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2. General context

The aim of this section is essentially to provide the reader with a few classical notations as well as basic concepts of interferometry. Paragraph 2.1 is a brief theoretical tutorial on inteferometry. The purpose of the Double Fourier interferometric mode probing both temporal and spatial coherence properties of sources is explained in paragraph 2.2. Eventually, paragraph 2.3 adresses the aim of this paper, that is to say the nature of the disturbances generating optical path fluctuations.

2.1. Brief tutorial on interferometry

Equations derivations are classical and can be found in litterature (Goodman 1985 for example). Nevertheless, I intend to give a fundamental subset of equations whose accurate knowledge is mandatory for a good understanding of the remaining of the article. Let us consider two pupils tex2html_wrap_inline1780 and tex2html_wrap_inline1782 of an interferometer and the corresponding sampled complex amplitudes of an astronomical wavefront tex2html_wrap_inline1784 and tex2html_wrap_inline1786, where tex2html_wrap_inline1788 is the wavenumber and t is time. The two amplitudes are combined and sent to a detector. The monochromatic energy detected at the output of the combiner is proportional to the average squared modulus (on a time scale far greater than the period of the wave) of the sum of the two fields:


equation212
For sake of simplicity, all multiplicative coefficients (detector gain, interferometer transmission, etc ...) will be set to one and their expressions will be dropped in the following equations. The monochromatic energy collected by the two pupils (which is proportionnal to the spectrum of the source) is supposed to be the same and the normalized total energy over the bandwidth is noted tex2html_wrap_inline1792. Equation (1) is then rewritten as:
eqnarray218
where tex2html_wrap_inline1794 is the complex degree of coherence of the two beams coming from the source and collected by the two pupils of the interferometer. For a monochromatic radiation, it has a simple expression as a function of the delay tex2html_wrap_inline1796 between the two beams (Goodman 1985):
equation227
where v is the rate of change of opd. tex2html_wrap_inline1800 is the coherence factor of the two beams or fringe visibility and is wavelength dependent. The value of visibility is determined by the geometrical aspect of the source and by the geometrical characteristics of the baseline. It is the Fourier transform of the intensity distribution of the source at a spatial frequency equal to the vector baseline over wavelength according to the Van Cittert-Zernike theorem (Born & Wolf 1980; Goodman 1985). Visibilitygif is the observable measured by interferometers.
It is equivalent to express delay either as a temporal delay tex2html_wrap_inline1802 or as an optical path difference x as the ratio of the two is the speed of the fringes v. In wide band, Eq. (2) becomes:
equation237
It is necessary to compensate delay of one the two beams with respect to the other one when recording the interferogram because the coherence length, in wide band, is only a few fringes. Monochromatic waves coherently interfere around the equal optical path position when the optical paths of the two beams are matched by a delay line.
The first term in Eq. (4) will be left aside in the following and I will only consider the second one which is the modulated part of the interferogram. When the complex spectrum is defined as the hermitian part of the spatio-temporal source spectrum (modulus is an even function and phase is an odd function of wavenumber):
equation244
the modulated part of energy, noted tex2html_wrap_inline1808, gets a more convenient expression:
equation253
In other words, the Fourier transform of the modulated interferometric signal is the complex spectrum of the astronomical source.

