Volcanos and Climate Geoengineering

The first thing that occurred to me when I heard about the Sarychev eruption was whether it was going to be large enough to inject significant quantities of sulphate aerosol into the stratosphere. Apparently, it is.

Sarychev Eruption Generates Large Cloud of Sulfur Dioxide

When sulfur dioxide reacts with water vapor, it creates sulfate ions (the precursors to sulfuric acid), which are very reflective. Powerful volcanic eruptions can inject sulfate aerosols into the stratosphere, beyond the reach of cleansing rainfall. At these altitudes, the sulfates can linger for months or years, cooling the climate by reflecting incoming sunlight. (The effect is stronger when the eruptions occur at tropical latitudes.) Carn says the persistence of such high concentrations of sulfur dioxide in the OMI data throughout the week indicates that the plume from Sarychev Peak reached high altitudes. Data from other satellites (such as CALIPSO) suggest that the volcanic plume reached altitudes of 10–15 kilometers, and perhaps as high as 21 kilometers.

In 1991, the eruption of Mount Pinatubo in the Philippines injected enough sulphate into the atmosphere to cause a 0.5° C drop in global temperature. This was caused by about 20 million tonnes of SO2. We are nowhere close to these kind of emission levels. After all, Pinatubo was one of the two biggest volcanic events of the century.

Injecting sulphate particles into the stratosphere has been proposed for a while now, I first wrote about it in 2006 when a prominent atmospheric chemist, Paul Crutzen wrote an article proposing this. The science behind this proposal is basic, sulphate aerosols of the size that would be formed from the oxidation of SO2 are the right size to scatter and reflect solar radiation back into space (my Masters thesis did a first order estimate of this effect from Indian emissions!). If injected directly into the stratosphere, they can stay there for a long time and will not deposit to the the Earth’s surface as acid rain. The issue is managing all the crazy regional variations in climate that would result, and the attendant complications in assigning blame, etc. It would also not help the oceans, which would acidify to hell with all the CO2.

Anyway, so much for that, the volcano is causing all kinds of havoc with Pacific travel and making for all kinds of cool pictures, which are about the most interesting thing happening at this point in time. We shall see how the sulphate situation plays out in the days to come when the dust settles.

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    funky MathES&T Online News: Can drugs found in water harm humans?

    Researchers agree that aquatic species face the greatest risk from exposure to low levels of pharmaceuticals, such as synthetic hormones, which can act as endocrine disrupters at environmental levels. However, little is known about the potential human health effects arising from complex drug mixtures.

    Well, it is often more difficult to analyze complex mixtures because Experimental Design 101 makes you want to isolate the effects. And when you do compounds one by one in series, the tendency is to always add them up from the individual experiments. Unfortunately, body chemistry is not like that. I’ve always wanted to design a study that started complex and then tried to isolate later.

    To his surprise, Pomati observed that this mixture of drugs at environmental levels inhibited the growth of human embryonic kidney cells. After 48 hours of exposure, cell proliferation was reduced by 10–30% compared with controls. However, no inhibition was observed when cells were exposed to only the toxic cancer drug at environmental levels.

    Well, that seems conclusive enough, but here comes the “Experimental Design 101” Scold:

    The results show that the growth inhibition is not due to the single most cytotoxic compound alone. But that does not conclusively prove that synergistic or additive effects exist between drugs in the mixture, cautions Thomas Heberer of the Institute of Food Chemistry at the Technical University of Berlin. To show that the individual drugs behave additively, Heberer suggests that researchers should analyze the effects of compounds with a common mode of action, such as antibiotics, alone and in various mixtures.

    No, No, and No. Doing this presupposes that you know that mechanism of action, meaning you’ve half answered your question. The question Heberer is trying to answer is “do individual drugs with the same mode of action behave additively”. The question Pomati is trying to answer is “Can we demonstrate cytotoxic effects of a cocktail of drugs at ambient levels in a laboratory setting”? These are two completely different questions and Pomati’s question is more valuable at this point in time. Heberer’s strategy, on the other hand, will keep a lab well funded for years to come! But, it is very much the final step.

    It is more important at this point in time to demonstrate other effects such as endocrine disruption, mutagenicity, etc in the lab at environmentally relevant levels of mixtures. Then we can get a better handle on which  effects are relevant and which ones to ignore.

  • Tar Sands Don't Fit in the Clean Energy Economy

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    Tell President Obama that he needs to stay on course to a clean energy future.

    via Obama2Canada

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    Once again, I will say that the future of the Oil Sands is not in Canadian hands, but in American hands. No Canadian government will turn off the tap, not now in this recession, not 3 years from now when we are on our next boom. It is going to take American pressure and the institution of a robust climate change mitigation program in the US. We shall see what happens in 2-3 years time.

