We do not often get the chance to use material with a negative cost but 
this may be one of them.  Figure 2 shows that the two top rings are made 
by lashing used tyres.  We have to pay for the rope but people pay us to 
take the tyres away.

The site    http://press.wrap.org.uk/article/18502/   quotes  amounts up 
to £8.21 each for truck tyres.   Does anyone have figures for the US?

I agree that we should study the biological effects of the first few 
sinks very carefully and try to adjust spacing for the best balance 
between oxygen, CO2 and nutrients.  I would hope that the effects will 
avoid those of the deluge of fertilizer coming down the Mississippi.

I do not think that we will be trying to cool a thick layer of the 
ocean. We preferentially remove the warmest water from the surface, say 
10 to 20 metres depending on our choice of valve wall depth and take it 
down to the thermocline at say 200 metres.   Nathan Myhrvold's model 
suggests that the mixed water rises to the level where it meets water of 
its own density and then spreads sideways like a fairly thin rock 
stratum.   Oil slicks with a higher viscosity spread out quite fast.  We 
have some control of this depth below the surface by choosing the mixing 
ratio though a shape change of the exit.  Ken wants us to get it up to 
100 metres below the surface where there is enough daylight to get the 
phytoplankton started.

As hurricanes provide lots of useful rain we do not want to stop all of 
them, just shift the Whitney-Hobgood figure a chosen amount to the left 
instead rather than letting it creep to the right. 
See http://wind.mit.edu/~emanuel/Papers_data_graphics.htm

Stephen

Emeritus Professor of Engineering Design
School of Engineering and Electronics
University of Edinburgh
Mayfield Road
Edinburgh EH9 3JL
Scotland
tel +44 131 650 5704
fax +44 131 650 5702
Mobile  07795 203 195
[email protected]
http://www.see.ed.ac.uk/~shs    



dsw_s wrote:
>> I hope that they will have a negative material cost.
>>     
>
> How does that work?  Are they made out of some kind of waste material?
>
>   
>> It seems better to stifle them early.
>>     
>
> They're what cools the sea surface farther down their paths, and warm
> Europe.  If you stifle them early, you'll presumably do the opposite.
> That could mean that when you finally don't stifle one, it will have
> warmer water at the latter part of its trajectory, and potentially do
> more damage.
>
>   
>> We do not need to cool the whole Atlantic basin but what goes around comes 
>> around.
>>     
>
> If you warm the whole Atlantic at depths around 100M, doesn't that
> come around too?
>
>   
>> What we are trying to do is replicate la Nina events in a permanent form and 
>> we know that these are very effective at stimulating fish growth. The 
>> artificial upwelling should steadily deliver the full cocktail of all the 
>> natural nutrients in the same way as the natural upwellings which are 
>> unfortunately rare.
>>     
>
> The ecology of a food source with occasional mastings or population
> explosions is likely to be different from that of a smaller but steady
> food source.  The more often we remake the ecology of the oceans, the
> more extinctions will accumulate.  On the other hand, artificial
> upwelling may help stop extinctions in some specific cases.  We need
> to learn about the ecology that we're already pervasively affecting.
> Interventions made in near-total ignorance are more likely to do harm
> than good.
>
>   
>> You write that hurricane formation needs hot water down to 150 feet.  If 
>> this is right it should make them more vulnerable to deliberate cooling.
>>     
>
> A thick layer of water is harder to cool than a thin layer, so if the
> development of hurricanes is dependent on the temperatures of a thick
> layer that should mean they're less sensitive to deliberate cooling.
>
>
>   
>>     
>
>   

-- 
The University of Edinburgh is a charitable body, registered in
Scotland, with registration number SC005336.


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