Design of a multiple-zone aperture and application to a Fabry-Perot interferometer.

A design for a multiple-zone aperture (MZA), which is applied to a Fabry-Perot interferometer for gaining greater throughput, is described. It is shown that there exists a definite value for the width of the aperture that gives, the minimum error in Doppler temperature measurements when instrumental parameters and the width of the source profiles are given. The effects caused by the imperfections of the MZA are analyzed. The successful use of an MZA with a 15-cm (6-in.) Fabry-Perot interferometer for measurement of an airglow emission line is described.

[1]  E. B. Armstrong Largeur de la raie 01 λ 5 577 du ciel nocturne et des aurores , 1958 .

[2]  A. Nagy,et al.  Interferometric measurements of the 6300 A Doppler temperature during a magnetic storm , 1969 .

[3]  P. Jacquinot,et al.  Caractères communs aux nouvelles méthodes de spectroscopie interférentielle ; Facteur de mérite , 1958 .

[4]  G. Hernández,et al.  Direct measurements of nighttime thermospheric winds and temperatures, 3. Monthly variations during solar minimum , 1977 .

[5]  J. Meaburn Scanning Fabry-Pérot interferometers for nebular studies , 1968 .

[6]  G. Hernandez Analytical description of a Fabry-Perot spectrometer. 3:Off-axis behavior and interference filters: erratum. , 1974, Applied optics.

[7]  M. A. Biondi,et al.  Equatorial F-region neutral winds from nightglow OI 630.0 nm Doppler shifts , 1978 .

[8]  A. Jarrett,et al.  Observations of the 6300 Å OI nightglow emission , 1966 .

[9]  G. Hernandez,et al.  Analytical description of a Fabry-Perot photoelectric spectrometer. , 1966, Applied optics.

[10]  P. Hays,et al.  A technique for recovering Doppler line profiles from fabry-perot interferometer fringes of very low intensity. , 1971, Applied optics.

[11]  P. Hays,et al.  Direct observations of thermospheric winds during geomagnetic storms , 1971 .

[12]  G. Shepherd,et al.  Upper atmospheric temperatures from Doppler line widths - II. Measurements on the OI 5577 and OI 6300 Å lines in aurora , 1962 .

[13]  G. Hernández,et al.  Simultaneous measurements of midlatitude thermospheric winds at 105° W and 79° W longitude , 1978 .

[14]  G. Hernández,et al.  Observations of large‐scale thermospheric waves during geomagnetic storms , 1978 .

[15]  R. V. Karandikar Interferometric measurements of λ5577 Å emission temperatures in aurora , 1968 .

[16]  D. Wark Doppler Widths of the Atomic Oxygen Lines in the Airglow. , 1960 .

[17]  L. V. D. Phil. LVI. The temperature distribution within the auroral region of the atmosphere , 1937 .

[18]  G. Hernández,et al.  Direct measurements of nighttime thermospheric winds and temperatures, 1. Seasonal variations during geomagnetic quiet periods , 1976 .

[19]  M. A. Biondi,et al.  Twilight and nighttime ionospheric temperatures from oxygen λ6300 and λ5577 spectral-line profiles , 1972 .

[20]  H. Babcock No. 259. A study of the green auroral line by the interference method. , 1923 .

[21]  G. Hernández,et al.  Direct measurements of nighttime thermospheric winds and temperatures, 2. Geomagnetic storms , 1976 .