imbalance? They certainly should be, if not then these trends in temperature are dominated by other factors than radiation imbalances.

Lester Via
August 30, 2013 12:00 pm

As Gail points out, it is unlikely that CERES is measuring the whole earth. If this is the case, then hot spots generated by forest fires will likely be missed (or ignored). The radiant energy released by forest fires is stored chemical energy originating from photosynthetically absorbed sunlight.

HaroldW
August 30, 2013 12:00 pm

“Curiously, the variations in upwelling longwave are about 6 months out of phase with the downwelling radiation.”
Willis, why do you find this curious? Solar will increase as Earth nears the sun, peaking in January at perihelion. Longwave should (in general) increase with surface temperature, which peaks in July.

August 30, 2013 12:01 pm

rgbatduke says:
August 30, 2013 at 11:08 am

Willis, something is not right, unless I’m losing my mind (always possible). The Earth’s orbit is quite eccentric. Aphelion is 152,000,000 km, perihelion is 147,000,000 km. The relative variation of TOA insolation must therefore by \Delta I = (P_s/4\pi R_p^2 – P_s/4\pi R_a^2 ). The Luminosity of the sun P_s = 3.85 x 10^26 Watts. Hence, 1418 W/m^2 at perihelion, 1326 W/m^2 at aphelion, \Delta I = 92 W/m^2. This is a roughly 7% annual variation. This is perhaps consistent with your top curve IF one does a whole lot of processing that is not described in your article. Is this just dividing by 4, the ratio between \pi R_e^2 and 4 \pi R_e^2?

The total variation (as you point out) is 96 W/m2 at TOA. However, if you average it over every time the satellite passes over that spot, day and night, you get a quarter of that variation. That is 24 W/m2 … which is also the variation shown in Figure 1.
I assume that rather than a theoretical value, this is the actual average value of the measurements for each given spot, some of which will be zero because it’s night-time when the satellite whizzes by.
More later, you raise a number of interesting issues.
w.

Greg Goodman
August 30, 2013 12:05 pm

http://ceres.larc.nasa.gov/science_information.php?page=EBAFclrsky
Monthly and climatological averages of TOA clear-sky (spatially complete) fluxes, all-sky fluxes, and cloud radiative effect (CRE), where the TOA net flux is constrained to the ocean heat storage.
click this link >>> Data Quality Summary

August 30, 2013 12:07 pm

coaldust says:
August 30, 2013 at 11:00 am

Wow. Uh, WOW. Just WOW.
The satellite measurements suggest trapping 5 W/m^2, this is regarded as implausible. SO MODELS ARE USED TO CALIBRATE THE MEASUREMENTS!?!
Complete and utter baloney. That’s not science. That’s fudge factors. The CERES data should be thrown out. It is very precisely measuring something that is completely useless.

Egads, no, that’s throwing the baby out with the bathwater. Precision is valuable even if the accuracy is relatively low. Overall, the measurements balance to within 1.5% or so. You are right that we shouldn’t use the models to calibrate the instruments … but never throw out good data, that’s a sin.
w.

george e. smith
August 30, 2013 12:11 pm

Well the only problem that I have with this analysis, is that it is very well known, by anyone who can read, that the TSI is about 1362 W/m^2 averaged over the year, with about a 0.1% p-p variation over the 11 year solar cycle; not 350.
So clearly, none of these “data” in figure 1 were actually MEASURED by anyone, anywhere, anyhow, anytime; there is no method of doing so.
So the data is all contrived, derived, devised, revised whatever.
They aren’t going to get real results, unless they actually measure the real values.
And it’s getting really tiresome, reading all these contrived model representations.

Greg Goodman
August 30, 2013 12:16 pm

Harold: “Longwave should (in general) increase with surface temperature, which peaks in July.”
It’s not just temperature (which does not peak in July in SH ) albedo is more important since it can vary more in %age terms that absolute temperature ( on the Kelvin scale).
I think one major factor will be albedo (reflectivity) change in the Arctic. Low reflectivity also means high emissivity. As Arctic ice retreats in the NH summer there will be a large increase in emitted IR from open water and melt-pools.
This is the negative albedo feedback alarmists ignore when wailing about “tipping points”.

Toto
August 30, 2013 12:20 pm

Can this analysis be done by latitude bands? And also by land/ocean? The lateral heat transfers would complicate the conclusions, but it would still be interesting.

george h.
August 30, 2013 12:20 pm

So, I guess the ocean sink must have been full of dishes back in the 1980’s.

Greg Goodman
August 30, 2013 12:23 pm

George: TSI is about 1362 W/m^2 averaged over the year, with about a 0.1% p-p variation over the 11 year solar cycle; not 350.
Try to keep up George, 1362 is straight-on instantaneous peak, averaged out over 24h across all the surface you get to divide by 4 , see above.
However, from the graph, I would eyeball the average line at around 345 and 1362/4=340.5
That’s a difference of about 5W/m2 …

August 30, 2013 12:24 pm

Aphan says:
August 30, 2013 at 11:01 am

Willis, can I ask you a possibly stupid question?

On my planet, the only stupid questions are the ones you don’t ask …

Why is it, that in all the discussions/studies/comments I’ve read about ocean heat, there NEVER, EVER seems to be even a mention of the fact that the core of this planet is HOT….FREAKING HOT…and that any “heat” in layers of the ocean below what can be heated by the sun/surface air temps, MIGHT actually be coming from BELOW the ocean’s floor?

The reason is that the amount of heat coming to the surface from the core of the earth is relatively small, on the order of a tenth of a watt per square metre when averaged over the planetary surface. We see hot magma coming from volcanoes, and hot water coming from hot springs … but how many of those are there? You can go for thousands of miles without encountering either one, so the average, even including suboceanic venting, is small when averaged over the 5.11E+14 square metres of earth’s surface …
You are correct that it does play a part in the oceanic circulation, however. But again, it’s small. Here’re the numbers. Consider the deepest ocean, say the bottom thousand metres.
One watt per square metre will heat one cubic metre of seawater by one-third of a degree C per year … so for the thousand deepest metres of the ocean, one watt will heat it by 0.0003°C per year. But we only have a tenth of a watt from geothermal, so that will warm the bottom thousand metres by …
0.00003°C per year = 0.03°C per thousand years.
So even on the timescales of oceanic overturning, which are one or a few thousands of years, geological heat is a third-order effect. That’s why although it is real, it is usually ignored in discussions of the climate fluctuations.
w.

Londo
August 30, 2013 12:35 pm

Climate science is very much like the deep oceans. If you try get to the bottom of it, it’s likely to crush you. Beware of the inquisition Willis but thank’s for a great post.

August 30, 2013 12:37 pm

Mark Bofill says:
August 30, 2013 at 11:51 am
It’s not necessarily the number of living things that matters, but the total biomass.
A recent hypothesis posits that life develops to solve certain organic chemical energetic conundra on a rocky planet with volcanism & an ocean (if not elsewhere as well), via carbon fixation.
http://phys.org/news/2012-12-life-inevitable-paper-pieces-metabolism.html