2.2. Double Fourier interferometry

A few different ways of doing interferometry (mostly depending on measured quantities) exist (see review by M. Shao 1992). Some interferometers recombine beams in the pupil plane whereas others are image plane oriented. Here, no distinction will be made between these two different philosophies. Some interferometers (type I) are operated in the long exposure mode, that is to say that a servoed delay line sets the optical path difference (thereafter opd) to a constant value allowing the integration of the interferometric signal to achieve high signal to noise (S/N) ratios on fringe modulation. The value of the opd can be varied to scan through the whole interferogram. Type II interferometers can be considered as short exposure interferometers. The interferogram is acquired during a continuous scan of the opd which is produced either by the Earth's rotation or by a translating retroreflecting unit moving at a constant speed or by a combination of the two. Integration is then no longer possible. Type I interferometers are not opd fluctuation sensitive as the opd is servoed, whereas many factors can introduce opd fluctuations in type II interferometers (this point will be adressed in Sect. 2.3). Type II interferometers are dedicated to spectral data analysis for they naturally reach a higher spectral resolution while type I data are reduced in direct space. These type II interferometers are called Double Fourier Interferometers (hereafter DFI) because they both probe spatial and temporal coherence properties of the light emitted by astrophysical sources (Itoh & Ohtsuka 1986; Mariotti & Ridgway 1988). Spatial information is contained in the modulated energy of interferograms as shown in Sect. 2.1 and is wavelength dependent. The Fourier transform of the interferogram sequence yields the source temporal spectrum rescaled by the visibility function. It has been shown (Ridgway et al. 1986) that an accurate knowledge of the visibility-wavelength relation would have fruitful astrophysical implications, as well as visibility as a function of spatial frequency. DFI allows the determination of the visibility as a function of wavelength and is the interferometric mode that is mostly concerned in the following of the paper.

2.3. Optical path fluctuations and phase information loss

As shown in Eq. (6) an interferogram can be considered as a temporal sequence whose Fourier transform is proportionnal to the spectrum of the source. The two conjugate variables are the opd (or time) in the direct space and wavenumber (or frequency) in the Fourier space; one shifts from one set of conjugate variables to the other by multiplying or dividing by the speed of the fringes. Thus opd varies linearly with time. This is what one should expect in an ideal interferometer. In reality this occurs in a different way. Opd does not vary linearily with time. Some opd distortions are introduced and have mechanical and atmospheric sources. Vibrations of static optics on the beam path change its length and make it oscillate. But they can be lowered to an inoffensive magnitude by increasing the stiffness of the optics and by absorbing vibrations. Non-linearities in the motion of the retroreflecting stage of the delay line cause opd to fluctuate but they can also be cancelled out by servoing the speed of the carriage supporting the retroreflector. Some fiercer fluctuations are generated by atmospheric turbulence. Here we assume that atmospheric perturbations of wavefronts are reduced to the 0-order ones (the spatially averaged pertubations on the pupil) and that higher orders have been filtered out by using monomode fibers for example (Coudé du Foresto & Ridgway 1991; Coudé du Foresto et al. 1992), by data reduction or with adaptive optics. The 0-order term is known as ``piston effect'' and opd fluctuations are due to differential piston between two apertures of the interferometer. But piston and differential piston stand for the same physical phenomenon.
Opd fluctuations result in the loss of the Fourier relation between the spectrum and the interferogram sequence preventing physical information recovery from the spectrum. Figure 3 of Sect. 3 shows four simulated low resolution spectra. The first one is computed from an opd fluctuation free interferogram whereas the others simulate observed spectra with regular turbulence conditions. It is obvious that without any piston correction no accurate information can be extracted from these spectra. Besides, piston introduces a random shift of the central fringe of the interferogram preventing measurement of the exact phase of visibilities, the accurate knowledge of which being essential to reconstruct a high resolution image of the source.
If most sources of optical path fluctuations have negligeable effects, atmospheric turbulence effects at optical wavelengths must be taken into account. It is possible to artificially increase the length of coherent interferogram by scanning at a high speed. Rapid scanning freezes piston but it does not reduce its amplitude. Besides, fast scanning reduces the instrumental visibility (hence the S/N ratio of the modulated signal) as the detector response decreases with increasing frequencies. Turbulence opd fluctuations thus turn out to be a strong limitation to optimum information extraction in optical astronomical interferometry. In the following Sects. I will expose a method to correct ``pistoned'' interferograms to retrieve the modulus of the spectrum and the phase to within a constant. This method does not take into account the possibility to retrieve the exact phase of visibilities and does not address the issue of image reconstruction in interferometry.


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