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The ocean turnover time is 1500 years, as determined from radiocarbon measurements.
This applies to heat uptake as well as CO2.
Thomas J. F. Goreau, PhD
President, Global Coral Reef Alliance
Chief Scientist, Blue Regeneration SL
President, Biorock Technology Inc.
Technical Advisor, Blue Guardians Programme, SIDS DOCK
37 Pleasant Street, Cambridge, MA 02139
gor...@globalcoral.org
www.globalcoral.org
Skype: tomgoreau
Tel: (1) 617-864-4226 (leave message)
Books:
Geotherapy: Innovative Methods of Soil Fertility Restoration, Carbon Sequestration, and Reversing CO2 Increase
http://www.crcpress.com/product/isbn/9781466595392
Innovative Methods of Marine Ecosystem Restoration
http://www.crcpress.com/product/isbn/9781466557734
No one can change the past, everybody can change the future
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On Sep 24, 2021, at 9:42 AM, briancar...@gmail.com <briancar...@gmail.com> wrote:
Thanks Mike and Ken for your responses. I would have expected the complicating factor of deep ocean carbon taking longer to be equilibrated. Otherwise I'm still looking for an answer about how long overall re-equilibration would take.
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I want to point out the scenario bias with what we see in the
literature and the big picture of future climate pathways.
There are no scenarios in the consensus world that go lower than
net zero or 1.5 C. The vast body of literature does not consider
quantities of atmospheric removal of CO2 (or other GHGs) needed
for restoration scenarios, where climate restoration is defined as
returning our climate to within the evolutionary boundaries of
stable Earth systems. So when understanding the big picture with
findings on the trajectory of our future climate and the
associated behavior of Earth systems, it must be understood that
Earth systems will further deteriorate with further warming with
all consensus scenarios. Further warming increases temperature and
other feedback processes, that include atmospheric/biosphere gas
equilibrium processes, as our current climate moves farther away
from the evolutionary boundaries of our former climate.
Hansen's "Young People's Burden..." suggests the upper limits of the evolutionary boundary conditions of our old climate, that represent the evolution of Earth systems, is centered around 350 ppm CO2 ("Holocene maximum" below). Our Earth systems will not instantly reevolve to new boundary conditions when boundary conditions change beyond systems' evolution. If we can turn the temperature around fast enough and cool Earth back to withing its systems' evolutionary boundaries before these systems complete their collapses that have already begun (Lenton 2019), Earth systems' evolutionary equilibrium will be maintained and outgassing begins.
If we continue to warm to 1.5 C as all the consensus scenarios
suggest, we move farther away from Earth systems' equilibrium and
sequestration increases. In other words, increased atmospheric CO2
with 1.5 C and net zero targets increases partial pressures of
atmospheric gases further from today, causing greater biosphere
absorption --if-- Earth systems remain healthy. Only through
restoration scenarios where we lower atmospheric CO2 below Earth
systems' equilibrium evolution will outgassing of sinks occur,
with the exception of collapsing Earth systems where sequestration
is degraded, eliminated or reversed.
Because there are no restoration scenarios accepted by consensus
reporting, what is described above is not included in the vast
majority of science on pathways our future climate will take,
especially consensus pathways. When we view findings or popular
press reporting of findings, it is vitally important to understand
the basis for findings. If we incur further warming, of course
climate processes are irreversible from where we are today, in
time frames that matter. If restoration scenarios are not
included in our vision of our future climate, there is literally
an existential bias in what findings reveal.
Caveat: The above concepts are generalizations. Some (all)
systems behave differently and their behavior varies from the
generalities described above. But in general, future climate
pathway findings exhibit a bias because they only consider
scenarios with further warming.
Bruce

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A pre-industrial GHG goal is needed to avoid serious disruption, which a 1.5 warming goal minimizes only with regard to worse: 2 or 5 degrees warming.
We need to start Geotherapy by planting trees and putting biochar into soil and regenerating blue carbon RIGHT NOW just as fast as we can, just in case a high technology fix can be developed in time to help later.
Thomas J. F. Goreau, PhD
President, Global Coral Reef Alliance
Chief Scientist, Blue Regeneration SL
President, Biorock Technology Inc.
