The world’s marine ecosystems risk being severely damaged by ocean acidification unless there are dramatic cuts in CO2 emissions, warn scientists.
The researchers warn that ocean acidification, which they refer to as “the other CO2 problem”, could make most regions of the ocean inhospitable to coral reefs by 2050, if atmospheric CO2 levels continue to increase.
This does indeed sound alarming, until you consider that corals became common in the oceans during the Ordovician Era – nearly 500 million years ago – when atmospheric CO2 levels were about 10X greater than they are today. (One might also note in the graph below that there was an ice age during the late Ordovician and early Silurian with CO2 levels 10X higher than current levels, and the correlation between CO2 and temperature is essentially nil throughout the Phanerozoic.)

Perhaps corals are not so tough as they used to be? In 1954, the US detonated the world’s largest nuclear weapon at Bikini Island in the South Pacific. The bomb was equivalent to 30 billion pounds of TNT, vapourised three islands, and raised water temperatures to 55,000 degrees. Yet half a century of rising CO2 later, the corals at Bikini are thriving. Another drop in pH of 0.075 will likely have less impact on the corals than a thermonuclear blast. The corals might even survive a rise in ocean temperatures of half a degree, since they flourished at times when the earth’s temperature was 10C higher than the present.
Discover more from Watts Up With That?
Subscribe to get the latest posts sent to your email.
Steven Goddard (06:30:43) :
Phil,
Several things are wrong with your last post. The link you posted, which has already been discussed at length – http://hahana.soest.hawaii.edu/hot/trends/trends.html – is a mixture of measured and calculated data. They provide no explanation of how they calculated data during years when there was no measurement.
As has been explained to you above the data labelled ‘calculated’ is obtained from measurements, there is no justification for not using it.
If you look just at their actual measured data in red (which is all that I am willing to work with,) there is no statistically significant trend. You can download all of their measured data for both of their measurement locations as I have explained and have provided spreadsheets of here.
See above
Secondly, your calculation of what a 150% increase in H+ would comprise of is incorrect. A 150% increase is a ratio of 2.5/1 and log10(2.5) = 0.4 – not 0.15 as you stated.
Agreed, your use of % misled me into thinking you meant a ratio, in any case a 0.15 decrease in pH is within the range of the IPCC SRES scenarios, the largest decrease is 0.35 so I’m not sure where the ‘150% prediction’ comes from? The A1FI scenario which gives the decrease of 0.35 is the ‘Fossil Fuel Intensive’ one with rapid economic growth.
Perhaps a more honest representation of the IPCC result would be to say that the range of values of pH in 2100 is from 7.75-7.95 down from the 2000 value of just under 8.1? Rather than take the worst case scenario, convert it to a % change (confusing to the average reader in any case since they might think that it referred to a change in pH), and then round up to the nearest 50%.
Richard S Courtney (07:08:15)
You continue to make assertions that are not only unsupported by evidence, but are demonstrably untrue. Let’s look at your comments on CO2 levels, and particularly carbon isotopes, in the light of the data that is accessible to policymakers and their scientific advisors:
The 13C data can be obtained by direct measurement (Mauna Loa since 1959; numerous other measuring stations) and from high resolution ice cores (especially the Law Dome cores). Some of the data and the methodologies are described here, for example:
Francey RJ, Allison CE, Etheridge DM, et al. (1999)
A 1000-year high precision record of delta C-13 in atmospheric CO2 TELLUS B-Chem Phys. Meteor 51, 170-193.
Meure CM et al. (2006) Law Dome CO2, CH4 and N2O ice core records extended to 2000 years BP Geophys. Res. Lett. 33, art # L14810
D. M. Etheridge et al (1996) “Natural and anthropogenic changes in atmospheric CO2 over the last 1000 years from air in Antarctic ice and firn. J. Geophys Res. 101, 4115 -4128
Here are some of your assertions:
That doesn’t work. The 12C:13C ratio isn’t just “in the direction expected” due to “a 50:50 chance that it will change in that direction or the other”. Inspection of the data demonstrates that the change in 12C:13C ratio has been in the “expected direction” continuously throughout the last 300 years or more. When our emissions were very low, the change in 12C:13C was very low (but in the “expected direction”). When our emissions were middling, so was the change in 12C:13C (still in the “expected direction”!), when our emissions were large, the change in the 12C:13C ratio was/is large (still in the “right direction”).
