Cross-posting thread, due to relevance.

I'm unaware of any modelling that has looked into the CO2 dissolution
effect of below-pre-industrial polar cooling. This would likely be at both
poles, due to the need to avoid a shift in the ITCZ

Comments from SRM geoengineering experts on this approach is particularly
welcome.

Andrew

On Tue, 14 Aug 2018, 06:55 Thomas Goreau, <[email protected]> wrote:

> A major factor in the Ice Age drawdown, which is claimed to be due to iron
> fertilization of phytoplankton seems instead/also to be the increased
> formation of very cold deep water around Antarctica with very high
> dissolved CO2 content due to the cold temperatures.
>
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> *Thomas J. F. Goreau, PhDPresident, Global Coral Reef AlliancePresident,
> Biorock Technology Inc.Coordinator, Soil Carbon AllianceCoordinator, United
> Nations Commission on Sustainable Development Small Island Developing
> States Partnership in New Sustainable Technologies37 Pleasant Street,
> Cambridge, MA [email protected]
> <[email protected]>www.globalcoral.org
> <http://www.globalcoral.org>Skype: tomgoreauTel: (1)
> 617-864-4226Books:Geotherapy: Innovative Methods of Soil Fertility
> Restoration, Carbon Sequestration, and Reversing
> CO2 Increasehttp://www.crcpress.com/product/isbn/9781466595392
> <http://www.crcpress.com/product/isbn/9781466595392>Innovative Methods of
> Marine Ecosystem
> Restorationhttp://www.crcpress.com/product/isbn/9781466557734
> <http://www.crcpress.com/product/isbn/9781466557734>*
>
> On Aug 14, 2018, at 7:24 AM, Charles Greene <[email protected]> wrote:
>
> Note the following quote from the “Dust in the Wind” website that was
> cited:
>
> "Although Martin had proposed that purposeful iron addition to the
> Southern Ocean could reduce the rise in atmospheric CO2, Sigman noted that
> the amount of CO2 removed though iron fertilization is likely to be minor
> compared to the amount of CO2 that humans are now pushing into the
> atmosphere.”
>
> “The dramatic fertilization that we observed during ice ages should have
> caused a decline in atmospheric CO2 over hundreds of years, which was
> important for climate changes over ice age cycles,” Sigman said. “But for
> humans to duplicate it today would require unprecedented engineering of the
> global environment, and it would still only compensate for less than 20
> years of fossil fuel burning.”
>
> On Aug 10, 2018, at 6:26 AM, 'Robert Tulip' via Carbon Dioxide Removal <
> [email protected]> wrote:
>
> Dear Thomas,
>
> Your claim that "the solutions to runaway global warming lie in the soil
> and terrestrial vegetation, not the oceans" appears to conflict with a
> dominant natural cooling mechanism of our planet.
>
> As I mentioned in reply to comments from Greg Rau, a paper published in
> Science available at Dust in the wind drove iron fertilization during ice
> age
> <https://www.princeton.edu/news/2014/03/21/dust-wind-drove-iron-fertilization-during-ice-age>,
> found that “iron fertilization of Southern Ocean plankton can explain
> roughly half of the CO2 decline during peak ice ages”.  This scale of
> impact, removing about 50 parts per million of CO2, could potentially be
> replicated in time frames relevant to anthropogenic climate change,
> especially since this increase in primary productivity due to dust also
> involves increased deposition of carbon to the ocean floor, as explained by
> Hendy <http://www.pnas.org/content/112/2/306>.
>
> The massive increase in ocean primary productivity in the ice ages, when
> CO2 level fell by 100 ppm, did not produce anoxia, or the other
> hypothetical adverse effects that people have posited, as indicated in
> benthic sediments.  The amount of unused nutrient in the High Nutrient Low
> Chlorophyll regions of the world ocean, more than sixty million square
> kilometres in size, is enough to significantly increase the ocean primary
> biomass, with likely flow-on benefits for biodiversity and cooling.
>
> Clearly there is much more need for research, especially computer
> modelling and field tests. The rationale is that working out the best ways
> to mimic the natural cooling feedback amplifiers of the ice age, for
> example using iron salt aerosol
> <https://www.earth-syst-dynam.net/8/1/2017/>, could well remove more
> carbon than the decarbonisation plans of the Paris Accord, at a fraction of
> the cost and risk.
>
> Robert Tulip
>
>
> ------------------------------
> *From:* Thomas Goreau <[email protected]>
> *To:* Greg Rau <[email protected]>
> *Cc:* Carbon Dioxide Removal <[email protected]>; "
> [email protected]" <[email protected]>; "[email protected]" <
> [email protected]>; "[email protected]" <[email protected]>;
> Soil Age <[email protected]>
> *Sent:* Friday, 10 August 2018, 5:20
> *Subject:* [CDR] Ocean carbon versus land carbon sequestration
>
> Unfortunately these errors are all too typical of the sort of nonsense
> about marine carbon widely propagated in the popular press.
>
> Terrrestrial biomass is around 200 times greater than ocean biomass.
