Engelbeen on why he thinks the CO2 increase is man made (part 3)

About carbon isotopes and oxygen use…

1. The different carbon isotopes in nature.

The carbon of CO2 is composed of different isotopes. Most is of the lighter type: 12C, which has 6 protons and 6 neutrons in its nucleus. About 1.1% is the heavier 13C which has 6 protons and 7 neutrons in the nucleus. There also is a tiny amount of 14C which has 6 protons and 8 neutrons in the nucleus. 14C is continuously formed in the upper stratosphere from the collisions of nitrogen with cosmic rays particles. This type of carbon (also formed by above-ground atomic bomb experiments in the 1950’s) is radio-active and can be used to determine the age of fossils up to about 60,000 years.

One can measure the 13C/12C ratio and compare it to a standard. The standard was some type of carbonate rock, called Pee Dee Belemnite (PDB). When the standard rock was exhausted, this was replaced by a zero definition in a Vienna conference, therefore the new standard is called the VPDB (Vienna PDB). Every carbon containing part of any subject can be measured for its 13C/12C ratio. The comparison with the standard is expressed as d13C in per thousand (the term mostly used is per mil):

(13C/12C)sampled – (13C/12C)standard

————————————————————— x 1.000

(13C/12C)standard

Where the standard is defined as 0.0112372 part of 13C to 1 part of total carbon. Thus positive values have more 13C, negative values have less 13C. Now, the interesting point is that vegetation growth in general uses by preference 12C, thus if you measure d13C in vegetation, you will see that it has quite low d13C values. As fossil fuels were formed from vegetation (or methanogenic bacteria, with similar preferences), these have low d13C values too.  Most other carbon sources (oceans, carbonate rock wearing, volcanic degassing,…) have higher d13C values. For a nice introduction of the isotope cycle in nature, see the web page of Anton Uriarte Cantolla ( http://homepage.mac.com/uriarte/carbon13.html ).

This is an interesting feature, as we can determine whether changes of CO2 levels in the atmosphere (observed to be currently -8 per mil VPDB) were caused by vegetation decay or fossil fuel burning (both about -24 per mil) or by ocean degassing (0 to +4 per mil).

2. Trends in carbon isotope ratios, the 13C/12C ratio.

From different CO2 baseline stations, we not only have CO2 measurements, but also d13C measurements. Although only over a period of about 25 years, the trend is clear and indicates an extra source of low d13C in the atmosphere.

Recent trends in d13C from direct measurements of ambient air at different baseline stations.

Data from http://cdiac.ornl.gov/trends/co2/contents.htm

ALT=Alert; BAR=Barrow; LJO=La Jolla; MLO=Mauna Loa; CUM=Cape Kumukahi; CHR=Christmas Island; SAM=Samoa; KER=Kermadec Island; NZD=New Zealand (Baring Head); SPO=South Pole.

Again, we see a lag in the trends with altitude and NH/SH border transfer and less variability in the SH. Again, this points to a source in the NH. If that is from vegetation decay (more present in the NH than in the SH) and/or from fossil fuel burning (90% in the NH) is solved in the investigation of Battle ea. http://www.sciencemag.org/cgi/reprint/287/5462/2467.pdf

More up-to-date (Bender e.a.) and not behind a paywall:

http://www.bowdoin.edu/~mbattle/papers_posters_and_talks/BenderGBC2005.pdf

Where it is shown that there is less oxygen used than can be calculated from fossil fuel burning. Vegetation thus produces O2, by incorporating more CO2 than is formed by decaying vegetation (which uses oxygen). This means that more 12C is incorporated, and thus more 13C is left behind in the atmosphere. Vegetation is thus a source of 13C and is not the cause of decreasing d13C ratios.

And we have several other, older measurements of d13C in the atmosphere: ice cores and firn (not completely closed air bubbles in the snow/ice). These align smoothly with the recent air measurements. There is a similar line of measurements from coralline sponges and sediments in the upper oceans. Coralline sponges grow in shallow waters and their skeleton is built from CO2 in the upper ocean waters, without altering the 13C/12C ratio in seawater at the time of building. The combination of atmospheric/firn/ice and ocean measurements gives a nice history of d13C changes over the past 600 years:

Figure from http://www.agu.org/pubs/crossref/2002/2001GC000264.shtml gives a comparison of upper ocean water and atmospheric d13C changes.

What we can see, is that the d13C levels as well as in the atmosphere as in the upper oceans start to decrease from 1850 on, that is at the start of the industrial revolution. In the 400 years before, there is only a small variation, probably caused by the temperature drop in the Little Ice Age.

In comparison, over the whole Holocene, the variation of d13C was only 0.4 per mil:

http://www.nature.com/nature/journal/v461/n7263/full/nature08393.html

And the change in d13C from the coldest part of the last glacial to the warm Holocene Optimum was only 0.7 per mil, slightly over the recent d13C change:

http://epic.awi.de/Publications/Khl2004e.pdf

The decrease of d13C in the atmosphere cannot be caused by some extra outgassing from the oceans, as that would INcrease the d13C ratios of the atmosphere (even including the fractionation at the ocean-air border), while we see a DEcrease both in the oceans and the atmosphere. This effectively excludes the oceans as the main cause of the increase.