So for example we can inspect the record (see data in Francey cited above, for example) and find that the annual changes in delta 13C are negative (as carbon is returned to the atmosphere from burning fossil fuels the 13C content of atmospheric CO2 <reduces since fossil fuels are 13C-depleted). Here’s some of the data grouped into periods. The change in 13C:12C (- delta, delta 13C per year) was not much above zero in the period 1700-1800, started to rise through the 19th century, was rather substantial during the first half of the 20th century, and rose very quickly in the 2nd half of the 20th century as our emissions similarly rocketed upwards during this period. Now the -delta,delta-13C values are changing by around 25e-2 per year.
year range…………..(-)delta-delta-13c
1700-1800………….<0.3e-3 per year
1800-1850………….1.5-2.1e-3 per year
1850-1900………….3.3e-3 per year
1900-1950………….6.2e-3 per year
1950-2000………….~18e-2 per year
That’s not true. If anything the rate of change in 13C:12C is a bit faster than expected in recent decades since the rate of increase of atmospheric CO2 is faster than the 13C-replenished atmospheric CO2 is able to equilibrate with CO2 in the surface layers of the oceans. See Figure 11 of Francey et al cited above.
Since the premises are false [your point (5) doesn’t contain a fact], your conclusions from here on are erroneous…
Foinavon:
I have said nothing here that is not true and everything I have said here is capable of checking by anybody with little effort. Your repeated claims to the contrary do not alter that.
And I am frustrated by your knit-picking and changing of the subject so whatever comments you now make to me – however silly and/or offensive they may be – wil go unanswered by me.
Steven Goddard:
I wish to ensure that you and all others are clear that I am not – repeat not -the “Richard” who made the grossly offensive remark to you. And, yes, whomever that anonymous person is, he/she should apologise to you.
Richard
Phil,
Given that there are quite a few years in the graph with “calculated data” that had no “measured data,” it is clear that the “calculated data” is not derived from any reported measured data.
If you download their measured data set, you can see that there are many years with no data and that the data set corresponds with the red (measured) data in the graph.
So far people have reported three raw measured pH data sets. Monterey, Aloha and Kahe. None of them show a statistically significant trend towards lower pH.
foinavon (03:54:11):
Surely by your own reasoning (add CO2 to blood…the pH goes down), it’s completely obvious that the carbonate concentration of blood will also decrease.
Au contraire, foinavon: by my “own reasoning” CO3 increases, as per my explanation, which you have not refuted in any way.
All you’ve done is to simply re-state over and over that CO3 must decrease when pH decreases from the addition of CO2 to solution, because, lo and behold, “H + CO3 = HCO3” if isolated from everything else – that is, when you have not shown this to be the case anywhere else – except in your in vacuo H.H. example, which, as I noted, simply postulated a ratio, quite apart from what actually happens when CO2 is added to water, both in the basic equations of inorganic chemistry and in real solutions.
J. Peden (09:51:57)
n.b. in order to be crystal clear regarding the meaning of “this” as per the statement below from the above-referenced post:
that is, when you have not shown this to be the case anywhere else
“this” refers to “that CO3 must decrease when pH decreases from the addition of CO2 to solution”
Richard S Courtney (08:57:13) :
That’s the point ‘though isn’t it Richard? We have “checked” and found that quite a bit of what you have said is demonstrably untrue. Isn’t that concerning to you?
It seems to me that we should be attempting to address the science in much the same way that scientists, policymakers and their advisors do. Otherwise we’re going to be increasingly at odds with well-informed policymaking in these important areas. It’s all very well to pursue notions that don’t accord with the straightforward evidence, but if we want to understand policymaking that relates to scientific analysis we should be more like King Canute, and less like his misguided courtiers!
Richard S Courtney (03:34:56) :
Phil:
I have made no “misleading posts”. I have only made factually accurate ones as anybody can check for themselves. If an apology is needed then it is from you for saying otherwise.