Technical Advisor, Blue Guardians Programme, SIDS DOCK
37 Pleasant Street, Cambridge, MA 02139
gor...@globalcoral.org
www.globalcoral.org
Skype: tomgoreau
Tel: (1) 617-864-4226 (leave message)
Books:
Geotherapy: Innovative Methods of Soil Fertility Restoration, Carbon Sequestration, and Reversing CO2 Increase
http://www.crcpress.com/product/isbn/9781466595392
Innovative Methods of Marine Ecosystem Restoration
http://www.crcpress.com/product/isbn/9781466557734
No one can change the past, everybody can change the future
From: <carbondiox...@googlegroups.com> on behalf of "Bruce Melton -- Austin, Texas" <bme...@earthlink.net>
Date: Friday, September 24, 2021 at 11:50 AM
To: "carbondiox...@googlegroups.com" <carbondiox...@googlegroups.com>
Subject: Re: [CDR] Re: Question re: re-equilibration of carbon stored in the ocean
I want to point out the scenario bias with what we see in the literature and the big picture of future climate pathways.
To view this discussion on the web visit
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B.1 Global surface temperature will continue to increase until at least the mid-century
under all emissions scenarios considered. Global warming of 1.5°C and 2°C will be
exceeded during the 21st century unless deep reductions in CO2 and other greenhouse
gas emissions occur in the coming decades. (SPM p. 16)
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Brian, thanks for this discussion. I find it hard to understand how net zero could stabilise the climate with liveable conditions, and without massive risk.
Net zero by 2050 would result in a trillion tonnes of anthropogenic carbon in the air that would then stay there for a long time unless there are large technological removals.
The last time GHGs were that high was millions of years ago, when temperatures and sea level were much higher than today.
Simple earth system equilibrium calculations suggest that without removing that extra carbon, higher temperature and sea level are eventually inevitable. And destabilising risks to forests, currents, ice, etc are severe.
Net zero looks to be a very complacent goal, in terms of human security and biodiversity conservation.
What am I missing?
Regards, Robert
From: carbondiox...@googlegroups.com <carbondiox...@googlegroups.com> On Behalf Of briancar...@gmail.com
Sent: Monday, 27 September 2021 2:22 AM
To: Carbon Dioxide Removal <CarbonDiox...@googlegroups.com>
Subject: Re: [CDR] Re: Question re: re-equilibration of carbon stored in the ocean
To Greg and group,
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It’s not quite right to imply that the temperature is “frozen in” once water leaves the surface.
The downwelled water is constantly exchanging heat with other water masses in the ocean through convection and eddy diffusion along pycnocline density surfaces (NOT laminar flow or diffusiion, which is far slower), and when it returns to the surface, around 1500 years later on the average, it will then re-equilibrate temperature with the atmosphere boundary layer.
Thomas J. F. Goreau, PhD
President, Global Coral Reef Alliance
Chief Scientist, Blue Regeneration SL
President, Biorock Technology Inc.
Technical Advisor, Blue Guardians Programme, SIDS DOCK
37 Pleasant Street, Cambridge, MA 02139
gor...@globalcoral.org
www.globalcoral.org
Skype: tomgoreau
Tel: (1) 617-864-4226 (leave message)
Books:
Geotherapy: Innovative Methods of Soil Fertility Restoration, Carbon Sequestration, and Reversing CO2 Increase
http://www.crcpress.com/product/isbn/9781466595392
Innovative Methods of Marine Ecosystem Restoration
http://www.crcpress.com/product/isbn/9781466557734
No one can change the past, everybody can change the future
Those with their heads in the sand will see the light when global warming and sea level rise wash the beach away
Geotherapy: Regenerating ecosystem services to reverse climate change
To view this discussion on the web visit
https://groups.google.com/d/msgid/CarbonDioxideRemoval/CAJ3C-042rrMdC0BcNAXhA06WtzWr56%2Bs17doctCVS%2Bigm7wM-A%40mail.gmail.com.
Andrew,
You said:
“Until water is down welled, it's much like soft drinks. Opening the can causes the dissolved CO2 to degas. This happens from absolute not partial pressure change in this example, but the effect is equivalent.”.
However, this is not the case as CO2 in soft drinks behaves differently from CO2 in sea water. In soft drinks CO2 is in the form of dissolved gas whereas in sea water very little CO2 is in the form of dissolved gas with most as bicarbonate and some as carbonate. The proportions will vary with pH – see the Bjerrum diagram showing the relative concentrations of the carbon species in seawater according to pH:

As you can see, the CO2 (aq) concentration at seawater pH of around 8 is a tiny fraction of the bicarbonate and carbonate concentrations – note the logarithmic scale.
Best wishes
Chris.