3. The 14C/12C ratio

14C is a carbon isotope that is produced in the atmosphere by the impact of cosmic rays. It is an unstable (radioactive) isotope and breaks down with a half-life time of less than 6,000 years. 14C is used for radiocarbon dating of not too old fossils (maximum 60,000 years). The amount of 14C in the atmosphere is variable (depends of the sun’s activity), but despite that, it allows for a reasonable good dating method. Until humans started to burn fossil fuels…

The amounts of 14C in the atmosphere and in vegetation is more or less in equilibrium (as is the case for 13C: a slight depletion, due to 12C preference of the biological reactions). But about half of it returns to the atmosphere within a year, by the decay of leaves. Other parts need more time, but a lot goes back into the atmosphere within a few decades. For the oceans, the lag between 14C going into the oceans (at the North Atlantic sink place of the great conveyor belt) is 500-1500 years, which gives a slight depletion of 14C, together with some very old carbonate going into solution which is completely 14C depleted. In pre-industrial times, there was an equilibrium between cosmogenic 14C production and oceanic depletion.

Fossil fuels at the moment of formation (either wood for coal or plankton for oil) incorporated some 14C, but as these are millions of years old, there is virtually no 14C anymore left. Just as is the case for 13C, the amount of CO2 released from fossil fuel burning dilutes the 14C content of the atmosphere. This caused problems for carbon dating from about 1890 on. Therefore a correction table is used to correct samples after 1890.

In the 1950’s another human intervention caused trouble for carbon dating: nuclear bomb testing induced a lot of radiation, which nearly doubled the atmospheric 14C content. Since then, the amount is fast decreasing, as the oceans replace it with “normal” 14C levels. The half life time of the excess 14C caused by this refresh rate is about 5 years.

This adds to the evidence that fossil fuel burning is the main cause of the increase of CO2 in the atmosphere…

T4. Trends in oxygen use.

To burn fossil fuels, you need oxygen. As for every type of fuel the ratio of oxygen use to fuel use is known, it is possible to calculate the total amount of oxygen which is used by fossil fuel burning. At the other hand, the real amount of oxygen which is used can be measured in the atmosphere. This is quite a challenging problem, as the change in atmospheric O2 from year to year is quite low, compared to the total amount of O2 (a few ppmv in over 200,000 ppmv). Moreover, as good as for CO2 as for oxygen, there is the seasonal to year-by-year influence of vegetation growth and decay. Only since the 1990’s, oxygen measurements with sufficient resolution are available. These revealed that there was less oxygen used than was calculated from fossil fuel use. This points to vegetation growth as source of extra O2, thus vegetation is a sink of CO2, at least since 1990.

This effectively excludes vegetation as the main cause of the recent increase.

The combination of O2 and d13C measurements allowed Battle e.a. to calculate how much CO2 was absorbed by vegetation and how much by the oceans (see the references above). The trends of O2 and CO2 in the period 1990-2000 can be combined in this nice diagram:

O2-CO2 trends 1990-2000, figure from the IPCC TAR

http://www.grida.no/climate/IPCC_tar/wg1/pdf/TAR-03.PDF

This doesn’t directly prove that all the CO2 increase in the atmosphere is from fossil fuel burning, but as both the oceans and vegetation are not the cause, and even show a net uptake, and other sources are much slower and/or smaller (rock weathering, volcanic outgassing,…), there is only one fast possible source: fossil fuel burning.

Engelbeen on why he thinks the CO2 increase is man made (part 3)

About carbon isotopes and oxygen use…

  1. The different carbon isotopes in nature.

The carbon of CO2 is composed of different isotopes. Most is of the lighter type: 12C, which has 6 protons and 6 neutrons in its nucleus. About 1.1% is the heavier 13C which has 6 protons and 7 neutrons in the nucleus. There also is a tiny amount of 14C which has 6 protons and 8 neutrons in the nucleus. 14C is continuously formed in the upper stratosphere from the collisions of nitrogen with cosmic rays particles. This type of carbon (also formed by above-ground atomic bomb experiments in the 1950’s) is radio-active and can be used to determine the age of fossils up to about 60,000 years.

