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I finally understand methane lifetimes

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Re: I finally understand methane lifetimes

#71
post #8

So, hydroxide radicals (OH) break down methane (CH4) into carbon dioxide (CO2). This is a good thing for the climate, as a molecule of methane has a much bigger warming effect than CO2. (Although it is odd that the CO2 produced by methane is not counted toward methane’s overall climate impact). There is limited OH in the atmosphere. As a result, more methane “uses up” the OH. That means that increased methane in the…

The short lifespan of an OH radical isn’t an issue if it’s deployed at the site of emission (à la scrubbers). You then don’t need them to last long enough to randomly bump into methane particles in the wild as you’re inducing them in a high-methane concentration environment where you expect them to react before they react with something else and break down. That’s the moral of the story for all climate control: don’t…

I remember someone pointing out that (1) there is a very large amount of advocacy based around going to the Great Pacific Garbage Patch and harvesting microplastic particles there; and (2) this is a colossally stupid idea, because there is almost no plastic in the Great Pacific Garbage Patch. It's a a part of the ocean where the level of plastic is higher than usual. But it's still a part of the ocean.

If you want to filter plastic out of the ocean, you want to filter it out of the input stream, where it's concentrated, not out of the end product of diluting the input stream with the entire ocean.

Interestingly, the wikipedia article on the Patch is headlined by a disclaiming of a very similar mistake:

> Despite the common public perception of the patch existing as giant islands of floating garbage, its low density (4 particles per cubic metre (3.1/cu yd)) prevents detection by satellite imagery, or even by casual boaters or divers in the area.

https://en.wikipedia.org/wiki/Great_Pacific_garbage_patch

Re: I finally understand methane lifetimes

#72

Earlier quoted context omitted.

I don't think it's that complicated. Start with water vapor - moisture evaporates from the ocean, lakes, soil, vegetation. On average such a water molecule stays in the atmosphere for 4-10 days - because water condenses as rain, unlike methane or carbon dioxide. Water vapor increase accounts for about 2/3 of the immediate global warming effect, but is controlled by temperature, which is in turn controlled by the CO2…

>I don't think it's that complicated The complicated part that I have spent many hours trying to understand is how more CO2 increases the greenhouse effect if the the frequencies it absorbs are already 100% absorbed. If current CO2 PPM absorbs 100% of the IR it can interact with, why does X+1 PPM have positive forcing? The feedback loop is already maxed out? If I shine a flashlight at a concrete wall, it doesn't matt…

> The complicated part that I have spent many hours trying to understand is how more CO2 increases the greenhouse effect if the the frequencies it absorbs are already 100% absorbed.

I'm curious where you're getting the figure that the relevant frequencies are 100% absorbed, I didn't think it was that high, but I'm far from an expert on this. I don't think you can ever get to 100%, just arbitrarily close -- there's always the chance that a given photon will get lucky and escape without hitting any CO2 molecule.

But I think that if every IR molecule that was radiated from earth hit a CO2 molecule, what would happen after that first absorption would matter. The photon would get re-radiated with an equal chance to go in any direction. If it goes up, great, it escapes into space -- but the more CO2, the more of a chance that it gets absorbed again and re-radiated back down.

So it's not a concrete wall, it's like a field of gopher holes with gophers that will take any golf ball that falls into their hole and chuck it out randomly. Even if the field is dense enough that you can't roll a golf ball directly across it without going into at least one hole, if you increase the density of gopher holes more, it still lowers the chance that the ball will make it to the other side.

*edit - This article[1] I just found goes more into the math, it helped clarify it a bit for me.

[1] https://www.geoexpro.com/articles/2022/04/recent-advances-in...

Re: I finally understand methane lifetimes

#73
post #34

Earlier quoted context omitted.

what could possibly go wrong? Let's put iron chloride where it doesn't belong, outside of our control. Haven't we done enough harm yet?

you could say the same about anything. Installing solar or wind power isn't natural part of the environment, and "something" could go wrong, better not do that either.

I think that falls within his qualifier as “under our control”… and also previously tested. I have no dog in the fight, but be honest about what the argument really is.

Re: I finally understand methane lifetimes

#74
post #51

Earlier quoted context omitted.

You forgot the albedo effect of the clouds. On both sides - top and bottom. This has not ever been modelled to my knowledge. And it is very complicated.

Albedo is included in every single atmospheric model.

Cloud albedo? Its effects depending on surface temps? Cloud cover changes wrt local climate change?

Do you have any sources for that?

