Path: utzoo!utgpu!news-server.csri.toronto.edu!rpi!usc!cs.utexas.edu!uwm.edu!lll-winken!sun-barr!olivea!mintaka!ai-lab!ai.mit.edu!bleck From: bleck@ai.mit.edu (Olaf Bleck) Newsgroups: rec.skydiving Subject: Re: High altitude landings Message-ID: <15939@life.ai.mit.edu> Date: 16 May 91 05:11:37 GMT References: <13377@exodus.Eng.Sun.COM> Sender: news@ai.mit.edu Organization: MIT Artificial Intelligence Laboratory Lines: 38 In article <13377@exodus.Eng.Sun.COM>, brent@terra.Eng.Sun.COM (Brent Callaghan) writes: |> The only uncertainty is the landing. The DZ will |> be in the Rockies at 9,500 MSL. How much harder |> will the landing be than at sea level ? |> |> What's the increase in rate |> of descent and ground speed ? First order calculation: Assume steady state fall rate under canopy, so weight equal to force on canopy: W=Pressure*Area=0.5*density*velocity^2(squared)*area of canopy Weight is constant at both sea level and 9,500ft, as is area, so density1*velocity1^2 = density2*velocity2^2 => velocity2 = velocity1 * Square Root (density1/density2) Using standard atmosphere, density of air at sea level = 1.19 kg/m^3 density of air at 3000meters = 0.885kg/m^3 so, velocity(3000m) = 1.16*velocity(sea level) Not too bad. This is assuming I didn't miss some key point in my calculation by sleeping through class as an undergrad! Of course this is a much hairier aerodynamic problem than this calcualtion, but I suspect this will get you kind of close, and I'm not current enough to figure it out. Believe it or don't, -Olaf A-12241