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paulHarkonen t1_ja0f231 wrote

That's fair, I'm more familiar with tracking things that have more local sources/sinks (which arguably CO2 has as well at the surface) which is why I noted that while all constituents have local variation it may not be very large in the case of CO2.

I appreciate the clarification though. I should really go look into some of the datasets and see how much surface variation you actually get when not intentionally chasing sources/sinks.

The fog bank example was intended to highlight how distinct different atmospheric "chunks" can be, not necessarily that the CO2 content would change. But again, the clarification is worthwhile here.

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CrustalTrudger t1_ja0iu29 wrote

The idea that there are remote areas where even the lower troposphere is sufficiently well mixed enough that sampling in one location represents a reasonable approximation of a global average is the whole concept behind the Mauna Loa Observatory and Keeling Curve.

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paulHarkonen t1_ja0wg8r wrote

Oooooh, I see what you're saying. You can find sample points that are sufficiently far from sources/sinks that your local measurements are (essentially) just measuring the aggregate of the troposphere.

That's different from saying that a local measurement at an arbitrary location is representative. Ok, I'm onboard now that I understand what you're saying. I was just commenting that local measurements are not necessarily reflective of larger scale measurements (which it sounds like is accurate with the exception of a few selective spots where the local readings happen to be better reflections of the average).

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