One can measure the 13C/12C ratio and compare it to a standard. The standard was some type of carbonate rock, called Pee Dee Belemnite (PDB). When the standard rock was exhausted, this was replaced by a zero definition in a Vienna conference, therefore the new standard is called the VPDB (Vienna PDB). Every carbon containing part of any subject can be measured for its 13C/12C ratio. The comparison with the standard is expressed as d13C in per thousand (the term mostly used is per mil):

(13C/12C)sampled – (13C/12C)standard

————————————————————— x 1.000

(13C/12C)standard

Where the standard is defined as 0.0112372 part of 13C to 1 part of total carbon. Thus positive values have more 13C, negative values have less 13C. Now, the interesting point is that vegetation growth in general uses by preference 12C, thus if you measure d13C in vegetation, you will see that it has quite low d13C values. As fossil fuels were formed from vegetation (or methanogenic bacteria, with similar preferences), these have low d13C values too.  Most other carbon sources (oceans, carbonate rock wearing, volcanic degassing,…) have higher d13C values. For a nice introduction of the isotope cycle in nature, see the web page of Anton Uriarte Cantolla ( http://homepage.mac.com/uriarte/carbon13.html ).

This is an interesting feature, as we can determine whether changes of CO2 levels in the atmosphere (observed to be currently -8 per mil VPDB) were caused by vegetation decay or fossil fuel burning (both about -24 per mil) or by ocean degassing (0 to +4 per mil).

  1. Trends in carbon isotope ratios, the 13C/12C ratio.

From different CO2 baseline stations, we not only have CO2 measurements, but also d13C measurements. Although only over a period of about 25 years, the trend is clear and indicates an extra source of low d13C in the atmosphere.

Recent trends in d13C from direct measurements of ambient air at different baseline stations.

Data from http://cdiac.ornl.gov/trends/co2/contents.htm

ALT=Alert; BAR=Barrow; LJO=La Jolla; MLO=Mauna Loa; CUM=Cape Kumukahi; CHR=Christmas Island; SAM=Samoa; KER=Kermadec Island; NZD=New Zealand (Baring Head); SPO=South Pole.

Again, we see a lag in the trends with altitude and NH/SH border transfer and less variability in the SH. Again, this points to a source in the NH. If that is from vegetation decay (more present in the NH than in the SH) and/or from fossil fuel burning (90% in the NH) is solved in the investigation of Battle ea. http://www.sciencemag.org/cgi/reprint/287/5462/2467.pdf

More up-to-date (Bender e.a.) and not behind a paywall:

http://www.bowdoin.edu/~mbattle/papers_posters_and_talks/BenderGBC2005.pdf

Where it is shown that there is less oxygen used than can be calculated from fossil fuel burning. Vegetation thus produces O2, by incorporating more CO2 than is formed by decaying vegetation (which uses oxygen). This means that more 12C is incorporated, and thus more 13C is left behind in the atmosphere. Vegetation is thus a source of 13C and is not the cause of decreasing d13C ratios.

And we have several other, older measurements of d13C in the atmosphere: ice cores and firn (not completely closed air bubbles in the snow/ice). These align smoothly with the recent air measurements. There is a similar line of measurements from coralline sponges and sediments in the upper oceans. Coralline sponges grow in shallow waters and their skeleton is built from CO2 in the upper ocean waters, without altering the 13C/12C ratio in seawater at the time of building. The combination of atmospheric/firn/ice and ocean measurements gives a nice history of d13C changes over the past 600 years:

Figure from http://www.agu.org/pubs/crossref/2002/2001GC000264.shtml gives a comparison of upper ocean water and atmospheric d13C changes.

What we can see, is that the d13C levels as well as in the atmosphere as in the upper oceans start to decrease from 1850 on, that is at the start of the industrial revolution. In the 400 years before, there is only a small variation, probably caused by the temperature drop in the Little Ice Age.

In comparison, over the whole Holocene, the variation of d13C was only 0.4 per mil:

http://www.nature.com/nature/journal/v461/n7263/full/nature08393.html

And the change in d13C from the coldest part of the last glacial to the warm Holocene Optimum was only 0.7 per mil, slightly over the recent d13C change:

http://epic.awi.de/Publications/Khl2004e.pdf

The decrease of d13C in the atmosphere cannot be caused by some extra outgassing from the oceans, as that would INcrease the d13C ratios of the atmosphere (even including the fractionation at the ocean-air border), while we see a DEcrease both in the oceans and the atmosphere. This effectively excludes the oceans as the main cause of the increase.

  1. The 14C/12C ratio

14C is a carbon isotope that is produced in the atmosphere by the impact of cosmic rays. It is an unstable (radioactive) isotope and breaks down with a half-life time of less than 6,000 years. 14C is used for radiocarbon dating of not too old fossils (maximum 60,000 years). The amount of 14C in the atmosphere is variable (depends of the sun’s activity), but despite that, it allows for a reasonable good dating method. Until humans started to burn fossil fuels…

The amounts of 14C in the atmosphere and in vegetation is more or less in equilibrium (as is the case for 13C: a slight depletion, due to 12C preference of the biological reactions). But about half of it returns to the atmosphere within a year, by the decay of leaves. Other parts need more time, but a lot goes back into the atmosphere within a few decades. For the oceans, the lag between 14C going into the oceans (at the North Atlantic sink place of the great conveyor belt) is 500-1500 years, which gives a slight depletion of 14C, together with some very old carbonate going into solution which is completely 14C depleted. In pre-industrial times, there was an equilibrium between cosmogenic 14C production and oceanic depletion.

