The heat content of the oceans is 1000 times greater than the heat content of the atmosphere, both of which “take up” heat. In El Nino years heat certainly appears to be given up by the Pacific. In La Nina years, what? - heat is absorbed?
Hello Ender,
That’s close enough, I think. For a quick look at these processes, readers may wish to watch a short video and read the descriptions in:
What are El Niño and La Niña?
OK, these are natural cycles. What is the impact of CO2 on these processes? I think that question has generated some weak answers.
Good question.
Fast answer: None that we’re sure of.
Better answers always involve forcings.
Though the El Niño and La Niña phases have, respectively, positive and negative forcings associated with them, averaged over time the full cycle represents no forcing at all. Conceivably, CO2 forcing may contribute to the magnitude of the forcings associated with the ENSO cycle.
Our climate’s
energy budget, the overall balance between energy flowing into and out of our climate system, includes the full spectrum of climate processes and mechanisms. To quantify and examine the energy budget, these processes and mechanisms are expressed as “forcings.” If we know all the forcings, we know by how much and how quickly climate change is occurring.
This is what we mean by forcing, with attention to its measure:
“Forcing” is the amount of energy delivered across a unit area (or more precisely the amount of power, energy delivered per second). Climate forcings are measured in watts per square meter (given as W•M^-2 in charts and the literature).
When
The Physical Science Basis 2013 was released, total anthropogenic forcing was estimated at 2.29 watts per square meter, of which 1.68 watts per square meter was attributed to increases in CO2. The difference is primarily due to CH4 emissions, with a forcing of .97 watts per square meter, offset by negative forcings from short-lived gases and aerosols.
While these are best available estimates, readers should not assume they are accurate to the given number of decimal places. These are statistical averages, with statistical confidence intervals. CO2 forcing, for instance, is reported with very high confidence to lie between 1.33 and 2.03 watts per square meter.
Forcings from ENSO are high enough to swamp the more stable anthropogenic signal, causing temporary spikes and troughs in GMST. El Niño and La Niña occur every three to five years. Averaging over longer periods can remove the ENSO signal. PDO cycles are much longer. Only two full PDO cycles were recorded in the last century.
This is the point I was making. There is simply insufficient data to support the assertion that the missing heat is in the oceans. That “it is presumed to be” may be legitimate, but “it is” is not, and ocean temperature charts going back to the early 60’s cannot be taken too seriously due to obvious “sampling limitations.” I’m not insisting the heat was not taken up in the oceans, all I’m saying is that we cannot claim to know that it was.
To be clear, there aren’t a lot of other places where the excess heat could have gone. Ideally, we’d have a firm subsurface temperature record to work with, but we don’t. Without it we can’t specify how much heat has been taken up below the surface, but we can still point out the most likely suspect, if you will.
This phrasing is fine and indicates the true state of knowledge of the matter, but here’s the question: if CO2 increases the heat in the climate system by causing the atmospheric temp to increase, how do the oceans get heated while the atmosphere does not? Atmospheric temperatures did not increase so all the excess heat went elsewhere, yet if CO2 is the culprit the excess heat must have originally been atmospheric. What’s the explanation for that?
CO2 increases the heat in the climate system by reflecting energy back toward the surface. The heat being reflected by atmospheric CO2 doesn’t originate in the atmosphere, however. Most of the heat being reflected originates on the surface, due both to its warmer temperatures and higher heat capacity. Most of that surface is ocean.
If warmed waters are piled up by tradewinds, or cycled deeper by ocean currents, cooler waters take their place, resulting in an increase in the amount of heat being taken up by the surface, because heat flow increases with lower temperatures. At the same time, those cooler waters create lower atmospheric temperatures due to the standard triad of conduction, convection, and radiation.
As ever, Jesse