>Consider that in the arctic, above 38 degrees north latitude, a
reduction of more than 1,134 Megawatts per square mile per day can be
achieved by replacing open seawater with a layer of snow-covered ice.

Megawatts per day?

On Aug 17, 9:45 pm, "Eugene I. Gordon" <euggor...@comcast.net> wrote:
> Peter:
>
> My dogs do not distinguish between spheres and circular plates; they will
> chase anything that I throw; they are all 'balls'.  I characterized the idea
> as silly but perhaps not as silly as might appear.
>
> Spray foam insulation in houses typically costs 90 cents pr square meter
> including installation. I would guess the large volume cost for spraying
> bursts of foam on the ocean by a ship to make round floating plates would be
> about 10 cents per square meter or $100 K per square kilometer or $100
> million for 1000 square kilometers on the ocean as say 1 square meter
> roughly circular pieces made by timed spray bursts. They would float freely
> and and remain on the surface and certainly reduce heat absorption even if
> they are covered by bird droppings, but in fact that might stay reasonably
> clean. They would be moved naturally out of the way of small and large boats
> and even if they break into pieces they would be effective in keeping
> sunlight from being absorbed by the water. Since they are insulating the
> effective surface reflectivity would be 100% even if they got dirty.
> Absorbed energy would be simply radiated away and not heat the water
> underneath unless it splashes over the warmed surface.
>
> If it indeed would cost no more than $100 million it would be a bargain if
> it made ice form by keeping the ocean water from heating.
>
> -gene
>
>   _____  
>
> From: Peter Read [mailto:pe...@read.org.nz] On Behalf Of Peter Read
> Sent: Monday, August 17, 2009 6:30 PM
> To: euggor...@comcast.net; terratw...@gmail.com;
> geoengineering@googlegroups.com
> Subject: Re: [geo] Re: atmospheric and oceanic warming
>
> Why balls when flat plates would do better? e.g. all the polystyrene packing
> material that gets junked, if it could be persuaded to stay white and if
> seals and polar bears could be persuaded not to eat it.  Or, if you get
> serious, what cost for 1000 sq Km of 2 cm thick polystyrene boards that
> would get embedded in the winter ice and maybe stop it melting through in
> the summer?
> Peter
>
> ----- Original Message -----
> From: Eugene I.  <mailto:euggor...@comcast.net> Gordon
> To: terratw...@gmail.com ; geoengineering@googlegroups.com
> Sent: Tuesday, August 18, 2009 4:21 AM
> Subject: [geo] Re: atmospheric and oceanic warming
>
> Thanks for your e-mail. There is a trivial typo; 97% should be 93%. If we
> could reverse the arctic ice melt it would go a long way toward reducing the
> rate of warming or even might achieve some cooling.
>
> In any case the earth is warming independent of manmade greenhouse gas and
> will continue to warm until the temperature reaches 25 C as it has done many
> times during the past 450 million years. That is an offline discussion thta
> we can have but the bottom line is that geoengineering is needed in any case
> with or without CO2 emissions and long term; reversing the artic ice melt
> may not be enough.
>
> My choice for reversing the ice melt would be to distribute SO2 over the
> Arctic only. It will slowly spread southward but the main cooling would be
> over the Arctic and that should allow more ice to form.
>
> Here is a silly idea. Form lightweight sunlight reflecting balls that can
> last for a few years and distribute them to float on the arctic ocean
> waters. That would certainly increase the solar reflectance and possibly
> allow ice to form trapping the balls in the ice. On open ocean they would
> not interfere with shipping, polar bears, etc.
>
> -gene
>
>   _____  
>
> From: geoengineering@googlegroups.com
> [mailto:geoengineer...@googlegroups.com] On Behalf Of Brian Abel
> Sent: Monday, August 17, 2009 12:50 AM
> To: geoengineering@googlegroups.com
> Subject: [geo] atmospheric and oceanic warming
>
> All,
>
> I would very much be interested in your opinion of a concept I have been
> exploring, but as to date I have yet to find similar proposals.  I would
> like to submit for your consideration a potentially effective approach to
> help globally manage some of the more concerning elements of atmospheric and
> oceanic warming.  Please feel free to respond with your harshest criticisms,
> any questions, and whatever supporting information you might have.  The idea
> is presented partially below, followed by a copy of some dialogue which will
> hopefully answer and help you ask the types of questions that a concept such
> as this might require.  Any modeling studies which you might be aware of
> evaluating oceanic heat rejection to arctic atmosphere, and/or arctic
> surface albedo adjustment would also be of tremendous interest to me.  
>
> Thank you.