No you constantly make misleading posts, this one included!
You say:
“Nonsense! The mass of the atmosphere is ~5×10^18kg, the annual fluctuation of CO2 is ~4ppm so that gives an annual fluctuation of ~20 Gtonne. The annual emission of fossil fuel worldwide in 2004 was ~27 Gtonne, so for your ‘order of magnitude’ greater release of CO2 should result in an annual fluctuation of ~50ppm!”
Sorry, but No!
Actually, yes, as anyone who cares to do the simple calculation can verify.
The Mauna Loa seasonal fluctuation is about 10 ppmv per year (not 4 ppm) see
http://www.esrl.noaa.gov/gmd/ccgg/trends/
Which part of ‘global’ didn’t you understand? In any case reference to that site reveals that the seasonal fluctuation at Mauna Loa is ~6ppm not the 10ppm that you claim. Misleading again!
And Mauna Loa is chosen as a sample site because its seasonal fluctuation is exceptionally low being less than half that elsewhere: e.g. the seasonal fluctuation is more than double that where measured in the Northern Hemisphere, e.g. at Alert, Estavan (both in Canada) and in the Shetland Islands (ref Keeling and Worf, ‘On Line Trends’ CDIAC.ORNL).
That was not the reason Mauna Loa was chosen, you conveniently chose ‘elsewhere’ to be restricted to the N hemisphere. Of course the sites in the S hemisphere show much lower fluctuations: Cape Grim, Baring Head, Samoa, Christmas Island etc. Here’s Bering Head for example:http://cdiac.ornl.gov/trends/co2/graphics/Baring_Head_NZ_CO2.jpg
More misleading information!
Your statement that “The annual emission of fossil fuel worldwide in 2004 was ~27 Gtonne” emphasises my repeated (above) statement that the anthropogenic emissions vary greatly from year-to-year.
How?
As I said, “in some years almost all the anthropogenic emission seems to be sequestered and in other years almost none” (according to data from CDIAC.ORNL). And I have repeatedly pointed out that there are justifiable reasons for smoothing the annual emissions data with at most 3-year averageing but the IPCC uses 5-year averages because 2-yeaqr, 3-year and 4-year smoothings do not work.
Yes you did say that, care to justify it with data?
Typically, according to the NASA estimate, the human emission is about 6.5 GtC/year: see
http://science.hq.nasa.gov/oceans/system/carbon.html
Why the switch in units to GtC, you wouldn’t be trying to mislead would you?
6.5 GtC= 24 Gtonne CO2.
The accumulation rate of CO2 in the atmosphere is equal to almost half the human emission. The human emission is about 6.5 GtC/year but the accumulation rate is about 3 GtC/year. However, this does not mean that half the human emission accumulates in the atmosphere, as is often stated.
No it means that the total non-anthropogenic sources-sinks must be less than the ‘human emission’ by ~3 GtC/year (11 Gtonne CO2)
The system does not ‘know’ where an emitted CO2 molecule originated and there are several CO2 flows in and out of the atmosphere that are much larger than the human emission. The total CO2 flow into the atmosphere is at least 156.5 GtC/year with 150 Gt of this being from natural origin and 6.5 Gt from human origin. So, on the average, about 2% of all emissions accumulate.
And these fluxes are ~balanced so they don’t show up in the measurements other than to modulate the CO2 uptake on a seasonal basis.
And the NASA estimate is that about 100 Gt of carbon are released to the air from the oceans and is sequestered by the oceans each year. This alone is a seasonal fluctuation that justifies my statement that the seasonal variation is an order of magnitude greater than the anthropogenic emission.
If it were a seasonal flux it would show up in the results but it doesn’t except in a small way as described above, it’s averaged out spatially and temporally (e.g. day/night). A bowl of water containing CO2 in equilibrium with a constant composition atmosphere above it doesn’t change [CO2] but fluxes of CO2 in both directions continue in both directions (as seen in by the atom test C-14 response, the spike took 15 yrs to half).
Furthermore, according to the NASA estimate, the carbon in the air is less than 2% of the carbon flowing between parts of the carbon cycle. And the recent increase to the carbon in the atmosphere is less than a third of that less than 2%.