Fossil fuels at the moment of formation (either wood for coal or plankton for oil) incorporated some 14C, but as these are millions of years old, there is virtually no 14C anymore left. Just as is the case for 13C, the amount of CO2 released from fossil fuel burning dilutes the 14C content of the atmosphere. This caused problems for carbon dating from about 1890 on. Therefore a correction table is used to correct samples after 1890.

In the 1950’s another human intervention caused trouble for carbon dating: nuclear bomb testing induced a lot of radiation, which nearly doubled the atmospheric 14C content. Since then, the amount is fast decreasing, as the oceans replace it with “normal” 14C levels. The half life time of the excess 14C caused by this refresh rate is about 5 years.

This adds to the evidence that fossil fuel burning is the main cause of the increase of CO2 in the atmosphere…

4

  1. Trends in oxygen use.

To burn fossil fuels, you need oxygen. As for every type of fuel the ratio of oxygen use to fuel use is known, it is possible to calculate the total amount of oxygen which is used by fossil fuel burning. At the other hand, the real amount of oxygen which is used can be measured in the atmosphere. This is quite a challenging problem, as the change in atmospheric O2 from year to year is quite low, compared to the total amount of O2 (a few ppmv in over 200,000 ppmv). Moreover, as good as for CO2 as for oxygen, there is the seasonal to year-by-year influence of vegetation growth and decay. Only since the 1990’s, oxygen measurements with sufficient resolution are available. These revealed that there was less oxygen used than was calculated from fossil fuel use. This points to vegetation growth as source of extra O2, thus vegetation is a sink of CO2, at least since 1990.

This effectively excludes vegetation as the main cause of the recent increase.

The combination of O2 and d13C measurements allowed Battle e.a. to calculate how much CO2 was absorbed by vegetation and how much by the oceans (see the references above). The trends of O2 and CO2 in the period 1990-2000 can be combined in this nice diagram:

O2-CO2 trends 1990-2000, figure from the IPCC TAR

http://www.grida.no/climate/IPCC_tar/wg1/pdf/TAR-03.PDF

This doesn’t directly prove that all the CO2 increase in the atmosphere is from fossil fuel burning, but as both the oceans and vegetation are not the cause, and even show a net uptake, and other sources are much slower and/or smaller (rock weathering, volcanic outgassing,…), there is only one fast possible source: fossil fuel burning.

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Roger Longstaff
September 16, 2010 7:48 am

Coal is a fossil fuel – but oil and gas?
Most of the mass of the planets in the solar system is comprised of hydrocarbons.
The possible implication is that reserves of oil and gas on Earth are virtually inexhaustible. I read somewhere that the Russians formed this theory decades ago (under instructions from Stalin?) and this has been responsible for an outstanding policy of energy exploitation. There is a lot of information and comment on the internet.
Comments, anybody?

Vince Causey
September 16, 2010 7:48 am

D. Patterson,
“Among the many flaws in the essay, the assumption that anthropogenic sources are the only possible explanation for increased d13Carb increases is among the fatal flaws to the argument.”
I think the article is saying that d13 is decreasing not increasing.

tallbloke
September 16, 2010 7:49 am

Hi Ferdinand, thanks for a clearly written article which appears to use good logic as far as it goes. I have a couple of questions.
1) You told us in an earlier installment that the ‘natural’ increase in co2 due to the earth being a degree warmer than it used to be would be around (IIRC) 20ppm (from oceanic de-gassing). But co2 has risen @110ppm from @280 to @390. If we are responsible for around half of that increase, 55ppm, and the expected natural increase due to oceanic de-gassing is 20ppm, what is responsible for the other @35ppm?
2) If the answer to 1) is “we don’t know”, then how do we know that the mystery factor wouldn’t cause more than 35ppm extra if we weren’t pumping fossil fuel produced co2 into the atmosphere? i.e. if there is a non-linear process at work, how do we know it wouldn’t ‘take up the slack’ if we emitted less?
Thanks and regards.

Kent Gatewood
September 16, 2010 7:55 am

The graph starts down in 1810 not 1850.

richard telford
September 16, 2010 7:56 am

erik sloneker says:
September 16, 2010 at 6:52 am
Anyone who has participated in a controlled burn of a patch of prairie grass understands that pre-industrial humans facilitated enormous CO2 emissions. Here in the central USA where prairie savannah dominated the landscape, entire states where thought to have been routinely burned off (every 1 to 3 years) by Native Americans.
—————————–
And 1-3 years later the grassland has regrown, reaccumulating carbon as organic matter. Therefore there is no long-term net production of CO2 from this system. In contrast not many coal horizons replenish in 1-3 years.

