NavList:
A Community Devoted to the Preservation and Practice of Celestial Navigation and Other Methods of Traditional Wayfinding
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From: Fred Hebard
Date: 2003 May 2, 21:47 -0400
From: Fred Hebard
Date: 2003 May 2, 21:47 -0400
According to the Smithsonian Meteorological Tables, one atmosphere is defined as 1013.250 mb, which the Nautical Almanac approximates as 1010 mb. One atmosphere corresponds to about 29.92 inches of mercury depending upon the local force of gravity. Reducing this by the factor of 0.9264 quoted by Paul Hirose as appropriate for 2100' elevation yields a standard pressure at 2100' elevation of 27.72 inches of Hg. I approximated these values as 30" Hg = one atmosphere and subtract 2 inches for 2100' elevation, which are fairly easy to remember; the approximation could be refined for the actual pressure obtained from the newspaper, tv or internet (drill down from http://iwin.nws.noaa.gov/iwin/graphicsversion/rbigmain.html into the political map of the U.S. to one state, and then to one station to find hourly reports of pressure and temperature). The approximation might yield a correction from the bottom of Table A4 correct (compared to George Huxtable's exact treatment) to within 0.1', perhaps 0.2' of arc. At one point in this quest I purchased the Smithsonian Meteorological Tables to try to compute some of the values, but it would take more study than I have time, patience and skill in physics (thank goodness that George is with us!). Mostly I was interested in determining the appropriate temperature to use, as the formulas employ the mean temperature of the air column. I note from page 389 of the Smithsonian Tables that refraction is also dependent upon the humidity of the air. This has not been factored into the corrections, perhaps because the mean humidity of the air column above a ship could not be determined accurately close to the sea. I am tempted to try to estimate the magnitude of the effect. It may be one of the factors causing discrepancies in Doug's observations. I am sure this was all well determined by the astronomers before 1850. We are treading into astronomy here, although this does lead back to my quest of checking the calibration of sextants, which service appears to be unavailable commercially in the United States. Fred