Last June, WIRED magazine wrote an in depth article that asked:
Can a Million Tons of Sulfur Dioxide Combat Climate Change?
The question arose from research from research at Lawrence Livermore National Laboratory near San Francisco, by Lowell Wood, a protégé of the brilliant and controversial hydrogen bomb inventor Edward Teller. The idea was simple: Inject sulfur dioxide into the stratosphere to reflect a portion of the sun’s rays back into space, thus cooling the planet. It also seemed to be within the realm of possibility to some.
Here is how it works:

Graphic and text below adapted from Wired magazine article
1. Make sulfur dioxide
A million tons of sulfur dioxide would be needed to begin the cooling process. Luckily SO2, a byproduct of coal-burning power plants, is a common industrial chemical.
2. Inject it into the stratosphere
Load the sulfur dioxide into aircraft — converted 747s, military fighters, or even large balloons — and carry it up to the stratosphere. This will cost about $1 billion a year.
3. Wait for the chemical reaction
In a series of reactions, sulfur dioxide combines with other molecules in the atmosphere, ultimately forming sulfuric acid. This H2SO4 binds to water to form aerosol droplets that absorb and reflect back into space 1 to 3 percent of the sun’s rays. (The particles also contribute to the depletion of the ozone layer, but scientists are researching alternate chemicals.)
4. Let the planet cool
Results will be quick, especially over the Arctic.
And just a few days ago, over a million tons of sulfur dioxide (SO2) was in fact injected into the atmosphere over the Pacific Ocean, here is a satellite sounder derived image of the cloud that has been released:

Source: AVO
The Terra/MODIS satellite snapped a nice image of the release, notice the obvious brown trail as the plume becomes airborne over the Pacific ocean:
Source: NASA


The National Snow and Ice Data Center (NSIDC)’s troublesome ice graph
Ice at the Arctic: 2007 and 2008 snapshots
Overall long term trend remains positive in lower troposphere.















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