I just learned 'about 9.8' which is true anywhere in the world.

Standard gravity is 9.80665 m/s2. That the number defined by the metric people who set all the world's units. In schools in the united states of america, we used 9.8. I don't recal using any more precision than that. Gravity at the surface does vary, but you don't need more presision than that for most academic purposes.

This is why you have so many Russians being thrown out of windows in high buildings. They're testing the local value of g.

We learned 9.82 m/^2. But in the classes I have as an engineering student we use 10 m/s^2. And I wish I was kidding when I say it's because it easier to do the math in your head. Well obviously for safety critical stuff we use the current value for wherever the math problem is located at

Well, g is not a real constant, it depends mostly on altitude. The true constant is G. g=9.8 is usually more than enough for your calculations, to the point we often round it to 10 for simplicity, or you remove it completely is the mass is too low. But actual numbers is only the very last step usually. The calculations will be made with letters. The value you use at the end for g depends on the precision you need, so it depends on the precision of the other parameters.

I learned 9.81 m/s2 and 32.2 ft/s2 with the qualifier being at sea level.

In freshman college physics we had a lab to measure gravity then had to use our lab result for the rest of the course.

In grade school i learned it was about 32 ft/s2, but by high school on it was all 9.8[1/06] m/s2. Then in engineering school it was sometimes 10. None of that had anything to do with local gravity and everything to do with Americans having to be special at first, followed by the fact that our science classes are actually in metric (statics and dynamics were in both as some fields of engineering haven’t metricated yet here). And the 10 is because you can round to a round number by barely even touching your fudge factor so why not.

I also learned 9.8.

This reminds me of the story of magnetic detonators for torpedos they tried to use in the early days of WW2. They detect the slight disturbance in the Earth's magnetic field caused by a gigantic hunk of floating metal, and that triggers the detonation.

However, they did not yet know that the Earth's magnetic field is not consistent over the whole planet, so while they calibrated it to the local field, it functioned very badly in other regions with different field strengths. Torpedo would either detonate far too early, doing minimal damage, or not detonate at all, just hitting the target ship with a loud thunk.

This was largely responsible for the ineffectiveness of American submarines in the early days of our WW2 involvement. Took us a couple years to sort too.

It was called the Mk 42 in case anyone wanted to read a little more. It's an amusing story. They never wanted to actually properly test them, because they were so damn expensive. So they just didn't. lol It wasn't until enough sailors complained and got a high ranking admiral on their side that it got sorted.

People learned different values for g for a number of reasons, but as far as I understand local variability is not one of them. The primary root cause seems to be accuracy of the measurement over time and the age of textbooks/course material.

Over time we have gotten better at measuring the true value of g through advances in technology and this has caused the taught value to shift a little. The value when initially measured had fairly large error margins, meaning that we were sure it was near a specific value but not sure of the exact value. As the tools improved we have reduced the uncertainty, getting to a more accurate and also more precise value, meaning more digits after the decimal as well as higher confidence in each digit. We have also changed what we mean by g over time, bringing it in line with the metric system and basing it on fundamental values and constants. From my understanding the most recent method relies on how much the repulsive force of an electromagnet with a specific number of culombs passing through is overcome by gravity at a specific distance from the center of the mass of Earth, so a little more removed from backyard science than measuring if things drop at the same speed at the top of a mountain and sea level.

Part 2 is the differences in how recent your material is. In my primary school in a relatively affluent area of an affluent country we had textbooks from the last 10 years. My partner went to a school in the same country but a worse area about 5km away from mine. Their school had textbooks literally 20 years old. In that time the measurements had changed, understandings had changed, and they were therefore taught things that were untrue. These sorts of differences based on geography reproduce the impacts of racism and inequality from the past into the future.

I've learned it as 9.81 but we usually round up to 10 for calculations. (this is for highschool. I haven't gotten to college yet)

9.81 in Scotland.

Seeing as the British invented gravity, most places just use our gravity rather than making their own.

g = 9.80665 m/s^2 at sea level. Higher than sea level lowers the value due to GR (General Relativity).

While I don’t know the answer and that for simplicity it should probably be a global average, it is probably some “constant“ measured from some location in either Europe or North America before they were able to measure globally using satellites.

Wow, I also didn't know it varied so much. I assumed it would be within about 9.81+-0.01 worldwide, since I (in UK) was also taught ~=9.81m/s^2

we learned it was about 9.8. We actually measured what it was near our school, and I think it came out to 9.82. We were told it was ok to use either 9.8, 9.82 or 10 in exams.

See Wikipedia for this.

ITT: People who all apparently remembers what the freaking constant for gravity is down to the decimal.