The flows between deep ocean and ocean surface layers are completely unknown and it is not possible even to estimate them. All we know is that the air contains aboout 760 GtC, the ocean surface layer about 800 GtC, and the deep oceans about 38,000 GtC. The thermohaline circulation conveys the major flows between deep ocean and ocean surface layers.
NASA also provides an estimate that the carbon in the ground as fossil fuels is 5,000 GtC, and humans are transferring it to the carbon cycle at a rate of 6.5 GtC per year.
In other words, the annual flow of carbon into the atmosphere from the burning of fossil fuels is less than 0.02% of the carbon flowing around the carbon cycle.
It is not obvious that so small an addition to the carbon cycle is certain to disrupt the system because no other activity in nature is so constant that it only varies by less than +/- 0.02% per year.
Disingenuous, because the net contribution by anthropogenic CO2 must be 11 Gtonne/year.
“The 13C data can be obtained by direct measurement (Mauna Loa since 1959; numerous other measuring stations)”
As I have taken pains to make clear on the prior CO2 Temperatures and Ice Ages thread, Spencer one year ago here at WUWT compared the 13C:12C fraction of the MLO seasonal signal with the long-term trend under F-Test. They were identical.
As the biogenic fluences are seasonal and the anthropogenic is given to be cause for the long term trend the 13C decrease cannot be assigned with any certainty whatever to the latter. The anthropogenic fluence, at least, has been scrubbed from view by the natural. Multiplying words does not add a jot to your argument.
Graeme Rodaughan (04:43:05) :
Simon Evans (08:41:06) :
Graeme Rodaughan (07:58:45) :
In this forum – I also raise my hand and second Alan Millar’s request.
Alan Millar’s question was addressed as follows:
Perhaps some of our alarmist friends would like to explain.
I’m not an alarmist, so I wont be responding to that.
Fair enough – I’ll re-ask politely.
Is anyone able to explain how a warming ocean could absorb CO2 and become more acidic – given that warming oceans have a well known property of outgassing CO2? – Or is this simply a non-starter?
Thanks.
Thanks Graeme. My explanation would be that both occur at the same time – outgassing and absorption, that is – the net effect simply being a matter of whichever is the greater, according to the variables of temperature (and also pH, a lowering of which will itself reduce the sink capacity of the oceans) and atmospheric concentration. At the moment the oceans are absorbing more than they are emitting, but the projections are for the reverse. Therefore, the extent of acidification is limited and, eventually it would be undone. The concern for the corals is that they will be destroyed in the interim. I should stress, though, that this is not my field, so don’t take my word for it! 🙂
Steven Goddard (09:39:49) :
Phil,
“Given that there are quite a few years in the graph with “calculated data” that had no “measured data,” it is clear that the “calculated data” is not derived from any reported measured data.”
Yes, but the claim is that “calculated” data comes from a different methodology not reliant on “measured” data methods. These words “calculate” and “meaure” could be confused when using same in the course of debating the issue.
“If you download their measured data set, you can see that there are many years with no data and that the data set corresponds with the red (measured) data in the graph.”
Holy moly. Can you repost a link to this data set? I think you may have already posted this, but it’s hard for me to search WUWT (especially a long thread like this one), and MS “Find” crashes my browser.
If there is no saved data from the past that could have been used to reconstruct ph for those missing “calculated” times, then it becomes very clear that this graph is very misleading, and junk. Are you sure you are looking at all data sets, not just the ones for the “measured” data?
Even were this not the case though, and “calculated” data plotted did exist, there is still the problem of why no “measured” data exists on much of the graph, why the “measured” was even included if the “calculated” method was more reliable or one was not a calibration of another (which by the large variation in data between the two is clearly not the case).
And there is the question of why the “measured” data was not trendlined as was the “calculated”, if the “measured” data was reliable and an accurate source of ph values.
J. Peden:
Btw, where do you think CO3 comes from to begin with?
CaCO3! We’ve been beating that drum for the last 100 posts!
You say that the Henderson Hasselbach equation is too simple to definitively show that CO2 levels reduce CO3(-2) equations. But this complicated science has ALREADY been done AND observed.