Re: I finally understand methane lifetimes

#75
post #8

So, hydroxide radicals (OH) break down methane (CH4) into carbon dioxide (CO2). This is a good thing for the climate, as a molecule of methane has a much bigger warming effect than CO2. (Although it is odd that the CO2 produced by methane is not counted toward methane’s overall climate impact). There is limited OH in the atmosphere. As a result, more methane “uses up” the OH. That means that increased methane in the…

Is there a connection between ozone and hydroxyl?

http://en.wikipedia.org/wiki/Ozone

"Ozone reacts directly with some hydrocarbons such as aldehydes and thus begins their removal from the air, but the products are themselves key components of smog. Ozone photolysis by UV light leads to production of the hydroxyl radical HO• and this plays a part in the removal of hydrocarbons from the air, but is also the first step in the creation of components of smog such as peroxyacyl nitrates, which can be powerful eye irritants. The atmospheric lifetime of tropospheric ozone is about 22 days; its main removal mechanisms are being deposited to the ground, the above-mentioned reaction giving HO•, and by reactions with OH and the peroxy radical HO2•."

Making more ozone is quite easy: take a UV-C disinfection lamp as used for an aquarium, and pump air through it.

At some concentration, the ozone itself could be hazardous, and it would be messy to clean up the soot from the smog as it falls.

I do wonder whether a little more surface ozone might help to make more hydroxyl to speed up the cleanup effort, especially if paired with a HEPA filter.

Re: I finally understand methane lifetimes

#76

Earlier quoted context omitted.

>I don't think it's that complicated The complicated part that I have spent many hours trying to understand is how more CO2 increases the greenhouse effect if the the frequencies it absorbs are already 100% absorbed. If current CO2 PPM absorbs 100% of the IR it can interact with, why does X+1 PPM have positive forcing? The feedback loop is already maxed out? If I shine a flashlight at a concrete wall, it doesn't matt…

> The complicated part that I have spent many hours trying to understand is how more CO2 increases the greenhouse effect if the the frequencies it absorbs are already 100% absorbed. I'm curious where you're getting the figure that the relevant frequencies are 100% absorbed, I didn't think it was that high, but I'm far from an expert on this. I don't think you can ever get to 100%, just arbitrarily close -- there's al…

>I'm curious where you're getting the figure that the relevant frequencies are 100% absorbed, I didn't think it was that high, but I'm far from an expert on this.

Last time I researched this I saw various estimates that IR in the CO2 absorptions bands only makes it 10-25 meters before it 99% of it is absorbed by CO2. Your link gives and average distance of 2.6m for IR in the CO2 absorption band.

>Assume that [C]=400 ppm. The mean free path becomes 2.646m so that N=3024. The probability of returning to the Earth becomes p(1)=0.9997. A photon with frequency or wavenumber near the centre of the absorption band is virtually certain to make the return to Earth. If the CO2 concentration is doubled, the probability doesn’t change much; it becomes p(1)=0.9998. Any CO2 increase has minor effect on the photons in the center of the absorption band. This part of the band is ‘saturated’.

The website and other papers I have read seem to argue that it is not the majority of photons in the center of the emission and absorption band, but a much smaller number of off band photons in the "wings" that matter for the greenhouse effect. When I have tried to read about how this works, I get bogged down by the complexity of the science, and a lot of different arguments from the climate skeptic community which I don't have the foundational understanding to reject. They say that the shoulder theory is bunk because it ignores interactions between CO2 and other molecules. Instead of photons bouncing from CO2 to CO2, they say that the CO2 passes the energy off to nitrogen and oxygen.

I don't really give too much weight to the climate skeptic criticism, but I do have to acknowledge that greenhouse effect is a lot more complicated than taught in grade school and there is still a lot of active research using extremely simplified models trying to model how it works from first principles with a lot of exclusions and assumptions. like the paper cited in the link you shared from 2012.

Thank you for sharing the link, I will take some time to try to read and digest it.

Re: I finally understand methane lifetimes

#77

Earlier quoted context omitted.

you could say the same about anything. Installing solar or wind power isn't natural part of the environment, and "something" could go wrong, better not do that either.

I think that falls within his qualifier as “under our control”… and also previously tested. I have no dog in the fight, but be honest about what the argument really is.

I guess I don't understand the distinction. Why one is out of our control? Certainly we could stop injecting extra iron into the atmosphere just as easily and dismantling a solar plant.

It seems like a lot of people conflate "out of control" with "I don't understand it".

Re: I finally understand methane lifetimes

#78

Earlier quoted context omitted.

I don't think it's that complicated. Start with water vapor - moisture evaporates from the ocean, lakes, soil, vegetation. On average such a water molecule stays in the atmosphere for 4-10 days - because water condenses as rain, unlike methane or carbon dioxide. Water vapor increase accounts for about 2/3 of the immediate global warming effect, but is controlled by temperature, which is in turn controlled by the CO2…

>I don't think it's that complicated The complicated part that I have spent many hours trying to understand is how more CO2 increases the greenhouse effect if the the frequencies it absorbs are already 100% absorbed. If current CO2 PPM absorbs 100% of the IR it can interact with, why does X+1 PPM have positive forcing? The feedback loop is already maxed out? If I shine a flashlight at a concrete wall, it doesn't matt…

So that question was addressed in the 1950s I believe by one Gilbert Plass who was initially involved in getting data for infrared guidance systems for air-to-air rockets (homing in on jet engines). The simple answer is that those frequencies are not saturated at altitude, i.e. 12 km up or so. Hence this is where CO2 exerts most of its effect. For a full discussion:

