Caldeira et al showed that moving water in this way causes warming.

A

On 8 Sep 2017 00:15, "'Robert Tulip' via geoengineering" <
[email protected]> wrote:

> Thanks Cristoph.
> Deep Ocean Water, with volume about a billion cubic kilometres below the
> thermocline, has about three ppm nitrate and phosphate, about 3000 cubic
> kilometres of each, as I understand the numbers. Tidal pumping arrays along
> the world's continental shelves could raise enough DOW to the surface,
> mimicking natural algae blooms, to fuel controlled algae production at the
> scale required for seven million square kilometres of factories.  Piping
> CO2 from power plants etc out to ocean algae farms could clean up all the
> polluted air of the world.
> Robert Tulip
>
>
> ------------------------------
> *From:* Christoph Voelker <[email protected]>
> *To:* [email protected]
> *Sent:* Friday, 8 September 2017, 8:43
> *Subject:* Re: [geo] Carbon budget/removal in NYTimes interactive
>
> I must admit that I am getting skeptical when I hear numbers in that order
> of magnitude:
> The total net primary production in the oceans presently is about 50 Gt
> carbon, and 80% of that is converted back into inorganic carbon (and
> nutrients) by heterotrophs before it gets a chance to sink out from the
> sunlit upper layer of the ocean. The roughly 10 Gt carbon (some newer works
> even estimate just 6 Gt carbon) that sink out have to be balanced by the
> upward mixing of nutrients (and a little bit by atmospheric deposition of
> bioavailable nitrogen and phosphorus) in the Redfield ratio of about
> 106:16:1 of C:N:P.
> So, if you want to remove 20 Gt carbon per year from the atmosphere, you'd
> have to increase the nutrient supply to the total surface ocean by a factor
> of three, maybe four. Maybe I am a bit too pessimistic here, because there
> are species like Sargassum which have a higher C:N:P ratio than the average
> phytoplankton, so you get somewhat more carbon per nitrogen/phosphorus. But
> even if it is just doubling, I can't imagine that you can sustain such a
> nutrient consumption by fertilizing from outside the ocean (especially
> since phosphorus is scarce already now), you'd have to tap into the
> inorganic nutrients stored in the deep ocean. How long can you do that?
> If we assume that we harvest all the 20 Gt carbon in algae from these
> factories and do something durable with them (to minimize lossed through
> heterotrophy and problems with creating oxygen minimum zones), we
> effectively remove nitrogen/phosphorus from the ocean. How much is that per
> year?
> Let us for simplicity assume Redfield ratios, I grant errors by a factor
> of two or so. 20 Gt carbon then corresponds to (20
> g/12(g/mol)/6.625(molC/molN))*1.0e15 or about 2.5e14 mol nitrogen. The
> ocean has a volume of 1.33e18 m^3, and the average concentration of
> available nitrogen (mostly nitrate) is 30 micromol/L or mmol/m^3
> (calculated from the world ocean atlas), most of that is in the deep ocean.
> This gives a total inventory of 4.0e16 mol nitrogen. 2.5e14 mol/year is
> thus more than half of a percent of the total available nitrogen in the
> world oceans, which means you could try that for about 150 years, then
> everything is gone At that pace, nitrogen fixers are unlikely to resupply
> the loss (nowaday, the residence time of nitrogen is roughly 5000 years),
> and they can do that only for nitrogen, not for phosphorus anyway. Letting
> technological problems aside (like: How do you move 2.5% of the total
> nitrogen in the world oceans evry year up to an area 2% of the ocean
> surface) I would call the whole idea - at least that the scale suggested -
> a prime example of an unsustainable process.
> Best regards,
> Christoph Voelker
>
> On 07.09.17 23:37, 'Robert Tulip' via geoengineering wrote:
>
> The assumption behind the NYT interactive model
> <https://www.nytimes.com/interactive/2017/08/29/opinion/climate-change-carbon-budget.html?action=click&pgtype=Homepage&clickSource=story-heading&module=opinion-c-col-right-region&region=opinion-c-col-right-region&WT.nav=opinion-c-col-right-region>
> that the upper bound for carbon removal is 12 GT CO2 by 2080 is too slow
> and small.  We should think five times as much and five times as fast.
> Immediate aggressive investment to build industrial algae factories at sea
> could remove twenty gigatons of carbon (50 GT CO2) from the air per year by
> 2030, using 2% of the ocean surface, funded by use of the produced algae.
> That would stabilise the climate and enable no change in emission
> trajectories, a policy result that would satisfy both the needs of the
> climate and the traditional economy.
> Robert Tulip
>
>
> ------------------------------
> *From:* Eric Durbrow <[email protected]> <[email protected]>
> *To:* geoengineering <[email protected]>
> <[email protected]>
> *Sent:* Thursday, 7 September 2017, 3:13
> *Subject:* [geo] Carbon budget/removal in NYTimes interactive
>
>
> FYI There is a slick interactive graphic at the NYTimes that lets people
> see if they can meet the world’s carbon budget restriction but a
> combination of reduced emissions AND achieving Carbon Removal.
>
> At
>
> https://www.nytimes.com/interactive/2017/08/29/
> opinion/climate-change-carbon-budget.html?action=click&
> pgtype=Homepage&clickSource=story-heading&module=opinion-
> c-col-right-region&region=opinion-c-col-right-region&WT.
> nav=opinion-c-col-right-region
>
> I failed after clicking on Reduce in all geographic areas and Achieve in
> Carbon Removal.
>
>
>
>
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> --
> Christoph Voelker
> Alfred Wegener Institute for Polar and Marine Research
> Am Handelshafen 12
> 27570 Bremerhaven, Germany
> e: [email protected]
> t: +49 471 4831 1848 <+49%20471%2048311848>
>
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