Hi Brian,

My first thought was that you must be mad to even consider such an idea.
But actually there is an acute problem with warm ocean currents melting
away at the terminations of Antarctic glaciers and causing accelerated ice
mass loss "beyond a tipping point" for some glaciers.  If we could mix the
colder currents with warmer currents, this might slow the ice mass loss.

Cheers, John


On Sat, Oct 10, 2015 at 8:29 AM, Brian White <gaiatechnic...@gmail.com>
wrote:

>
> <https://upload.wikimedia.org/wikipedia/commons/8/87/Drake-Passage_profile_hg.png>
> The drake passage is around 800 km wide and if the current in the southern
> half of the passage was slowed (even slightly) the Antarctic continent
> could be released from its splendid isolation.  If a series of anchors with
> wire ropes 2 km long held up by some sort of buoy (4 or 8 thousand of
> them)  were dropped from the Antarctic side, they would slow  the freezing
> current somewhat and create eddies as the current passes them.  The eddies
> would warm the water and this would reduce the extreme temperature
> differences that cause the winds. Very gradually, we could stop the
> freezing current and the winds that keeps it separate from the rest of the
> climate of the earth.   What happens then?   Will the continent melt or
> will the extra water vapor mean more ice there? Will the southern ozone
> hole fill?  (It is big because it is so cold).
> https://www.youtube.com/watch?v=IfSJigmL8kI
>
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