Marko
September 16, 2010 8:00 am

Roger. If methane is a “fossil fuel” and Saturn’s moon Titan is a big ball of methane it must mean one of two things.
Since the scientific concensus claims hydrocarbons are based on organic matter, and who can argue against scientific concensus, Titan was obviously a life bearing moon.

David Jones
September 16, 2010 8:01 am

nevket240 says:
September 16, 2010 at 4:38 am
((What we can see, is that the d13C levels as well as in the atmosphere as in the upper oceans start to decrease from 1850 on, that is at the start of the industrial revolution. ))
1850- the start of the industrial revolution, eh??
Rubbish. Then again the worlds only 10,000 years old, isn’t it??
You had tens of millions of people burning peat, charcoal, coal etc but there was NO CO2 influence until some dastardly bastard started a boiler and burnt wood.
Start again FE this one is a shocker.
regards
The thought that occurred to me was that 1850 is also close to the end of the LIA, when temperatures commenced warming anyway.

PeterB in Indianapolis
September 16, 2010 8:02 am

“I am left wondering who it is that says human beings are not adding CO2 to the atmosphere. That is true while at the same time adding more water vapor.
CH4 + 2O2 => 2H2O + CO2
More molecules of water are added to atmosphere by at least 2:1 and reducing O2. The real story then is that we will not be able to breath at some point in the distant future because we have burned up all the oxygen.”
Your equation was great, and then your conclusion became incredibly silly. At higher CO2 concentrations, all photosynthetic organisms photosynthesize at a higher rate, converting more CO2 BACK to O2. You have to include this equation as well.
Your conclusion assumes that there are no other chemical reactions going on than the one you listed, and that O2 is the “limiting reagent” for the equation you listed. Let me assure you that there are BIG reactions going on all of the time which counterbalance the reaction that you showed, and as such, it is HIGHLY unlikely that O2 is the limiting reagent.
Something truly bizzare would have to happen for the world to run out of Oxygen any time in the next few billion years.

k winterkorn
September 16, 2010 8:03 am

I think the article above is persuasive that much of the CO2 increase is from biologic sources, not mineral sources or outgassing from a warming ocean. However, the quick jump to man is at “fault” (as someone above used the word), is a little too quick. Man’s contribution is small compared with other biologic sources (decay of plants, peat, soil, maybe even oil seeps, etc.) The non-human biologic sources may accelerate when the Earth is warmed for other reasons. I have not see that this is excluded or quantified.
Is the total biomass of bacteria, fungi, insects, etc., not likely to increase as the climate warms?

Enneagram
September 16, 2010 8:09 am

When CO2 charged blood (venous blood) retention in the brain , brain begins to manufacture the most fantastic theories about CO2. Be very careful GWRS. as this condition leads to Auto-immune Illnesses.

douglas
September 16, 2010 8:27 am

Why is there no thought given to the possibility that human addition of C02 to atmosphere just slows the outgassing from the oceans. The system is seeking equilibrium, human are just beating the ocean to the punch. The increase in atmospheric concentration would happen anyway.

September 16, 2010 8:27 am

Thanks Nylo,
I have added links to co2 http://antonuriarte.blogspot.com/ the Blog of Antón Uriarte, San Sebastián, Gipuzkoa, España.
It is good to see not all is lost in Spain!

Roger Longstaff
September 16, 2010 8:29 am

Marco – you are quite correct, how could I doubt the “scientific consensus”?
I really should get back to the day job (space science) and search for the trillions of farting cows on Titan.

Dave Springer
September 16, 2010 8:32 am

This analysis is deeply flawed – there is not one mention of methane. One commenter touched upon it indirectly by mentioning that the analysis fails to consider bacteria. Methane is produced by bacteria, bacteria have twice the preference for carbon 12 as do plants (see the diagram in the OP showing methane at -50 compared to organic sources at -24, and methane released in the atmosphere degrades in less than a decade into CO2 and water vapor. As well, “fossil” methane exists in huge quantities as methane hydrate in both permafrost and in sea floor sediments both of which release the gas when warming occurs.
Methane concentration in the atmosphere more than doubled (715ppb in 1890 to 1732ppb in 1990) since the beginning of the industrial revolution. Interestingly the growth in atmospheric concentration has slowed significantly in the past decade.
Good article: “The Other Greenhouse Gas”
http://www.scienceline.org/2007/03/env_knight_ipcccows/
At any rate there’s an elephant in the room named “Methane” that can handily explain the decline in atmospheric C13. Why is there mention of it in the OP?
Engelbeen on manmade CO2: FAIL

redneck
September 16, 2010 8:38 am

This post raises an interesting question. If human use of fossil fuels results in decreasing the d13C ratio and thus increasing both the amount and percentage of 12C available in the atmosphere what affect does this have on plants which prefer 12C? It would seem to me it could only result in faster plant growth. Anybody out there know how low d13C ratios affect plants?