>
> Dissolved organic carbon is very resistant to decomposition, it is
> composed of residues inedible to bacteria that lasts for thousands of years
> but forms slowly.
>
> Most terrestrial biomass is soil carbon with lifetimes of centuries to
> millennia, and woody tree trunks with lifetime of decades to centuries, but
> most ocean biomass dies, rots, or is eaten and returned to the atmosphere
> as CO2 in just days.
>
> All this stuff recently posted about growing marine biomass as a carbon
> sink is literally pie in the sky, you just can’t grow it fast enough and
> keep it from recycling to make the difference needed to atmospheric CO2.
>
> Soil carbon enhancement is the only likely way to cost-effectively store
> carbon and bank it to increase positive future benefits in soil fertility
> and food production.
>
> On the other hand most CDR proposals are far more costly, and by removing
> CO2 and blocking the natural recycling of carbon, are just running down the
> future capacity of the biosphere to safely regulate global atmospheric
> composition, temperatures, water supplies, and food, our planetary life
> support systems.
>
> Soil carbon enhancement could draw down the dangerous excess CO2 to safe
> levels in decades if we used state of the art carbon farming methods, but
> unfortunately only a few people are now doing so.
>
> The solutions to runaway global warming lie in the soil and terrestrial
> vegetation, not the oceans.
>
>
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>
> *Thomas J. F. Goreau, PhDPresident, Global Coral Reef AlliancePresident,
> Biorock Technology Inc.Coordinator, Soil Carbon AllianceCoordinator, United
> Nations Commission on Sustainable Development Small Island Developing
> States Partnership in New Sustainable Technologies37 Pleasant Street,
> Cambridge, MA [email protected]
> <[email protected]>www.globalcoral.org
> <http://www.globalcoral.org/>Skype: tomgoreauTel: (1)
> 617-864-4226Books:Geotherapy: Innovative Methods of Soil Fertility
> Restoration, Carbon Sequestration, and Reversing
> CO2 Increasehttp://www.crcpress.com/product/isbn/9781466595392
> <http://www.crcpress.com/product/isbn/9781466595392>Innovative Methods of
> Marine Ecosystem
> Restorationhttp://www.crcpress.com/product/isbn/9781466557734
> <http://www.crcpress.com/product/isbn/9781466557734>*
>
> On Aug 9, 2018, at 8:55 AM, Greg Rau <[email protected]> wrote:
>
>
>
> https://www.scientificamerican.com/article/first-photos-of-ocean-carbon-molecules-hold-clues-to-future-warming/?utm_source=newsletter&utm_medium=email&utm_campaign=daily-digest&utm_content=link&utm_term=2018-08-09_top-stories&spMailingID=57152538&spUserID=MzMzNDg5MjEwMjQ1S0&spJobID=1461217435&spReportId=MTQ2MTIxNzQzNQS2
>
> "From undulating surface to inky black depths, Earth’s oceans are littered
> with the carcasses of tiny life-forms called phytoplankton that in life
> form the basis of the marine food chain.
>
> These microscopic ghosts contain a reservoir of carbon estimated at a
> staggering 662 gigatons—200 times greater than the amount stored in all
> living plants and animals—that could come back to haunt us if unleashed
> from its watery grave as planet-warming carbon dioxide.
>
> Some of the carbon-containing molecules in these plankton remnants will
> remain locked away for millions of years on the seafloor, but some will
> break down and enter the atmosphere as carbon dioxide. A huge portion will
> continue to circulate freely in the ocean for generations. But exactly
> which molecules are destined for which fate—and therefore how much of this
> vast carbon pool is headed for the atmosphere via ocean warming,
> acidification, sunlight or digestion by microbes—is an outstanding
> question. Answering it requires a clearer picture of the structure of the
> molecules that contain this carbon. An international team of scientists has
> now taken the first “photographs” of these molecules in an effort to start
> parsing that out. This first glimpse suggests that while a catastrophic
> breakdown and release of carbon seems unlikely, there is much left to
> understand about the behavior of oceanic carbon."
>
> GR - Some inexcusable errors here.  Carcasses of phytoplankton do not
> constitute 662 Gt C, but rather dissolved organic carbon (DOC) derived from
> biomass (mostly marine) constitute some 700 Gt C in the ocean (IPCC 2013,
> Fig. 6.1). Living marine biomass is only 3 Gt. Meantime, living biomass on
> land is some 500 Gt C. So no way is DOC "200 times greater than the [C]
> amount stored in all living plants and animals". Nevertheless, we indeed
> need to make sure that the DOC doesn't "come back to haunt us" such as if
> climate change accelerates DOC respiration.  For further perspective, the
> ocean contains 38,000 Gt C in dissolved inorganic form, dwarfing any other
> reservoir in contact with the atmosphere (850 Gt C). I.e it's pretty clear
> where nature likes to store C; shall we follow her lead or try to do
> something different?
>
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