>    -Brian M. Abel
>     <terratw...@gmail.com>
>
> Global Warming Initiative
>
> A conceptual approach to the problem of global warming
>
> As concern continues to mount over global warming and controversy rages over
> the role the "greenhouse" gases play in climate change, one thing is
> certain; the planet appears to be warming up at an alarming rate.  
>
> A great deal of consideration has been given to reducing greenhouse gas
> emissions as a means of slowing or reversing global warming.  However, until
> an alternative to carbon-based energy sources is found, reducing man-made
> CO2 emissions is little more than a pipe dream.  And even the most
> optimistic of proponents for greenhouse gas reductions acknowledge that it
> may take decades to reverse the global trend - if it is possible at all.
>
> We are now prepared to propose a conceptual alternative to the issue of
> global warming.
>
> Background:
>
> The Earth receives an enormous amount of solar radiation. Just above the
> atmosphere, the solar power flux density averages about 1367 watts/m2, or
> 1.28 * 1014 watts over the entire earth. This power is balanced over time by
> a roughly equal amount of power radiating from the earth. Ideally Energy In
> should equal Energy Out.  Various factors can influence this balance in one
> or the other direction, resulting in an atmospheric and/or planetary
> temperature change.
>
> We are convinced that an immediate and workable alternative to reducing
> greenhouse gases to reduce global warming lies in reducing the amount of
> heat captured and retained by the planet from solar energy.  This can be
> accomplished by changing the albedo (simply stated, reflectivity) of a
> portion of the planet's surface.  By reflecting more solar energy away from
> the planet, less heat is absorbed.  
>
> Albedo is defined in terms of a 0 - 1 scale with 0 representing total
> absorption of all of the incoming solar energy and 1 representing total
> reflection of all incoming solar energy.  Figure 1 shows the relative
> reflectivity of various planetary components as a percentage of the energy
> they reflect.  For example, fresh snow at roughly 84% reflects 84% of the
> incoming energy and would have an albedo of .84
>
> We propose a method of assisting a natural positive feedback cycle involving
> the polar ice caps.  Snow-covered arctic ice has an albedo of 0.8, meaning
> 80 percent of the received sunlight is reflected back to space.  By
> contrast, the albedo for sea water is around 0.07, meaning that only 7
> percent of the received sunlight is reflected.  Or, in other words, 97% of
> the solar energy goes into the seawater.
>
> A Growing Crisis:
>
> According to Worldwatch Institute; "the Earth's ice cover is melting in more
> places and at higher rates than at any time since record keeping began."
>
> As our planet's best reflector melts, more and more solar energy is being
> absorbed by the ocean, causing it to heat up even more -- which, of course,
> will trigger even further losses of ice. This in turn causes sea levels to
> rise, dilutes ocean water, disturbs normal currents, and impacts various
> marine and terrestrial life cycles.
>
> The Concept: "TerraTweaking"
>
> We approach the problem by asking the question "What would happen if a
> portion of the lost ice and snow cover could be restored?"  Suppose, by
> applying technologies well within mankind's grasp, significant areas could
> be given new ice and snow cover.  Would it be possible to locally raise the
> albedo of an area sufficiently to offset a portion of the temperature rise.
> Early indications suggest that the answer may be "yes".
>
> The concept of terraforming, the transformation of the atmosphere (or
> biosphere) of another planet into one having the characteristics of Earth,
> originated in science fiction but has, in recent years, found serious
> proponents within the technical community.  Although terraforming of another
> planet is currently well beyond the technical abilities of mankind, if for
> no other reason than the simple logistics of transporting supplies,
> equipment, personnel, etc. to an other planet, "terratweaking" of our own
> planet may well be within our grasp.
>
> Imagine a fleet of ships equipped with snow-making equipment capable of
> covering large areas of low-albedo ocean or bare land with a blanket of
> snow.  Consider that in the arctic, above 38 degrees north latitude, a
> reduction of more than 1,134 Megawatts per square mile per day can be
> achieved by replacing open seawater with a layer of snow-covered ice.  As
> more solar heat is reflected away from the area, less heat is absorbed by
> the seawater, allowing ice and snow cover to remain longer.  As more ice and
> snow is formed, salt is pushed into the ocean water below the ice where it
> sinks and thereby contributes to thermohaline circulation, natures global
> heat "conveyer belt".  This process is a positive feedback system which
> naturally seeks to be self perpetuating.  In the same manner, as snow and
> ice cover diminishes, the process can function as a negative feedback
> system.  By providing a small push ("tweak") in the right direction, we
> believe that it may be possible to retard or even reverse the current
> warming trend.
>
> Detailed Description:
>
> As seasonal new sea ice begins forming in polar regions, saltwater is
> distilled aboard an ocean-worthy vessel. Brine, a by-product of the
> distillation process, is discharged back
>
> ...
>
> read more »
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