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One easy way is to find out the temp at the field you are at. Take the
standard sea level temp of 15C and using the altitude of where you are at, subtract 2C for every thousand feet. For every 1 degree above standard, add 120 feet, or 600 feet for every 5C. Add that to the field altitude. Gives you a great ballpark idea in no time. Example: 3,000 foot field at 20C 15C - (3 x 2) = 9C (should be standard temp for that altitude) 20C - 9C = 11 11 x 120 = 1320 3000 + 1320 = 4320 density altitude On Tue, 15 Jun 2004 18:21:34 -0700, The OTHER Kevin in San Diego skiddz *AT* adelphia *DOT* net wrote: Anyone got a "formula" for figuring out pressure and density altitudes quickly and reasonably accurately, specifically if the knowns are Field Elevation Barometric Pressure in inches of mercury Temperature in degress Celsius. My instructor went over this for quite a while in ground school last night, but went about it in such a way we all pretty much got lost halfway through it. I thought perusing my 3 pages of notes would shed some light on it, but my results aren't "meshing" with the D.A charts in my P.O H - they're quite a bit off as a matter of fact. I've called 3 of my fellow classmates and they're just as confused as I am. A nice easy way to figure it out would be appreciated and maybe a condensed explanation as well. I've got a pile of textbooks to peruse for more details.. Thx! |
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