I’ll quote myself again:
http://www.publicaffairs.noaa.gov/releases2002/mar02/noaa02r305.html
“Our results are important in understanding the ocean’s role in the global carbon cycle,” Anderson said. “Prior to this study, large changes in ocean carbonate chemistry had been proposed to explain the changes in atmospheric carbon dioxide. Over thousands of years, calcium carbonate compensation appears to be the dominant variable controlling the ocean carbonate (and carbon dioxide) inventory. When carbon dioxide from the atmosphere is added to the oceans, the calcium carbonate on the seafloor dissolves to minimize the carbon dioxide change in the ocean. ”
If [CO2] increases [CO3(-2)] in the ocean, shouldn’t it be easier to form CaCO3 due to this equilibria: CaCO3 == Ca(++) & CO3(-2) according to Le Chatlier’s principal? In fact, the opposite is shown to be true. The addition of H+ ions is more important to [CO3(-2)] than the dissociation of HCO3(-1) by CO2.
You guys are too focused on the generation of CO3(-2) by CO2 in pure water. CaCO3 is the much greater buffer (which is why oceans are alkaline and not acidic).
I rest my case again.
Steven Goddard (09:39:49) :
Phil,
Given that there are quite a few years in the graph with “calculated data” that had no “measured data,” it is clear that the “calculated data” is not derived from any reported measured data.
No that’s not true the ‘measured data’ refers to direct measurement of pH, ‘calculated’ refers to calculated from other related titrametric methods. I cited a reference earlier.
gary gulrud (11:08:35) :
“The 13C data can be obtained by direct measurement (Mauna Loa since 1959; numerous other measuring stations)”
As I have taken pains to make clear on the prior CO2 Temperatures and Ice Ages thread, Spencer one year ago here at WUWT compared the 13C:12C fraction of the MLO seasonal signal with the long-term trend under F-Test. They were identical.
And as others here, including me have pointed out, that was the result of an elementary math error by Spencer. If you read his recent blog on the subject he makes a different argument about C12/C13 and studiously avoids reference to his post of a year ago! Clearly even he doesn’t believe what he wrote a year ago was reliable, but hasn’t posted a retraction.
http://www.drroyspencer.com/2009/01/increasing-atmospheric-co2-manmade…or-natural/
J Peden, Foinavon:
If there is still debate on this, a little General Chem…
1) H2CO3 = H+ + HCO3- with Ka1 = [HCO3-][H+]/[H2CO3] = 4.2E-7
2) HCO3- = H+ + CO32- with Ka2 = [H+][CO32-]/[HCO3-] = 4.8E-11
overall equilibrium constant, K = Ka1/Ka2 = [HCO3-]^2 / [H2CO3][CO32-]
Increasing CO2 = increasing H2CO3 via CO2 + H2O = H2CO3. Since [H2CO3] is in the denominator of K, an increase in H2CO3 is compensated for by an increase in [HCO3-] and a decrease in [CO32-] governed by the equilibria above. The reason that 2) shifts to the left is due to the relatively large increase in the amount of H+ via 1) because Ka1 is 4 orders of magnitude higher that Ka2! Incidentally, this overall K is equivalent to the RC statement that CO2+H2O+CO32- = 2HCO3-
Chem iz fun…but Chem Eng iz funner
In Phil. (11:07:54) above :Why the switch in units to GtC, you wouldn’t be trying to mislead would you?
6.5 GtC= 24 Gtonne O2
O2 is a typo it should be CO2, moderator please adjust it if possible. Thanks.
Reply: Done ~ charles the moderator
Your comment shows what is wrong with the sceptic view. You just don’t read the evidence,or ignore it if you do. Below is the report on one species Heliopora coerulea from the aforementioned assessment by the 39 scientists. You say that they do not mention CO2, well look closely (I’ve highlighted the relevant part to help you) and see for yourself.
This species is collected for the curio and jewelry trade (dried skeletons give blue color), and the aquarium trade. In 2005, 2,868
pieces of live and 5,787 pieces of raw Heliopora coerulea were exported for the aquarium and curio trade (E. Wood, pers
comm.).
