2022
DOI: 10.7498/aps.71.20212086
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Thermal imaging drift monitoring of Doppler asymmetric spatial heterodyne spectroscopy for wind measurement based on segmented edge fitting

Abstract: Doppler asymmetric spatial heterodyne spectroscopy is recently developed for spaceborne measurement of middle and upper atmospheric wind field, which relies on the accurate inverse of interferogram phase to calculate the Doppler shift of airglow emission lines. The change of temperature leads to thermal deformation of the optical and mechanical components, causing thermal drift of the imaging plane relative to detector, changing the distribution of interferogram phase on pixels, and directly introducing phase … Show more

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Cited by 4 publications
(3 citation statements)
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“…At present, phase inversion mainly uses an inversion method based on the Fourier transform 23 , 24 . The process of this method is as follows.…”
Section: Principle Of the Dash Interferometermentioning
confidence: 99%
See 1 more Smart Citation
“…At present, phase inversion mainly uses an inversion method based on the Fourier transform 23 , 24 . The process of this method is as follows.…”
Section: Principle Of the Dash Interferometermentioning
confidence: 99%
“…At present, phase inversion mainly uses an inversion method based on the Fourier transform. 23,24 The process of this method is as follows. The real fringe data of the interferogram are transformed to the frequency domain by a Fourier transform, and the characteristic peaks are extracted in the frequency domain to obtain the target spectrum.…”
Section: Principle Of the Dash Interferometermentioning
confidence: 99%
“…It uses the perfect Fourier transform relationship between the interferogram and the incident light spectrum to invert the Doppler frequency shift of the incident light spectrum by calculating the complex interferogram phase [19]. The representative instrument is the Michelson Interferometer for Global Highresolution Thermospheric Imaging (MIGHTI) [20,21], which was launched in 2019 and is used to detect the horizontal wind velocity profiles and thermospheric temperatures in the altitude range of 90-300 km. Due to the large OPD, the DASH technique has a large phase error in spectral recovery.…”
Section: Introductionmentioning
confidence: 99%