Tau.Neutrino said:
With cleaner air higher up what is the average height of human caused pollution?
Goes searching, there’s not much about particle matter vs height in air….
PM2.5 particles in the air
https://www.epa.vic.gov.au/for-community/environmental-information/air-quality/pm25-particles-in-the-air
Ambient (outdoor) air pollution
https://www.who.int/news-room/fact-sheets/detail/ambient-(outdoor)-air-quality-and-health
Particulate Matter (PM) Basics
https://www.epa.gov/pm-pollution/particulate-matter-pm-basics
Particulate air pollution is the single greatest threat to human health globally.
https://aqli.epic.uchicago.edu/pollution-facts/
> You could always go as high as the ozone layer.
Yes.
As part of my work in CSIRO, I’ve done some work on the penetration of pollution up into the atmosphere, as well as mechanisms by which pollution is removed from the atmosphere.
I’ll start by debunking “inversion layer”. This is a relatively rare phenomenon that forms on only some locations for some periods of time. It occurs when a layer of stable air sits over the top of some neutrally stable (slightly turbulent) air. Pollution rises much more rapidly through the turbulent air than through the stable air, which under rare conditions traps pollution at lower levels causing severe pollution problems for some cities. But it’s temporary, lasting two to three weeks at worst.
Next step from that is to introduce you to the concept of the troposphere. The troposphere starts at the Earth’s surface and extends 8 to 14.5 kilometers high. The concentration of pollution decreases exponentially with distance up in the troposphere. With the lightest gases, including hydrogen and methane, the concentration increrases with height through the troposphere. With heavier gases such as CO2 and CFCs, the concentration decreases only very slowly with height. With the smallest aeroisols, soot from combustion, very little reaches to the top of the troposphere. For larger aerosols they don’t get to the top unless …
Once a pollutant manages to get itself injected into the stratosphere, it sometimes stays there a long time, but sometimes not. Injection methods include atomic bombs and volcanoes. Aerosols settle out.
… a key feature, one could even say a defining feature, of the stratosphere is the presence of cosmic rays from the Sun. These cosmic rays break down atmospheric pollutants at different rates.
To be continued (and to include the difference between washout and rainout).