From: carbondiox...@googlegroups.com <carbondiox...@googlegroups.com> On Behalf Of Andrew Lockley
Sent: 29 November 2021 22:02
Cc: Carbon Dioxide Removal <CarbonDiox...@googlegroups.com>
Subject: Re: [CDR] Question re: re-equilibration of carbon stored in the ocean
At CEC 15 there was a presentation (Ken's?) showing the persistent effects on ocean water. Once water has downwelled, it's no longer in contact with the atmosphere. It cannot then exchange heat (or CO2) with the atmosphere, and exchange with adjacent water masses is limited (presumably more so in laminar flow).
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Andrew,
Your post may be a simplification but your comparison between the release of CO2 from soft drinks and getting to equilibrium between CO2 in the atmosphere and CO2 in sea water after removal of CO2 from sea water is not a valid one as I said previously.
Also, the equilibration of the ocean with the atmosphere is not instantaneous but can take from days to weeks or longer. See the paper by Bach et al. (2021) – https://www.nature.com/articles/s41467-021-22837-2 who say:
“Atmospheric CO2 influx into the surface seawater, after CO2-fixation by Sargassum, takes 2.5–18 times longer than the CO2-deficient seawater remains in contact with the atmosphere, potentially hindering CDR verification.”
Also, note that Planetary Hydrogen (https://www.planetaryhydrogen.com/) in their presentations have assumed a period of weeks to months for equilibration of CO2 after ocean alkalinity enhancement.
Also, some parts of the ocean appear not to be in equilibrium with the atmosphere e.g. Karl and Letelier (2008) - https://www.int-res.com/abstracts/meps/v364/p257-268/ - say this about the Pacific Ocean at Station ALOHA, so it would appear that equilibrium cannot be assumed to be inevitable.
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Sorry to pile on, Andrew! As Chris points out, ocean CO2 is much more complicated than a soda bottle, a misleading analogy worth correcting.
Measurements of CO2 in surface water and air have been done worldwide for decades and are rarely in equilibrium. So that is rarely the starting point for deep water.
In general tropical waters are supersaturated and polar waters undersaturated compared to the atmosphere, as expected from solubility coefficients, so there are strong regional and seasonal fluxes in both directions vertically and horizontally.
Dissolved CO2 is almost never limiting for marine phytoplankton, except that it can be locally depleted inside dense green “pea soup” blooms where CO2 uptake exceeds the rate at which bicarbonate can resupply it.
Part of that disequilibrium is because hydration of CO2 is the kinetically slow, rate-limiting step, and so is largely mediated enzymatically by carbonic anhydrase, and affected by surface microfilms.
Andrew’s point though was purely about subsurface transport and equilibration, but there are significant CO2 sources and sinks WITHIN the ocean, and very rapid horizontal mixing of both heat and CO2 by eddies along density surfaces, but much less vertical mixing, thus keeping the lid on acid high CO2 bottom waters fed by decomposition of all that organic matter falling to the bottom.
Small changes in ocean circulation can greatly change the rate and location at which that CO2 comes back to the surface, as it must eventually.
Dumping algae on the deep ocean bottom gives you around 1500 years CO2 delay on the average, but much less in the Atlantic.
Bicarbonate alkalinization gives around 100,000 years of carbon storage.
Limestone and black carbon (high grade biochar) a few 100,000,000 years.
Thomas J. F. Goreau, PhD
President, Global Coral Reef Alliance
Chief Scientist, Blue Regeneration SL
President, Biorock Technology Inc.
Technical Advisor, Blue Guardians Programme, SIDS DOCK
37 Pleasant Street, Cambridge, MA 02139
gor...@globalcoral.org
www.globalcoral.org
Skype: tomgoreau
Tel: (1) 617-864-4226 (leave message)
Books:
Geotherapy: Innovative Methods of Soil Fertility Restoration, Carbon Sequestration, and Reversing CO2 Increase
http://www.crcpress.com/product/isbn/9781466595392
Innovative Methods of Marine Ecosystem Restoration
http://www.crcpress.com/product/isbn/9781466557734
No one can change the past, everybody can change the future
Those with their heads in the sand will see the light when global warming and sea level rise wash the beach away
Geotherapy: Regenerating ecosystem services to reverse climate change
To view this discussion on the web visit
https://groups.google.com/d/msgid/CarbonDioxideRemoval/0c2901d7e6ab%24eed87c00%24cc897400%24%40btinternet.com.
Two comments.
The comment that sea water takes time to reach equilibrium with atmospheric CO2 is correct; transfer of CO2 to water is the rate limiting step for surface grown biomass. It also helps explain why one gets ocean spring “blooms” rather than persistent growth of biomass. But regardless: water in the North Atlantic, despite replenishment by the Gulf Stream, is essentially saturated in CO2 prior to downwelling: dats is in p 206 in
Zhou, S., Flynn, P.C. Geoengineering Downwelling Ocean Currents: A Cost Assessment. Climatic Change 71, 203–220 (2005). https://doi.org/10.1007/s10584-005-5933-0
Peter
Peter Flynn, P. Eng., Ph. D.