Merrick
September 16, 2010 8:47 am

I don’t disagree with the conclusions of the author, but he seems to be ignoring basic differential equations. Pick a point in the past – let’s say 200 years ago. Before that point almost no fossil fuels were burned (coal had been used for some time before that, but no extensive industrialization had yet taken place). So all of the sources were effectively neutral: oceans were d13+ and plants were d13-. But on the whole the ocean absorbed as much as it emitted and the plants absorbed as much as they emitted. Now add a strong d13- component to the mix: fossil fuel burning. And fossil fuel burning has no effective negative component: no strong d13- absorber to natch it. So, the ocean absorbs CO2, for instance, but it’s absorbing CO2 that has been enriched by fossil fuel emissions. Since the ocean has NO strong bias, the FRACTION of CO2 in the atmosphere that originated with fossil fuel burning (as opposed to all other sources) HAS to go up and the d13- effect HAS to be observed. But that statement does not lead one to the conclusion that all or some of the CO2 concentration delta is because of fossil fuel burning. Only that because of the isotopic differene we can tell that fossil fuels have been emitted into the atmosphere. This argument on it’s own only supports that observation.
Even is CO2 concentrations were DECREASING the isotope ratio would be impacted by fossil fuels – and more strongly to boot. So, no, I’d argue this measurement alone doesn’t get one all the way to blaming fossil fuels for the increase in CO2 concentration.
Any time that there is a net atmosphereic shift to/from vegitation and to/from ocean there is going to be a shift in isotope ratios in the atmospheres. That’s also completely true and completely independent of whether or not you even start thinking about fossil fuels. Since we know that gas solubility in water varies with temperature and that plant growth rates vary with temperature, precipitation, and land usage, isn’t a single measurement of an isotope shift in the atmosphere a little bit light data to jump straight to fossil fuels?
I know that it’s a tough problem (from the standpoint of available data), but until we have good science that identifies of all the CO2 sinks and all of the CO2 sources as well as a good estimate of all their rates this is going to remain an open question.
But thanks to the author for contributing to the discussion.

September 16, 2010 8:49 am

RW says:
“We know that fossil fuels release CO2; we know that humans have burned more than enough to account for the observed rise. Therefore, humans have cause the rise.”
You need a course in logic, son. “Therefore…” may or may not be true, but it does not logically follow in your statement.
Instead of playing a logic-challenged game, explain your belief of why a rise in a harmless trace gas is a problem that will plead to climate catastrophe, rather than being the beneficial effect of the rise in T since the LIA.
If possible, try to keep the arm-waving to a minimum. And try to use Occam’s Razor as it was intended: there is no good reason [other than feeding at the public trough] to add an extraneous variable like CO2 to the long-accepted theory of natural climate variability — which has never been falsified despite the $billions in public funds being fruitlessly wasted trying to disprove it.