> "Plass pursued a thorough set of one-dimensional computations, taking into account the structure of the absorption bands at all layers of the atmosphere. In 1956 he explained clearly, for the first time, that the water vapor absorption lines did not block the quite different CO2 absorption spectrum, adding that there was scarcely any water in the upper atmosphere anyway. He further explained that although some of the CO2 band itself was truly saturated, there were many lines to the side where adding more of the gas would increase the absorption of radiation. His arguments and calculations showed convincingly that adding or subtracting CO2 could seriously affect the radiation balance, layer by layer through the atmosphere, altering the temperature by a degree or more down to ground level."

https://history.aip.org/climate/Radmath.htm

Here's an additional bit of data that explains this rather oft-repeated old trope about CO2 saturation:

> "The early experiments that sent radiation through gases in a tube, measuring bands of the spectrum at sea-level pressure and temperature, had been misleading. The bands seen at sea level were actually made up of overlapping spectral lines, which in the primitive early instruments had been smeared out into broad bands. Improved physics theory and precise laboratory measurements in the 1940s and after encouraged a new way of looking at the absorption. Scientists were especially struck to find that at low pressure and temperature, each band resolved into a cluster of sharply defined lines, like a picket fence, with gaps between the lines where radiation would get through."

Re: I finally understand methane lifetimes

#79
post #44

Half lives are a poor term for this; you are really looking for reaction rates, which are dynamic systems. Methane doesn't just disappear, it reacts with something else. A radioactive isotope's decay is relatively self contained, so the half life terminology holds. A microgram or a kilogram of U-235 will decay at about the same rate, making half life a useful number. Methane reacts with OH, which is sourced from diff…

As someone whose academic background was in nuclear stuff (but ~10 years ago alas), I had fun read of this article for the considerations like "ohh, a 'half life' with multiple decay modes of varying weights depending on the environment, etc. Gives an itch to dive back into numbers wrangling/plotting!

I agree that an accurate description of the (atmospheric in this case) systems over time definitely needs reaction rates, but similar considerations are also needed with nuclear radiation in a lot of situations too: e.g. the overall uhh radioactivity (for lack of recollection of precise terms) is a function of the chain of decay products, which are also often radioactive. That is to say, you might start with half-lives in calculations for dose estimation as a function of time, but you quickly get into more complex things. Also in the nuclear realm, add sources, like a running reactor, or a fresh set of fuel rods, and you get some very interesting effects over time!

I think this article was a fair example walkthrough of how things quickly get more complex than the numbers (mis)quoted to the public. I was hoping it would go further, even.

Re: I finally understand methane lifetimes

#80

Earlier quoted context omitted.

In this case, I think people want to ban large-scale deployments of untested, unvalidated technologies with no definitive positive effect and a non-negligible probability of disastrous consequences. I myself am an atmospheric chemist and no one has banned me from doing scientic research.

Read their letter and paper. They don’t want to ban large scale deployments. They want to ban any deployments, even for small-scale research purposes. This will ensure that all unvalidated technologies remain untested. That’s unfortunate because we all know we can’t decarbonize in time. We need other braking mechanisms and we should be pretty open to experimentation. If no one is upset with your particular atmospheri…

"we all know we can’t decarbonize in time"

I guess you mean "we all know that almost no current government has the political courage to do what is necessary so that we decarbonize in time".

Or " we all know that we don't have the fortitude to do to do what is necessary so that we decarbonize in time". => that version is better if governments do what their public opinion is willing to do.

To fight in the WWI and WII, the most advanced economies of those times turned in less than two years into war economies, where more than 50% of the GDP was directed to the war effort.

True for Germany, France, the UK plus, for WWII, the USA, the USSR, Japan.

The Apollo program amounted during the 60s to 4% of the US GDP, just for the political sake of keeping up with the USSR.

If we considered - as we should - the dereliction of climate and the on-going massive reduction of biodiversity as an existential threat, we would act accordingly.

We can decarbonize in time. But we don't want to "look up", e.g. to listen to the Science.

Australia is having huge fires and large floods every year now - but still elect a government in denial of the causes.

In the USA, the natural disasters are rising sharply in frequency and magnitude (current drought in the West, hurricanes etc).

Etc etc.

When it will become unbearable, we will at last act accordingly. The solutions are there already.

There are many breakthroughs (batteries for example, to store surplus of renewables energies so that it can be used at will when necessary). Far many more would occur if we invested money in research and R&D.

We ought not to bet on a hypothetical magic bullet. Not that we shouldn't fund those research. Startups with small odds to succeeded easily raise VC money since a success would offer a huge ROI.

But the trap is to bet the future of the world on a hypothetical magic bullet when the solutions already exist. We just don't want to do what necessary to implement them.

The USA, Canada, Australia for example emit 3 times more CO2 than France per inhabitant. However, the loss of biodiversity is as fast (and maybe higher) in France (which governments do very little to tackle gashouse emissions).

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