NavList:
A Community Devoted to the Preservation and Practice of Celestial Navigation and Other Methods of Traditional Wayfinding
Re: Lunar Distances with Alex's SNO-T
From: Bill B
Date: 2006 Oct 31, 16:35 -0400
From: Bill B
Date: 2006 Oct 31, 16:35 -0400
Alex I have a topo map for our area. My apartment is just about 705 feet above sea level. Yours should be close, perhaps a bit lower. The Wabash river in is approx. 520 ft in Lafayette/West Lafayette. Will look up your place if you wish. According to USA Today: http://www.usatoday.com/weather/resources/askjack/wfaqpres.htm "The pressure reported for Denver, or any official observation station for that matter, is not the actual pressure on the surface, but rather is the pressure corrected to sea level. The reason this is done is so that meaningful maps of constant pressure lines, called isobars, can be drawn for stations across the USA. These maps are useful for picking out areas of relative high and low pressure. If pressure readings were not corrected, places like Denver would almost always have lower pressure than spots at lower elevations. Essentially, the map would reflect topography, rather than weather systems in the atmosphere." A while back Frank, if I recall, gave a method for converting the broadcast barometric pressure to local station pressure. On a calculator divide your altitude above see level by -32000 (maybe -34000?). Then hit (on my TI-30XA) 2nd then LN. (You are looking for e^x, the mathematically inclined can say it better, but that's the cookbook method). Multiply the broadcast pressure by the above result to get local (station) pressure. I use it with inches Hg, so not sure if it also works in millibars, but don't see why it would not. Perhaps Frank can clear up my fuzzy memory. There is some interesting information a well as a formula at: http://en.wikipedia.org/wiki/Atmospheric_pressure Bill --~--~---------~--~----~------------~-------~--~----~ To post to this group, send email to NavList@fer3.com To , send email to NavList-@fer3.com -~----------~----~----~----~------~----~------~--~---