Emeritus Professor and Poole Chair in Management for Engineers
Department of Mechanical Engineering
University of Alberta
Edmonton, Alberta, Canada
From: 'Chris Vivian' via Carbon Dioxide Removal <CarbonDiox...@googlegroups.com>
Sent: Wednesday, December 1, 2021 5:07 AM
To: 'Andrew Lockley' <andrew....@gmail.com>
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I have been slightly puzzled by comments of late that Antarctic waters are undersaturated in CO2.
Some years back, Songjian Zhou and I looked at ways to get more CO2 into the deep ocean, and we speculated that North Atlantic water would be undersaturated in CO2, since it had a component of the warm Gulf Stream flowing north. The thought was that CO2 uptake took time, so the cold water in the North Atlantic would not have equilibrated. We found data that suggested that this is simply wrong: numerous samples indicated near saturation in CO2. We abandoned the thought of exploring ways to enhance CO2 concentration in the North Atlantic Deep Water, the downwelling current that is the offset of the Gulf Stream. Data on saturation in the North Atlantic is in the attached paper.
So the thought that this is not the case in the Antarctic is interesting. Perhaps even moreso because of the report of upwelling deep water in the Antarctic degassing; I cannot imagine that this component would degas past saturation.
Peter Flynn
Peter Flynn, P. Eng., Ph. D.
Emeritus Professor and Poole Chair in Management for Engineers
Department of Mechanical Engineering
University of Alberta
Edmonton, Alberta, Canada
As you can see, the CO2 (aq) concentration at seawater pH of around 8 is a tiny fraction of the bicarbonate and carbonate concentrations – note the logarithmic scale.
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The atmospheric data in Long et al (cited below) show clear strong Antarctic Circumpolar Current uptake of CO2 from the atmosphere in the Southern Hemisphere Summer (just starting):
The Antarctic Circumpolar Current ACC is the largest cold water current, highly unsaturated in CO2, and has the strongest ocean waves to mix water with air, making it the most crucial zone controlling global CO2 uptake from atmosphere to the ocean. New papers of measurements on very different time scales show these fluxes can change dramatically, with major carbon dioxide removal implications.
Long et al, 2021, Strong Southern Ocean carbon uptake evident in airborne observations, Science, 374:1275-1280, presents aircraft measurements in 2016 that show rapid seasonal changes in CO2 atmosphere ocean fluxes, with the largest atmosphere drawdown during the southern summer, confirmed by surface measurements from 1999-2019. They discuss the need for more air-borne measurements to quantify changing fluxes and do not seem to discuss long-term trends.
Wu, S., Lembke-Jene, L., Lamy, F. et al. Orbital- and millennial-scale Antarctic Circumpolar Current variability in Drake Passage over the past 140,000 years. Nat Commun 12, 3948 (2021). https://doi.org/10.1038/s41467-021-24264-9 discuss changes in the ACC over an entire glacial/interglacial cycle. Sediments at the bottom of the Drake Passage, the critical choke point of the ACC, show strong variations in grain size related to current velocity, with highest speeds in warm periods and least during glaciations. The last Interglacial around 130,000 years ago was 1-2 C warmer than today, and the ACC velocity even higher than present. Increasing velocities expected with global warming should cause more release of CO2 from ocean to atmosphere, potentially turning a sink into a source.
It should be noted that the 2021 Antarctic winter had an extremely strong cold anomaly and Polar High Pressure Zone, surrounded by very low pressure zone over the ACC. The high pressure gradient drove very strong, cold, outward katabatic winds from the Ice Cap over the ACC, and strong winds caused very high waves and atmosphere-ocean fluxes. When the 2021 Southern Summer began, the Polar High Pressure Zone disappeared, strongly weakening wind and wave induced atmosphere-ocean CO2 transport. Dramatic weather changes like this should be reflected in rapidly changing CO2 sources and sinks.
Similar airborne sensing is needed over the world’s strongest, and hottest ocean currents, the Equatorial Currents, the major source of CO2 from ocean to atmosphere. These are subject to strong changes on ENSO, Madden-Julian, and other cycles, and after a very prolonged La Niña, the next El Niño, which appears to be starting, could cause large variations in the major ocean-atmosphere CO2 sources.
Small fluctuations in either current could dramatically change atmosphere CO2 trends. As Wally Broecker used to point out: you should expect surprises when you mess with climate!
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