About this "beyond nonsensical" idea:

I was just commenting a post which dealt with angular momentum and which 
proposed to use kite devices. About this point, I only added the adjective 
"strong". About ships, their being submitted to storm winds isn't, indeed, 
necessary for my idea: submarines could do the job as well. And they could more 
easily move between inside the hurricane's eye - where the surface winds are 
weaker - and outside the whole hurricane - where the crew could safely join the 
rest of the world. Reversed propellers and other hydrodynamic brakes, in order 
to exchange angular momentum, could be fitted to submarines as well as to ships.

Their "strength" and the kites' one is a matter of design, but mainly of size 
and finally of materials quantities. I do not pretend that I have done the 
least beginning of an economic appraisal, but if anyone was willing to, it 
would be a good thing.

Best,

Denis.
De : David Schnare [mailto:[email protected]]
Envoyé : jeudi 11 juin 2009 13:09
À : Bonnelle Denis
Cc : [email protected]; geoengineering; [email protected]
Objet : Re: [geo] Re: Just in Time for Hurricane Season

For those of us who have been on a ship, on the ocean and near a hurricane, 
much less under it, the idea of having any ship, much less many of them, flying 
kites and reversing engines in some kind of large circle is beyond nonsensical. 
 It's sort of like having the government control GM - might sound like a good 
idea, but really!

d
On Thu, Jun 11, 2009 at 5:59 AM, Bonnelle Denis 
<[email protected]<mailto:[email protected]>> wrote:

This analysis is interesting, but I'd split the first sentence in three parts: 
"To have harmful wind speeds, a hurricane needs to have a large underpressure 
air column in its middle, and this underpressure has to be protected by the 
centrifugal force, which results from a lot of angular momentum".

However, when these ideas are being translated to figures (numbers), an 
important parameter comes in : the radius. The centrifugal force effect is 
negligible at the beginning of the air path (when Coriolis's force builds the 
angular momentum up) and at the end of the same path. It is only in its middle, 
i.e. at a middle altitude (maybe from 1000 m to 8000 m) that this effect is 
maximum.

So, if you'd like to use some strong kites to create a drag, a useful device 
could be to have some boats along a circle in the hurricane's eye, being drawn 
by kites 1000 or 2000 m high, using their propellers as brakes (and even 
transmitting some mechanichal power to an electrical engine which would act as 
a power generator). This would transfer the hurricane's angular momentum - at 
the point where this momentum is most implicated in the hurricane's 
self-stability - to the sea, i.e. it would create an interesting angular drag.

Conversely, I am not very much convinced by angular momentum exchanges with the 
upper layer of the hurricane's air.

Best,

Denis Bonnelle
[email protected]<mailto:[email protected]>


-----Message d'origine-----
De : [email protected]<mailto:[email protected]> 
[mailto:[email protected]<mailto:[email protected]>]
 De la part de dsw_s
Envoyé : mercredi 10 juin 2009 10:55
À : geoengineering
Objet : [geo] Re: Just in Time for Hurricane Season


To have harmful wind speeds, a hurricane needs to have lots of angular
momentum.  If some of the angular momentum could be dispersed to
farther from the center of the storm, wind speeds would be lower.  If
I understand it right, a hurricane has air coming in from the
periphery at low altitude, rising in the middle, and dispersing at
higher altitude.  If the storm is remaining steady or strengthening
(in terms of the total angular momentum of its winds), the outgoing
air must have less angular momentum than the incoming air by an amount
at least equal to the angular momentum lost to drag at the surface.
Suppose we have something for drag suspended at an altitude where air
is moving inward, from balloons at an altitude where air is moving
outward.  That should transfer angular momentum from the inward-moving
air to the outward-moving air.

Alternatively, one could fly over the edges of the storm and drop long
ropes with a kite on one end and on the other end a weight of
approximately the same density of water.  The kites would fly
themselves for a while before being destroyed, creating drag and
decreasing the angular momentum of the air they came in contact with.
As the air moved in toward the center of the hurricane, the change in
wind speed would be multiplied according to conservation of momentum
just as the wind speed itself is.




--
David W. Schnare
Center for Environmental Stewardship

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