    I do not believe this campaign will make any difference whatsoever, Obama is in Canada for something like 3 hours, and presumably will have other things to talk about.

  • NASA chief not worried about climate

    Ladies and gentlemen, I give you the chief of NASA, Michael Griffin

    NASA chief not worried about climate – Yahoo! News

    I guess I would ask which human beings, where and when, are to be accorded the privilege of deciding that this particular climate that we have right here today, right now, is the best climate for all other human beings. I think that’s a rather arrogant position for people to take,” Griffin said.

    Nothing more to say other than if I were American, I would first be a little ashamed, I would then start demanding his resignation. This is the chief of one of this country’s premier scientific institutions, one that does a lot of weather and climate research, one that employs the world’s foremost scientific voice on global warming. Here’s what Hansen had to say…

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    GE – we bring good things to life (and kill them with Diesel exhaust).

    Clean Air Watch – Blog for Clean Air

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    I have nothing to say, just another example of the plutocracy-protectionary principle, nothing new, same old Modus Operandi.

  • Combating Global Warming with Frankensulfates

    I don’t quite know how to react.

    Chemical & Engineering News: Latest News – Support Voiced For Geo-Engineering Research To Combat Global Warming

    The call to at least consider audacious geo-engineering steps that would fill the stratosphere with globe-cooling aerosols to check global warming got louder last week. In Science, Tom M. L. Wigley of the National Center for Atmospheric Research, in Boulder, Colo., writes that reducing carbon dioxide emissions is the long-term solution to global warming but that nearer term engineering of the atmosphere might provide “additional time to address the economic and technological challenges faced by a mitigation-only approach” (DOI: 10.1126/science.1131728). Last month, Nobelist Paul J. Crutzen of the Max Planck Institute for Chemistry, in Mainz, Germany, made headlines with an essay in the journal Climatic Change calling for more research into the pros and cons of injecting sulfate-based aerosols into the stratosphere as a sunlight-reflecting, cooling foil to global warming (C&EN, Aug. 7, page 19).

    The paper is still not out for public consumption, because “YOUR INSTITUTIONAL SUBSCRIPTION DOES NOT INCLUDE THIS ITEM:” (How an organization that is funded wholly by government (taxpayer) money can publish in journals that make you pay to read their contents is the subject of a different rant). Nevertheless, this modeling effort builds on Crutzen’s earlier essay which I just finished reading.

    Sulfate particles reflect incoming solar radiation, reducing the amount of light incident on earth and lowering the average temperature. This has been known for years, and I am sure every aerosol scientist has thought “Well, if there was some way of putting particles in the atmosphere to reflect more light, this whole global warming thing would just go away”. But the obvious issue with this approach is that sulfates in the troposphere are nasty, they cause acid rain, haze, increased mortality, etc. Crutzen expands on this further.

    The great advantage of placing reflective particles in the stratosphere is their long residence time of about 1–2 years, compared to a week in the troposphere. Thus, much less sulfur, only a few percent, would be required in the stratosphere to achieve similar cooling as the tropospheric sulfate aerosol (e.g., Dickinson, 1996; Schneider, 1996; NAS, 1992; Stern, 2005). This would make it possible to reduce air pollution near the ground, improve ecological conditions and reduce the concomitant climate warming. The main issue with the albedo modification method is whether it is environmentally safe, without significant side effects

    Which I guess is the key question, let alone the practicalities of introducing and maintaining 5.3 Tg (terra grams or million metric tonnes) of sulfur in the stratosphere successfully. This is a 10% increase from the current emissions of 55 Tg/year, so I guess it is not a terribly large number. Crutzen estimates that it will cost 25-30 billion dollars per year to have a loading of 1-2 Tg (to combat the most optimistic global warming scenario), though he cites a personal communication with someone at the National Academy of Sciences in 1992. This number is bogus, how do you know what something will cost if you don’t know how you’re going to do it? Crutzen has some ideas…

    Locally, the stratospheric albedo modification scheme, even when conducted at remote tropical island sites or from ships, would be a messy operation. An alternative may be to release a S-containing gas at the earth’s surface, or better from balloons, in the tropical stratosphere

    In other words, speculation at this point in time. The bottom line is this, the idea is not revolutionary, heck, even I thought of this in the mid 90s when I was doing sulfate aerosol work. The mechanics of how this will be done without causing some unforeseen other major issue is the real question that will take years to answer. Meanwhile, this silly personal virtue called conservation still works, look at this graph (from an NY Times article through the Washington Monthly), if Cali can do it, so can you.

    blog_california_electricity_usage.gif

  • California takes coals out of the fire

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    This is important because California is a huge market and is imposing its market power wisely. It will buy coal power if sequestration actually works.

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