swestrup: (Default)
swestrup ([personal profile] swestrup) wrote2007-08-07 11:04 pm

FYI

This, it turns out, is NOT the best weather to be wearing two pairs of socks, underwear, long underwear, jeans, a long-sleeved shirt, jeans jacket, winter coat, toque, snood, and two pairs of gloves, all zipped up as tight as possible and all seams covered with a layer or two of duct tape. Oh, and safety goggles.

I think I'll just go over here now and melt for a bit.

Edit: For those wondering WTF, see Taxlady's Post

[identity profile] sps.livejournal.com 2007-08-08 05:02 am (UTC)(link)
Well, but they do. Don't they?

[identity profile] sps.livejournal.com 2007-08-08 07:49 am (UTC)(link)
Really? The back of my envelope predicts that even for nicely shaped objects, they only have to fall for a few seconds before drag becomes a significant factor. If he can find a 150-200m cliff...? Or have I lost an order of magnitude somewhere?

[identity profile] sps.livejournal.com 2007-08-08 10:16 am (UTC)(link)
I thought drag was roughly (r^2)(v^3). In any case, the question is one of whether Aristotle had a good enough theory of atmosphere to abstract it away from his theory of falling. Absent that, it's slanderous to accuse him of being wrong if he folds drag into his theory, don't you think? My overall impression of the ancients is that they had good measurements, but weak theory.