Editing Talk:852: Local g
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It affects more than sports. I work in calibration. A weight used for *force* measurements (10N, for example) has to be calibrated for local gravity - 1% change in local gravity vs 0.1% weight tolerance...[[Special:Contributions/108.162.219.154|108.162.219.154]] 15:39, 19 May 2017 (UTC) | It affects more than sports. I work in calibration. A weight used for *force* measurements (10N, for example) has to be calibrated for local gravity - 1% change in local gravity vs 0.1% weight tolerance...[[Special:Contributions/108.162.219.154|108.162.219.154]] 15:39, 19 May 2017 (UTC) | ||
β | The explanation usually given for Bob Beamon's 8.91 metre (29.75 ft) long jump at the 1968 Olympics is that the Mexico City air (at an altitude of 8000ft/2480m) was thinner. But sure, if you also want to credit as well something that needs special, high-calibration equipment and complex math to measure, go ahead. #### | + | The explanation usually given for Bob Beamon's 8.91 metre (29.75 ft) long jump at the 1968 Olympics is that the Mexico City air (at an altitude of 8000ft/2480m) was thinner. But sure, if you also want to credit as well something that needs special, high-calibration equipment and complex math to measure, go ahead. #### |
β | + | Is there an actual example where it would have made a difference in the Olympics? [[Special:Contributions/162.158.179.108|162.158.179.108]] 12:00, 23 July 2021 (UTC) |