The huge Heliopora stands that extend for almost 10 km in Banda Aceh, Indonesia were the most damaged species of all corals
due to the earthquake (Foster et al. 2006).
In general, the major threat to corals is global climate change, in particular, temperature extremes leading to bleaching and
increased susceptibility to disease, increased severity of ENSO events and storms, and ocean acidification. In addition to global
climate change, corals are also threatened by disease, and a number of localized threats. The severity of these combined threats
to the global population of each individual species is not known.
Coral disease has emerged as a serious threat to coral reefs worldwide and is a major cause of reef deterioration (Weil et al.
2006). The numbers of diseases and coral species affected, as well as the distribution of diseases have all increased dramatically
within the last decade (Porter et al. 2001, Green and Bruckner 2000, Sutherland et al. 2004, Weil 2004). Coral disease epizootics
Conservation Measures
have resulted in significant losses of coral cover and were implicated in the dramatic decline of acroporids in the Florida Keys
(Aronson and Precht 2001, Porter et al. 2001, Patterson et al. 2002). In the Indo-Pacific, disease is also on the rise with disease
outbreaks recently reported from the Great Barrier Reef (Willis et al. 2004), Marshall Islands (Jacobson 2006) and the
Northwestern Hawaiian Islands (Aeby, 2006). Increased coral disease levels on the Great Barrier Reef were correlated with
increased ocean temperatures (Willis et al. 2007) supporting the prediction that disease levels will be increasing with higher sea
surface temperatures. Escalating anthropogenic stressors combined with the threats associated with global climate change of
increases in coral disease, frequency and duration of coral bleaching and ocean acidification place coral reefs in the Indo-Pacific
at high risk of collapse.
Here is a link to the reports on individual coral species in the assessment. http://www.sci.odu.edu/gmsa/about/corals.shtmlRead them and you will see repeated many times the main danger to coral species from climate change and ocean acidification.
I’m sure you mean well and are as concerned about the corals as I am, but you have to look at the evidence and take notice of what the experts in their firld are telling us. Only then can we take the steps necessary to protect a very important resource for future generations.
Hmmmm … still no takers.
OK … 2 sigma.
(Meaning, show me, that the “signal” of lowering pH can be demonstrated, via a classical Gage R&Red set of runs, to be able to demonstrate a 2 sigma margin versus all errors and noise vis a vis repeatability and reliability, plus, bias factors, across a semi infinite half space of ocean mass).
“” This species is collected for the curio and jewelry trade (dried skeletons give blue color), and the aquarium trade. In 2005, 2,868
pieces of live and 5,787 pieces of raw Heliopora coerulea were exported for the aquarium and curio trade (E. Wood, pers
comm.).
The huge Heliopora stands that extend for almost 10 km in Banda Aceh, Indonesia were the most damaged species of all corals
due to the earthquake (Foster et al. 2006). “”
Yep ! unmistakable evidence of global warming and acidification !
George
“” foinavon (13:02:16) :
George E. Smith (12:07:00)
George, we’ve already had the dismal non-”argument” about the meaning of “acidification”. Are you really going to proceed down a pedantic diversion over the meaning of “sinusoidal”?
Remember that words are only labels for the things that we are choosing to describe.
“Sinusoidal” is actually not a bad description of the very well-characterised cyclic variation in the atmospheric CO2 concentration that follows the seasonal growth/decay cycle in the N. hemisphere which is where most of the earth’s flora “resides”. Since the sinusoidal variation lies on a rising trend of growing atmospheric CO2 it does look a bit “sawtooth”.
So let’s call it “sawtooth” if you like. We both know what we’re looking at. “”
Well Foinavon; contrary to what you appear to have assumed, my comment was not at all a “pedantic diversion”; and it was not intended to be dismissive of your comment. If you took it that way, then I apologise.
BUT; would you not agree that the distinction between “roughly sinusoidal” and “roughly sawtooth”, is very significant in the sense that each would be the result of quite different physical processes.