George E. Smith
September 16, 2010 8:53 am

“””” This adds to the evidence that fossil fuel burning is the main cause of the increase of CO2 in the atmosphere… “”””
Well Englebeen; thanks very much for a very well detailed presentation of the whole Carbon Isotope question. It is certainly the most readable and informative presentation of that subject I have ever seen; so I am going to print it out and add itto my collection of Climate related papers.
However with regard to the heading I pasted from your paper. It’s nt the first time I have seen that stated. Everybody pushing the man-made GW story says that; so I guess it must be true.
Well no it doesn’t. What you have presented does not make that case. What it does establish, is that it is quite apparent that somewhere along the line of the recent history of Atmospheric CO2 and its changes, a NEW SOURCE of carbon started to be incorporated into the total carbon cycle (short term) as a result of human burning of fossil fuels. It DOES NOT prove that that particular source of new carbon is responsible for the increased amount of CO2 in the atmosphere.
Now let me make myself clear on this point. I am NOT arguing that CO2 is NO going up in the atmosphere; I am not arguing that human activities are NOT the cause of (at least some of) that increased CO2 in the atmosphere. I’m simply saying that our burning of fossil fuels is certainly releasing to the atmosphere a new source of carbon that exhibits a difefrent signature; but the isotope argument doesn’t prove that all of the increase consists of fossil fuel carbon.
We could illustrate the point by saying; suppose that we discovered in America a humungous expanse of new petroleum; that just came gushing out of every well we put down there and gave us a dirt cheap local source of super high quality petroleum that we exploited to the maximum. But this source of petroleum is weird; it contains a sizeable percentage of Argon; for unknown reasons; and so much Argon that we don’t know what to do with it; so we just let it vent off as we let the oil gush out.
We can expect that if we had been collecting data on Argon in the atmosphere all these years; that we would start to see an upturn in the amount of Argon in the atmosphere as we extracted more of this weird oil and vented the Argon.
Somebody who observed this data and knew of this particular deposit; could reasonably conjecture that we must be tapping that pool of weird oil.
Same thing with the CO2 isotope story. Yes it demonstrates that carbon from fossil fuel sources is entering the environment as a result of our use of fossil fuel deposits. It does not prove that that is the cause of the increase in atmopsheric CO2 (although that very well might be true).
Many years ago, I was involved in the deposition of epitaxial Gallium Arsenide Phosphide, onto Gallium Arsenide wafers to make LEDs. We made our own Epitaxial Reactors, and I personally designed and built a part of the reactor that handled and controlled the gas mixtures.
We would start the process, by injecting into the reactor (after a purging cycle) a stream of Hydrogen that contained a low percentage of Arsine (AsH3). This gas would percolate through a fine long capillary that was wound up inside a three litre bottle that filled with the gas, and then exited out the other end of the bottle to the reactor to grow a layer of pure GaAs on the wafers. After establishing a steady growth and growing a base layer of GaAs, the gas flow of the Arsine mixture was dropped about about 40% ans simultaneously a new source of Hydrogen replaced the missing gas; and the new source contained Phosphine (PH3) , so the total hydrogen flow rate into the capillary remained unchanged; but now the composition changed from only an Arsine additive to a 60/40 mix of AsH3/PH3; and the change was instantaneous. This mixture was injected into the capillary and thence into the three litre bottle which was already full of Hydrogen plus a 100% content of Arsine. So the reactor continued to grow a 100% gallium Arsenide epi layer; but as the new mixture was added into the three litres of hydrogen mixture, the percentage of Arsine slowly dropped, while the percentage of Phosphine slowly increased; all automatically controlled by simple gas mixing laws; with no process controlelrs needed. The changing gas mixture now started to deposit a changing composition epi layer slowly grading from 100% gaAs to a GaAs0.6P0.4 mixed crystal that made the then highest efficiency Red LEDs. The smooth grading process followed the normal exponential time constant curve dictated by the volume of the bottle and the lenght and diameter of the capillary , along with the total flow rate.
Actually, it was a bit more complicated than that, since we put three such capillary/bottles in series to give a synchronous three pole low pass filter, that changed the grading profile to a near Gaussian transition.
The final gas composition mixture entering the reactor to grow the material could have been monitored; and simply revealed how the composition slowly changed merely as a result of an instantaneous step change in starting conditions launched by doign the Arsine Phosphine switch.
Same thin is happening with the earth atmosphere; the fossil fuel content of the atmospheric carbon continues to increase; because we have continuously been using a new source of energy that contains that carbon and releasing its end product (CO2 ) to the atmosphere. The fact that the total CO2 is going up, is a quite separate issue fromt eh fact that we burn fossil fuels.
And I repeat; Iam NOT claiming that humans are not the source of the increase in CO2; I don’t know what is; It is interesting that it is just 800 years since the mediaeval warm period when the earth Temperatures were hotter than now; and 800 years seems to be the propagation delay enshrined in the paleo records of Temperature rise followed by CO2 rise 800 years later .(and fall too).
And again; thanks for the very detailed exposition; which I must digest in more detail.

Enneagram
September 16, 2010 9:03 am

Andres Valencia says:
September 16, 2010 at 8:27 am
Thanks for the link. It surprised me that the USA has the greatest number of installed WINDMILLS: 33,000 . A lot of windmills to tear down by Don Anthony Quixote of Watts!!

September 16, 2010 9:04 am

HelmutU says:
September 16, 2010 at 6:58 am :
That the IPCC minimum contribution of anthopogenic CO2 is 21%, and that the signature should, by this calculation, be -11%, but is actually -8%, up from -7% (my computer doesn’t appear to have a mill sign). It is this conclusion I was looking for with all the graphs and discussion of mechanisms. I didn’t see it.
The recyling of fossil fuel CO2 is certainly a concern. The half-life of CO2 is a big deal. The removal process is proportional in some fashion to the total concentration, so we will continue to see a signature after introduction into the atmosphere. Another factor with a large uncertainty.
The fine points of the math are beyond not just me, but many others. Could we see someone working out:
a) the current, cumulative contribution of CO2 from fossil fuels post 1850 and 1945 (the start of so much was being dumped in the air) based on the isotopic data,
b) the incremental increase year-to year as a proportion of 2 ppm, from this isotopic data, and
c) the proportion of CO2 from fossil fuels incrementally added AFTER taking into consideration the half-life of CO2 and the changed proportion of fossil fuel CO2 in the previous year’s atmosphere?
I hate to ask questions in this forum for lack of response. Complaints or accolades dominate the bogosphere as dialogue does not go well. But to advance, critical review must be matched with critical response.

