Saturday, June 14, 2014

Reversing Global Warming, part one






People are always talking about the weather, but I am proposing that we do something about it. This is the first of three (or maybe more) posts about reducing reversing global warming.

People have been talking and writing about global warming since they stopped talking about the next ice age; that was around 1980. SO far it has all be words. It climate scientists are so sure that human activity has been causing a rise in temperatures, then we should correct the damage before it will be too late.

According to the climate scientists atmospheric CO2 is the thing that has caused rising temperatures, so we should bring the CO2 down to pre-industrial levels, and one method for doing that has been known since back when climate scientists were talking about the new ice age that was about to start. There were articles about how cooling started, and one of the theories was that seeding the oceans with iron would cause plankton blooms that would soak up CO2, and shrimp and other small animals would eat the plankton and multiply, thus exhaling CO2, so there would be no net change in the amount of atmospheric CO2, except for that carbon that would fall to the bottom of the ocean when the predators defecated. More recently it has been theorized that iron rich dust blown from deserts blowing into the oceans led to ice ages during the last four million years. (See link below)

People have, as the linked article states, tested part of this by spreading iron dust on the ocean. That has resulted in plankton blooms, as one would expect. But no one has dumped in enough iron to change the atmosphere at all. If the theory is correct, then a billion tons of iron dust would be enough to remove a substantial amount of CO2 from the atmosphere.

Even though a billion tons may seem like an amazingly large amount of iron, it isn’t all that much. Consider that a 10x10 steel I-beam weighs about fifty pounds per linear foot, so a billion pounds would translate to twenty million linear feet of bean, and if we cut the beam into forty foot sections, then there only be five hundred thousand beams, or the amount in a small city.

The iron would have to be ground rather finely. Single celled animals would have to eat the dust, and it would have to be light enough that it could float on a breeze. For that reason the iron would have to be ground to that small size. It wouldn’t make much difference whether the iron were pure or oxidized, so we could grind up ore very finely and use that, rather than wasting refined metal. There would be extraneous material in the ground ore, but that wouldn’t hurt, and it might help. U.S. production of iron ore is about two billion metric tons annually, so a twenty-five percent increase for two years would produce all of the iron dust we would need. If that schedule became a problem, then we could stretch production over another year or two. And, if it turned out that applications of iron dust would have to continue, it could become a permanent industry.

The actual schedule would have to be determined by experiments that have not yet been done that would show whether continued applications of iron dust were necessary and whether the applications would be continuous or periodic. Pouring on too much might just result in the extra sinking to the ocean bed.

Another thing that we don’t know is whether the iron dust causing a phytoplankton bloom causing a drop in CO2 levels would have immediate effects. As we can see from last fifteen years increases in CO2 do not cause immediate temperature rises, and the same may be true of decreases on CO2 levels. We also do not know whether the increase in animals that would eat the phytoplankton would have any effect.

It might be wise to regard the first ten years of applying iron dust to the ocean as an experiment to see whether it would be effective. An alternative theory about atmospheric CO2 and climate is that the CO2 is an effect of increasing temperatures, rather than a cause. I won’t argue this position, because we should be planning to test the theory.




I’ll present another method next time.

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