For example, when I look at the satelite graphs of the solar constant measured over sunspot cycles, the resulting variation I would call “roughly sinusoidal”, or even “sinusoidal” if trying to be brief; yet it clearly isn’t sinusoidal, because the peaks are sharper than the troughs, indicating the presence of a second harmonic component. That then begs the question of what physical processes going on in the sun lead to that second harmonic deviation from a sinusoid.
So back to the ML data. The peak and trough turnarounds are very sharp transitions from upslope to downslope and vice versa. Clearly this is not the result of a nearly linear feedback oscillator, which would produce a sinusoidal oscillation.
There is a definite on/off transition occurring, which cause the ML cyclic seasonal variation; and that leads to the question; what is that on/off mechanism.
Now for one thing, deciduous trees lie dormant through the fall/.winter, and then sprout leaves (very quickly) in the spring. I have a home in California’s central valley agricultural area where stone fruit orchards abound (and grapes). Those plants are sprouting leaves en masse, as I type this.
Those trees in the winter, are not taking up CO2 since they have no leaves. The leaves return in the spring in a matter of a week or two; and from there they start sucking up CO2. To a large extent, the mass of foliage doesn’t change after that two week leaf growth period, so you have a rather constant CO2 extraction rate once the leaves are there, and such a mechanism would in fact lead to a saw tooth cyclic variation in CO2. To me the leaf growth/shedding processes of spring and fall, amount to a rectangular pulsed waveform, with rise and fall times of the order of two weeks, but since the time constant of the excess CO2 uptake by that growth process is long comared to the season, the CO2 response is an integration of that rectangular drive signal.
NOW ! I am NOT claiming that this is the process which explains the ML cyclic waveform; but I am saying it is one operating process, which would create such a response.
If you find, and look at the NOAA three dimensional CO2 graph form pole to pole, you will notice that the southern hemisphere cycling is much suppressed from the northern, and to my eye, the very limited south pole cycling, is in fact much closer to a “roughly sinusoidal” variation (still with harmonic content) than it is to a saw tooth; and that suggests to me that the southern CO2 uptake, is likely more ocean related, than land plant growth.
So you see, I was not trying to be smart alecky; but hinting that the waveform isa clue to the mechanism.
But as I said, if you took it as frivolous comment on your post please accept my apology; it wasn’t intended that way at all.
George
Well done George for doing what sceptics do best…picking that little bit that suits your point of view whilst ignoring the more important and relevant evidence and information. If you continue reading you see the main reasons, read the other reports and you may finally remove those sound bite blinkers.
@ur momisugly Steven Goddard et al.,
There still seems to be a great deal of confusion over the meaning of ‘calculated’ vs. ‘measured’ for pH data from the HOT datasets, despite that fact that I’ve explained the meanings at least twice now. In any event, let me try to communicate once and for all how these data were generated.
Seawater pH can be assessed using three methods:
1) With combination electrodes calibrated in appropriate buffers (NIST buffers don’t work well—one needs to use Tris-based buffers made in an artificial seawater solution).
Of the three methods available, this is the LEAST ACCURATE method, and wasn’t used to obtain any of the HOT (or BATS, etc.) data. While this method can be precise to better than +/- 0.005 pH units, it is rarely accurate to +/- 0.005 pH units or better.
2) Spectrophotometrically using the indicator dye m-cresol purple (Clayton and Byrne, 1992). This method did not exist when people started taking the HOT data, therefore could not be used.
Accuracy, as has been assessed in the lab and on many NOAA cruises, is on the order of +/- 0.001 pH units or better. Precision (assessed likewise) is typically +/- 0.0004 pH units or better, and can be up to an order of magnitude better. This is a good method to determine pH when very high accuracy is needed, but unfortunately is somewhat labor intensive (I know, I’ve used this method extensively). This method was used to determine pH in SOME of the Niskin water samples from these sites from 1992-1997, and 2003-present.
The ‘measured’ pH data for the HOT datasets were assessed using this method.
3) Calculated given measured values of:
1) total CO2/DIC, 2) total alkalinity, 3) salinity, 4) total P, 5) total Si, 6) in situ pressure, 7) in situ temperature, 8) experimentally determined dissociation constants (e.g., K1, K2) for carbonic acid.
The accuracy and precision of this method are similar to the m-cresol purple spec. method (~accuracy +/- 0.0007 or better, precision +/- 0.0005 or better).
