
NavList:
A Community Devoted to the Preservation and Practice of Celestial Navigation and Other Methods of Traditional Wayfinding
Re: sextant index error measurement
From: George Huxtable
Date: 2006 Nov 5, 10:27 -0000
From: George Huxtable
Date: 2006 Nov 5, 10:27 -0000
Jim wrote-| | It still concerns me that although you have compensated for | parallax,the effect of refraction when using the horizon would need to | be considered.The comment that the tables allow for this,in my opinion | applies only to the object.It seems to me that adjusting the sextant to | the horizon would allow for this error.In the past I have adjusted my | sextant to a nearby roof line and then taken it to the beach and found | that the true and reflected horizons were not inline. Well, the discrepancy, between making a zero-check against a nearby roofline, compared with using a horizon, is the effect of sextant parallax, nothing to do with refraction. If a sextant has an offset between the sightlines of 2 inches, and the roof was 100 yards away, the error, compared with lining it up on a distant horizon, would be nearly 2 arc-minutes, so it would be very noticeable, and any observations which used that as an index-zero would be badly out.. When you check index error with a horizon, it's true that the direction of the horizon is displaced, due to refraction, but that displacement is almost exactly the same for the direct view through the horizon mirror, as it is for the reflected view through the index mirror, from a point only a couple of inches higher up. So that any refraction has a quite negligible effect on such error checking. For that purpose dip tables are irrelevant. However, when you use the horizon line for a quite different purpose, for a horizontal reference when measuring an altitude, then any refraction of light, in its path from the distant sea-surface to the observer's eye, must be taken into account, as precisely as possible. This is done in the dip tables, which allow for two separate sources of dip. One is geometrical, due to the curvature of the Earth, and is exactly predictable. The other ir refraction, for which standard atmospheric conditions are assumed. However, if the vertical air-temperature gradient near the sea surface differs significantly from its assumed value, unexpected values of dip (know as "anomalous dip") can result, which give rise to unknown errors in the resulting altitude. If I have misunderstood what Jim is getting at, I hope he will put me right. George. contact George Huxtable at george@huxtable.u-net.com or at +44 1865 820222 (from UK, 01865 820222) or at 1 Sandy Lane, Southmoor, Abingdon, Oxon OX13 5HX, UK. --~--~---------~--~----~------------~-------~--~----~ To post to this group, send email to NavList@fer3.com To unsubscribe, send email to NavList-unsubscribe@fer3.com -~----------~----~----~----~------~----~------~--~---