1950
DOI: 10.1017/s037346330003486x
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Investigations into the Dip of the Horizon

Abstract: The dip of the horizon resulting from the observer's height of eye can be calculated from the formula Dip = 1′·06√H, where H is the height of eye in feet, or by Dip = 1′·93√h, where h is the height in metres. In this paper the latter form will be used so that comparison can be made with studies in international publications.

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Cited by 5 publications
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“…So the total width of this image depends on the height of the tallest irregularities on the surface: rocks and bushes on dry land, or the largest waves on water. The importance of the dip of the sea horizon for celestial navigation has produced a huge literature on this subject; e.g., [67][68][69][70][71], some of which has been incorporated in the literature of refraction [72] and mirages [73,74].…”
Section: Complicationsmentioning
confidence: 99%
“…So the total width of this image depends on the height of the tallest irregularities on the surface: rocks and bushes on dry land, or the largest waves on water. The importance of the dip of the sea horizon for celestial navigation has produced a huge literature on this subject; e.g., [67][68][69][70][71], some of which has been incorporated in the literature of refraction [72] and mirages [73,74].…”
Section: Complicationsmentioning
confidence: 99%