The ‘calculated’ pH data for the HOT datasets were assessed using this method, and can be re-assessed ad nauseum. All of these data are freely available on the website, and we can produce our own analyses of these results all we want all day long everyday. These data (along with a great deal more) cover the entire period.
Something worth pointing out is that all of these methods, and indeed EVERY possible method of determining pH relies on calculations from measured values. All provide a ‘calculated’ pH relative to experimentally determined calibration values.
The ‘measured’ data in the graphic I presented are for a given subset of the Nisken bottle samples during the sampling period. Only a subset of the Nisken samples could be analyzed because these measurements are somewhat time sensitive, so have to be analyzed rather quickly after sampling.
The ‘calculated’ data in the graphic include data from a much larger set of Nisken bottle samples.
Hence, these data were collected at the same general sites, but they represent measurements of different water masses. The ‘calculated’ values are broader in scope while the ‘measured’ values include only a subset of the same water masses.
If I may use an analogy, the ‘measured’ values here are like measuring the rate of unemployment in all cities in Florida with a population greater than 70,000. The ‘calculated’ values here are like measuring the rate of unemployment in all cities in Florida with a population greater than 5,000. They will inherently include some of the same values and express the same property, but not over precisely the same landscape.
If you still don’t understand where these data come from (and keep in mind, we can analyze and re-analyze, and re-re-analyze all we want since all of the data are freely available) I’m not sure how much more I can help. If you’d like help in obtaining the pertinent data and in analysis I’m happy to get you started.
Claiming that the data should be thrown out simply because you don’t understand where they came from (it’s all in the references/methodology), however, is ridiculous, and terribly nieve. Again, your ignorance is not evidence.
Best,
Chris
p.s. And beyond this point of contention, look at the big picture: if CO2 is added to the atmosphere, is it logically possible that some of it will not dissolved into the ocean? (no, of course not) Is it logically possible (notwithstanding J. Peden et al.,’s severe misunderstanding of carbonate chemistry) to add CO2 to sea water and not reduce the pH of that water? (no, of course not)
Phil (11:07:54) :
“Of course the sites in the S hemisphere show much lower fluctuations: Cape Grim, Baring Head, Samoa, Christmas Island etc. Here’s Bering Head for example:http://cdiac.ornl.gov/trends/co2/graphics/Baring_Head_NZ_CO2.jpg
More misleading information!’
Indeed it is.Baring head station information you supplied has been “seasonally adjusted” This is not a continuous sample it is adjusted for the southern wind flows only ie southern ocean.This is good reasoning as the northern and prevailing aspect is dominated by a regenerating temperate rainforest .
Niwa comments as such
“CO2 concentrations in units of 10^–6 mole/mole (ppm) are shown to the period 2007. Data points represent measurements during southerly wind events extracted from a near-continuous record which has much greater high frequency variability but displays the same long term trend. The red curve shows a time varying trend with the seasonal cycle removed.”
The seasonal ‘sawtooth” of the “unadjusted” co2 record is similar to the CH4 (albeit with different measurements)
http://www.niwa.co.nz/__data/assets/image/0020/43454/Bhd_ch4_800.jpg
Chris J,
If you look at the “calculated” pH data, it has an extremely high standard deviation, does not correlate well with the measured pH data in coincident years, and shows a large inexplicable drop in pH from 1989-1994 (before the measured pH data set started.) That drop, plus inconsistent low calculated readings the last couple of years accounts for almost their entire claimed trend. The calculated data shows variations as high as 0.8 during time periods when the measured data has a peak variance of only 0.2.
I am surprised that they would include such an obviously flawed data set in their trend analysis.
Pete D (11:45:37) :
Thanks for setting out the situation in that way. It makes a lot of sense. However, looking at Ka2, I’m still not totally convinced that, given the equally large increase in [HCO3] in equation 1 resulting from an addition of CO2, equation 2 will be driven to the left by the increase in [H] enough/net to necessitate a net decrease in CO3. K doesn’t necessarily say that, either.
I’ll conceed that you might be right, but I’m still not sure about the net decrease of CO3.