Mike Edwards
September 16, 2010 9:08 am

Mr Engelbeen – an excellent article, well put together.
However, what it does not actually do is show unequivocally that the extra percentage of CO2 we observe in the atmosphere today, compared with historical times, is there purely because of human burning of fossil fuels.
There is no doubt that human burning of fossil fuels has dumped a vast quantity of CO2 into the atmosphere and into the oceans. And the changes in isotope ratios found in the atmosphere and the oceans bear testimony to that.
However, consider an alternative hypothesis: that the amount of CO2 in the atmosphere is actually controlled by the exchange of CO2 between the oceans and the atmosphere, with the oceans acting as a vast reservoir of CO2. Envisage that in this hypothesis, the percentage of CO2 in the atmosphere is controlled by factors affecting the oceans, for example the temperature of the oceans – so that merely adding CO2 to the atmosphere by burning simply results in absorption by the oceans.
In this hypothesis, the recent rise in CO2 in the atmosphere is dictated by the oceans – for example, as the oceans warm there is outgassing of CO2 which causes the amount of CO2 in the atmosphere to rise.
With constant interchange of CO2 between the oceans and the atmosphere, the isotope concentration values described would be consistent with this hypothesis, just as well as with the hypothesis that the CO2 concentration has rise purely because of human emissions of CO2.

September 16, 2010 9:10 am

Well done and clearly laid out.

Dave Springer
September 16, 2010 9:12 am

I see one commenter mentioned CH4 (methane) before I did by showing its degradation equation: CH4 + (2)O2 -> (2)H2O + CO2.
One might begin objecting to CH4 as the C13 dilutant by saying that CH4 concentration in the atmosphere is hundreds of times less than CO2. While that’s true one must take into account that CO2 doesn’t degrade in ten years like methane does. Therefore all the methane released into the atmosphere since the beginning of the industrial revolution has long since degraded into water vapor and CO2. The remaining ~1800 parts per billion in the atmosphere today is what was emitted in only the last 10 years! Once you factor that into the equation along with CH4’s being twice the C13 dilutant as manmade (fossil) CO2 one finds that methane is a very significant source of low-C13 CO2. It also consumes oxygen when it degrades and so works to ever so slightly lower atmospheric O2.
I’m not sure if the vastly increased emission of methane which precisely mimics the burning of fossil fuel is an equal contributor to the so-called manmade CO2 signature in the atmosphere but it is certainly significant enough that any analysis like the OP which ignores it is fundamentally flawed.

George E. Smith
September 16, 2010 9:22 am

The NASA map certainly puts the Kibosh on the notion that CO2 in the atmospehre is well mixed; and that appears to be a starting assumption in climate models. It clearly isn’t even approximately well mixed. To me; well mixed would eman that no matter where or when I took a sample of the atmosphere and analysed it, I would get the same composition on a molecular species (and isotopic) basis; at least within limits of differences that are of no consequence to any climate argument; and of course excluding taking a sample up somebody’s tailpipe or chimney.
One thing does puzzle me. The oceans and the atmosphere are presumably somewhat near equilibrium in the Henry’s Law sense as to the segregation of CO2 between atmosphere and ocean. And we are told that the carbon in deep water storage, is not getting out into the atmosphere. So why is it that the CO2 isotopic composition of the near surface ocean water, and the near surface atmosphere don’t match. Is somebody claiming (proof please) that the Henry’s Law Segregation at the interface is highly isotope dependent. I haven’t heard that claim made before. Why isn’t the ocean exchanging exactly the same isotopic CO2 with the atmospehre whether releasing or taking up ?

intrepid_wanders
September 16, 2010 9:26 am

While I do understand the hypothesis that is being presented, there still remains the issue of “understanding” of isotopes specifically, carbon.
C-12 -> Stable
C-13 -> Stable
C-14 -> beta decay + N14
N-14 + n -> C-14 + H-1
B-13 -> C-13 + beta decay
So, the first thing that comes to mind is the source of C-13 is B-13 with an electron ejection (decay is tens of millisecs).
Next question is how did Boron get into the atmosphere? Oceanic Boric Acid?
http://www.google.com/url?sa=t&source=web&cd=1&sqi=2&ved=0CBIQFjAA&url=http%3A%2F%2Fwww3.interscience.wiley.com%2Fjournal%2F123311171%2Farticletext%3FDOI%3D10.1111%252Fj.2153-3490.1959.tb00039.x&ei=QTaSTJz4G43QsAPqveDkCQ&usg=AFQjCNG_Ew6QdUBveKDaZRERT8k6SbsSfQ
Perhaps…
Another question is how much of the past carbon is converted to C-14? How much B-13?
http://cdiac.esd.ornl.gov/trends/co2/well-gr.html
Of COURSE man made (nuke testing), but not fossil fuel related. Unfortunately, lots of variables.
Based on available data and information, I could not even measure the “natural effect” vs “fossil fuel effect”. 100% Uncertain Unknowns.
A good presentation of the measurement hypothesis can be found here:
http://www.google.com/url?sa=t&source=web&cd=20&ved=0CEYQFjAJOAo&url=http%3A%2F%2Fwww.geo.cornell.edu%2Feas%2Feducation%2Fcourse%2Fdescr%2FEAS302%2F06Lectures%2F302_06Lecture33.pdf&ei=4UKSTP2MG5S6sQPKzbXBCg&usg=AFQjCNFkClELnSw4fTSpsPwkZHu7O1yctg
The error bars are helpful in my conclusion that isotope ratios are cool, but work in progress.