1968
DOI: 10.1007/bf02525701
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The use of atmospheric dispersion in optical distance measurement

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Cited by 10 publications
(6 citation statements)
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“…In addition to describing the ray tracing procedure we (1) give examples of differences between Ds and D, (2) indicate errors associated with the dual zenith angle method for height difference determination, and (3) demonstrate from both theory and the ray-tracing calculations through real atmospheres that a systematic error in multiwavelength measurements results from neglecting the physical path length difference between the two light beams (of different wavelength) through the dispersive atmosphere. • Owens [1968] cites results from a technical report by Thayer that indicate similar limitations to the use of a dual-color system, as derived here. Huggett and Slater [1977] give equations for, and field measurements made in California with, a three-wavelength instrument.…”
Section: Ray Tracingsupporting
confidence: 61%
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“…In addition to describing the ray tracing procedure we (1) give examples of differences between Ds and D, (2) indicate errors associated with the dual zenith angle method for height difference determination, and (3) demonstrate from both theory and the ray-tracing calculations through real atmospheres that a systematic error in multiwavelength measurements results from neglecting the physical path length difference between the two light beams (of different wavelength) through the dispersive atmosphere. • Owens [1968] cites results from a technical report by Thayer that indicate similar limitations to the use of a dual-color system, as derived here. Huggett and Slater [1977] give equations for, and field measurements made in California with, a three-wavelength instrument.…”
Section: Ray Tracingsupporting
confidence: 61%
“…The dual-color distance-measuring instrument accounts for the refractive index along the line on the basis of dispersion [Owens, 1968;Bouricius and Earnshaw, 1974;Slater and Huggett, 1976;Huggett and Slater, 1977]. The approach assumes that the physical path is the same for each beam, allowing one to obtain the difference in refractive index from the difference in optical path length.…”
Section: Dual-color Lasermentioning
confidence: 99%
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“…Alternatively, the two-colour method proposed by Bender and Owens1516 can realize air refractive index correction without precise knowledge of environmental parameters31718192021. The basic principle of the method is to employ lights with two different wavelengths to measure the same geometrical distance D and thus obtain two optical distances D 1 and D 2 .…”
mentioning
confidence: 99%
“…Atmospheric parameters such as the temperature, pressure, humidity, and possibly the CO 2 content are measured to calculate the refractive index using the Edlén equation 6 , 7 , However, it is difficult to get an accurate distribution of these parameters along the optical path, especially at long distances and with a moving stage 8 . Nevertheless, the influence of the turbulence of the atmosphere can be corrected using the two-color method proposed by Bender and Owens 9 , 10 , which is widely used in optical frequency combs 11 14 and laser interferometers 15 18 . This method measures a geometric distance, L , with both wavelength λ 1 and λ 2 , to obtain two optical distances, L λ 1 and L λ 2 , and gives the geometric distance L = L λ 1 − A ( L λ 2 − L λ 1 ), where A is the so-called A-coefficient in two-color method that represents the dispersion relation for air refractive indices at two wavelengths.The conventional two-color method eliminated the influence of the atmosphere, yet simultaneously enlarged the uncertainties in measured optical distances, Δ L λ 1 and Δ L λ 2 , because of the stability of the laser wavelength, thermal expansion and the optical thermal drift 19 .…”
Section: Introductionmentioning
confidence: 99%