Abstract

ABSTRACT MICADO, a near-infrared imager for the Extremely Large Telescope, is being designed to deliver diffraction limited imaging and 50 microarcsecond (μas) astrometric accuracy. MICADO employs an atmospheric dispersion corrector (ADC) to keep the chromatic elongation of the point spread function (PSF) under control. We must understand the dispersion and residuals after correction to reach the optimum performance. Therefore, we identified several sources of chromatic dispersion that need to be considered for the MICADO ADC. First, we compared common models of atmospheric dispersion to investigate whether these models remain suitable for MICADO. We showed that the differential dispersion between common atmospheric models and integration over the full atmosphere is less than 10 μas for most observations in H band. We then performed an error propagation analysis to understand the uncertainty in the atmospheric dispersion as a function of atmospheric conditions. In addition, we investigated the impact of photometric colour on the astrometric performance. While the differential refraction between stars within the same field of view can be significant, the inclusion of an ADC rendered this effect negligible. For MICADO specifically, we found that the current optomechanical design dominates the residual dispersion budget of 0.4 milliarcseconds (mas), with a contribution of 0.31 mas due to the positioning accuracy of the prisms and up to 0.15 mas due to a mismatch between the dispersive properties of the glass and the atmosphere. We found no showstoppers in the design of the MICADO ADC for achieving 50 μas relative astrometric accuracy.

Highlights

  • The generation of large telescopes, such as the Extremely Large Telescope (ELT; ESO 2011), the Thirty Meter Telescope (Sanders 2013) and the Giant Magellan Telescope (Johns et al 2012), offer a significant increase in aperture diameter

  • The increased resolution and desired astrometric performance of upcoming imaging instruments on the generation of extremely large telescopes required atmospheric dispersion to be studied in more detail than before

  • For MICADO the residual chromatic dispersion on the detector is required to be smaller than 0.4 mas in H band to achieve the desired astrometric accuracy of 50 μas

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Summary

INTRODUCTION

The generation of large telescopes, such as the Extremely Large Telescope (ELT; ESO 2011), the Thirty Meter Telescope (Sanders 2013) and the Giant Magellan Telescope (Johns et al 2012), offer a significant increase in aperture diameter With this increase in telescope size, several unwanted optical effects become important or can no longer be assumed negligible and have to be reconsidered Due to the wavelength dependence of the atmosphere’s refractive index, light with shorter wavelengths is refracted more than light with longer wavelengths, causing an elongation of the PSF To counteract this effect, MICADO incorporates an atmospheric dispersion corrector (ADC) consisting of two mirrored counter-rotating Amici prisms. By finding a sufficiently detailed model of the atmosphere and ADC, we are able to study the various systematic and random contributors to the chromatic dispersion expected on the image plane of MICADO.

ATMOSPHERIC DISPERSION
Plane-parallel atmosphere model
Cassini’s refraction model
Refraction integral
Error function model
Oriani’s theorem
Our preferred model
Refractivity model
DESCRIPTION OF THE ADC
Dispersion of an atmospheric dispersion corrector
Discretization of the dispersion correction
Systematic errors of the atmospheric dispersion calculation
The Zemax atmospheric dispersion model
Impact of local weather along the line of sight
Differential dispersion as a result of optical properties
Differential refraction as a result of different photometric colour
ADDITIONAL CONSIDERATIONS
CONCLUSIONS
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